9a0d6456d9c5b7a9a6d5ca3899f960fa3f06785a 2020-09-23T13:24:38 (Month 12) December Mean Direction of the Maximum Directionally Resolved Wave Power Wave Energy Resource | Direction of Maximum Directionally Resolved Wave Power | Monthly Means The December mean direction of the maximum directionally resolved wave power is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using December data from December 1980 to December 2010. The direction of the maximum directionally resolved wave power is 0j and is used as the characteristic direction of the sea-state. Note, accurate determination of the directionally resolved wave power, J0, and its maximum, Jm, and hence 0j require spectral data, which was not archived at all grid points of the CAWCR wave hindcast. Here, we provide estimates of Jm using spectra reconstructed with archived gridded wave partition data, assuming a Pierson-Moskowitz spectra fit to each partition, with assumed spreading, and superimposed to produce a reconstructed spectra. Further details of the method used to estimate Jm are provided in the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The December mean direction of the maximum directionally resolved wave power is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using December data from December 1980 to December 2010. The direction of the maximum directionally resolved wave power is 0j and is used as the characteristic direction of the sea-state. Note, accurate determination of the directionally resolved wave power, J0, and its maximum, Jm, and hence 0j require spectral data, which was not archived at all grid points of the CAWCR wave hindcast. Here, we provide estimates of Jm using spectra reconstructed with archived gridded wave partition data, assuming a Pierson-Moskowitz spectra fit to each partition, with assumed spreading, and superimposed to produce a reconstructed spectra. Further details of the method used to estimate Jm are provided in the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.jthm_avg.12 http://oa-gis.csiro.au/data/jthm/ww3.aus_4m.jthm_avg.12.nc e64e0b29e3bfd45cca9d6f6fc985667d4ad3dd6d 2020-09-23T13:24:38 Annual Mean Spectral Width Wave Energy Resource | Wave Spectral Width | Statistics The annual mean spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The annual mean spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.nu_avg http://oa-gis.csiro.au/data/nu/ww3.aus_4m.nu_avg.nc 0f374bf7bb0a8f42872f0b0fdeea9c9f97820967 2020-09-23T13:24:38 Monthly Variability of Spectral Width Wave Energy Resource | Wave Spectral Width | Statistics The monthly variability of spectral width provides a convenient measure of the variability of the mean monthly spectral width over a typical year. It is determined as maximum range of the mean monthly annual cycle calculated from the CAWCR global wave hindcast. The mean monthly annual cycles were determined using the archived hourly 4’ Australian grid from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The monthly variability of spectral width provides a convenient measure of the variability of the mean monthly spectral width over a typical year. It is determined as maximum range of the mean monthly annual cycle calculated from the CAWCR global wave hindcast. The mean monthly annual cycles were determined using the archived hourly 4’ Australian grid from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.nu_avg_mv http://oa-gis.csiro.au/data/nu/ww3.aus_4m.nu_avg_mv.nc b91afea358d1fe6fb0298a2c1584350b0a04bc07 2020-09-23T13:24:38 Maximum Spectral Width Wave Energy Resource | Wave Spectral Width | Statistics The maximum spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The maximum spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.nu_max http://oa-gis.csiro.au/data/nu/ww3.aus_4m.nu_max.nc 12209e60d480656467e72cce65d1a0e384ec0f67 2020-09-23T13:24:39 Minimum Spectral Width Wave Energy Resource | Wave Spectral Width | Statistics The minimum spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The minimum spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.nu_min http://oa-gis.csiro.au/data/nu/ww3.aus_4m.nu_min.nc 7ac65f260a838e770ed79b4b063e1bc032344267 2020-09-23T13:24:39 10th Percentile of Spectral Width Wave Energy Resource | Wave Spectral Width | Statistics The 10th percentile of spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The 10th percentile of spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.nu_p10 http://oa-gis.csiro.au/data/nu/ww3.aus_4m.nu_p10.nc 3b1ae9e52f47640cfb98b32f389b271476d46b68 2020-09-23T13:24:39 50th Percentile of Spectral Width Wave Energy Resource | Wave Spectral Width | Statistics The 50th percentile of spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The 50th percentile of spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.nu_p50 http://oa-gis.csiro.au/data/nu/ww3.aus_4m.nu_p50.nc 4fa7df0553020f92d0473d7d0a636c025ada76a7 2020-09-23T13:24:39 90th Percentile of Spectral Width Wave Energy Resource | Wave Spectral Width | Statistics The 90th percentile of spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The 90th percentile of spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.nu_p90 http://oa-gis.csiro.au/data/nu/ww3.aus_4m.nu_p90.nc b2eecf74b456e61c124ed3c29c2e2cf3ce5546a5 2020-09-23T13:24:39 Standard Deviation of Spectral Width Wave Energy Resource | Wave Spectral Width | Statistics The standard deviation of spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The standard deviation of spectral width is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. The spectral width characterises the relative spreading of energy along the wave spectrum. The spectral width is defined as the standard deviation of the period variance density, normalised by energy period. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). Spectral width is not standard output from the WaveWatch III model, but is determined from available parameters HS, T01 and T02, from which the moments m0, m1 and m2 can be determined. For further details on the calculation of the spectral width, please refer to the Atlas report (Hemer et al., 2016) For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.nu_std http://oa-gis.csiro.au/data/nu/ww3.aus_4m.nu_std.nc 2325e18768d3a95e6e65d6e1090a2979069189d6 2020-09-23T13:24:39 Annual Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Statistics The annual mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The annual mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg.nc af02b8cf40ac92fc7d3d677fa8c1b3bbb421f9d9 2020-09-23T13:24:39 (Month 01) January Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The January mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using January data from January 1980 to January 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The January mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using January data from January 1980 to January 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg01 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg01.nc 14e9db4e523d4f43fc101b622598516a64f1eb39 2020-09-23T13:24:39 (Month 02) February Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The February mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using February data from February 1980 to February 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The February mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using February data from February 1980 to February 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg02 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg02.nc 47dc040597d5a70af3b032f2272ef52367aa2318 2020-09-23T13:24:39 (Month 03) March Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The March mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using March data from March 1980 to March 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The March mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using March data from March 1980 to March 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg03 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg03.nc 8750f81b00a6837f96b49c0a612e885727639ba0 2020-09-23T13:24:39 (Month 04) April Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The April mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using April data from April 1980 to April 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The April mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using April data from April 1980 to April 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg04 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg04.nc 154ddaab049f83d90859fbc15bee73064d1c1ba0 2020-09-23T13:24:40 (Month 05) May Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The May mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using May data from May 1980 to May 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The May mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using May data from May 1980 to May 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg05 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg05.nc c064b580c560ba03ef97ffbbb4cc0988f9fbab57 2020-09-23T13:24:40 (Month 06) June Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The June mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using June data from June 1980 to June 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The June mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using June data from June 1980 to June 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg06 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg06.nc a277ee08241a25f956a3c4d9d655b25cf315ec42 2020-09-23T13:24:40 (Month 07) July Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The July mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using July data from July 1980 to July 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The July mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using July data from July 1980 to July 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg07 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg07.nc a78e8fad4fba30d357288aae224a535758c56483 2020-09-23T13:24:40 (Month 08) August Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The August mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using August data from August 1980 to August 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The August mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using August data from August 1980 to August 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg08 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg08.nc fa9b69bfe342ffbfc333b7ecefd66118098461fc 2020-09-23T13:24:40 (Month 09) September Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The September mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using September data from September 1980 to September 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The September mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using September data from September 1980 to September 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg09 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg09.nc 64de53311df497d0bac1d63214549269ecf194c0 2020-09-23T13:24:40 (Month 10) October Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The October mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using October data from October 1980 to October 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The October mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using October data from October 1980 to October 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg10 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg10.nc dc90e1ed5b56f5a2ce89d57f556eacfcdd4f6859 2020-09-23T13:24:40 (Month 11) November Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The November mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using November data from November 1980 to November 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The November mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using November data from November 1980 to November 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg11 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg11.nc 0002a60c4e9d8cd03c1f284e75116f978f62e83d 2020-09-23T13:24:40 (Month 12) December Mean Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Monthly Means The December mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using December data from December 1980 to December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The December mean wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using December data from December 1980 to December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg12 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg12.nc 80c542ea9c321d208a736554615bef86be7bfaf2 2020-09-23T13:24:40 Monthly Variability of Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Statistics The monthly variability of wave energy period provides a convenient measure of the variability of the mean monthly wave energy period over a typical year. It is determined as maximum range of the mean monthly annual cycle calculated from the CAWCR global wave hindcast. The mean monthly annual cycles were determined using the archived hourly 4’ Australian grid from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The monthly variability of wave energy period provides a convenient measure of the variability of the mean monthly wave energy period over a typical year. It is determined as maximum range of the mean monthly annual cycle calculated from the CAWCR global wave hindcast. The mean monthly annual cycles were determined using the archived hourly 4’ Australian grid from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_avg_mv http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_avg_mv.nc 5446e4710af8d48813d82017190dbe905b3dca78 2020-09-23T13:24:40 Maximum Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Statistics The maximum wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The maximum wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_max http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_max.nc c9f34467b3f7c20b08e5f48d0ef57ceeb7bb1c77 2020-09-23T13:24:41 Minimum Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Statistics The minimum wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The minimum wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_min http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_min.nc 0857e8d7561f0f3dbd48ab5a956e0d2f450e27de 2020-09-23T13:24:41 10th Percentile of Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Statistics The 10th percentile of wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The 10th percentile of wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_p10 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_p10.nc 1a67924c30a0e73c2cf1f740aeb3c1b1f9ceec9e 2020-09-23T13:24:41 50th Percentile of Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Statistics The 50th percentile of wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The 50th percentile of wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_p50 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_p50.nc 1497f896e3233c130c9881ecbeabef4dd9211f60 2020-09-23T13:24:41 90th Percentile of Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Statistics The 90th percentile of wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The 90th percentile of wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_p90 http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_p90.nc 08dd18cac0f9c3338300f33ab10bbd100d246a42 2020-09-23T13:24:41 Standard Deviation of Wave Energy Period Earth Science | Oceans | Ocean Waves Earth Science | Oceans | Ocean Waves | Wave Period Wave Energy Resource | Wave Period | Statistics The standard deviation of wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. The standard deviation of wave energy period is derived from the CAWCR global wave hindcast, using data from the archived hourly 4’ Australian grid, using data from 1st January 1980 to 31st December 2010. Wave energy period, Te is a measure of the length of a wave. The wave energy period is the mean period of the wave field with respect to the spectral distribution of energy in the wave field. An equation describing its calculation can be found in the the atlas report (Hemer et al., 2016). For further information on the CAWCR wave hindcast, see Durrant et al (2014)**. See DAP entry http://dx.doi.org/10.4225/08/523168703DCC5 for 1979-2010 data. Please note that the licensee/user is required to acknowledge the source of this data on the following terms: 'Source: Bureau of Meteorology and CSIRO © 2013'. Apart from dealings under the Copyright Act 1968, the licensee shall not reproduce (electronically or otherwise), modify or supply (by sale or otherwise) this data without written permission. Please contact us for more information. Input data: NCEP CFSv2 surface winds and sea ice, http://cfs.ncep.noaa.gov. Wave model used: WaveWatch III, http://polar.ncep.noaa.gov/waves/wavewatch/wavewatch.shtml The Centre for Australian Weather and Climate Research (CAWCR) is a partnership between the Bureau of Meteorology and CSIRO. Hindcast modelling undertaken as part of the PACCSAP (Pacific-Australia Climate Change Science and Adaptation Planning) Project 4.3 "High resolution wind-wave climate and projections of change in the Pacific region for coastal hazard assessments" in 2012, funded by DCCEE and AusAID and undertaken jointly by CSIRO and the BoM. This dataset was produced as part of the Australian Renewable Energy Agency – CSIRO Oceans and Atmosphere Flagship co-funded Australian Wave Energy Atlas Project. Bureau of Meteorology Australia CSIRO Australia 175.00038146972656 -49.999998331069946 100.0 3.000264883041382 dataset http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?request=GetLegendGraphic&format=image%2Fpng&width=20&height=20&layer=awavea2019%3Aww3.aus_4m.te_std http://oa-gis.csiro.au/data/te/ww3.aus_4m.te_std.nc 4ba50e4a3243fa768797dcdbc1541204db89a7e1 2020-09-23T13:24:19 GeoServer Web Map Service service WFS WMS GEOSERVER A compliant implementation of WMS plus most of the SLD extension (dynamic styling). Can also generate PDF, SVG, KML, GeoRSS A compliant implementation of WMS plus most of the SLD extension (dynamic styling). Can also generate PDF, SVG, KML, GeoRSS http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& http://oa-gis.csiro.au/geoserver/wms?SERVICE=WMS& 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