Projected 21st century changes in extreme wind-wave events

被引:128
作者
Meucci, Alberto [1 ]
Young, Ian R. [1 ]
Hemer, Mark [2 ]
Kirezci, Ebru [1 ]
Ranasinghe, Roshanka [3 ,4 ,5 ]
机构
[1] Univ Melbourne, Dept Infrastruct Engn, Melbourne, Vic 3010, Australia
[2] CSIRO Oceans & Atmosphere, Hobart, Tas 7001, Australia
[3] IHE Delft, Dept Water Sci & Engn, POB 3015, NL-2610 DA Delft, Netherlands
[4] Deltares, Harbour Coastal & Offshore Engn, POB 177, NL-2600 MH Delft, Netherlands
[5] Univ Twente, Fac Engn Technol, Water Engn & Management, POB 217, NL-7500 AE Enschede, Netherlands
基金
澳大利亚研究理事会;
关键词
CLIMATE-CHANGE SIGNAL; TROPICAL CYCLONES; OCEAN WIND; ENSEMBLE; CMIP5; UNCERTAINTY; HEIGHTS; TRENDS; SPEED; SEA;
D O I
10.1126/sciadv.aaz7295
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
We describe an innovative approach to estimate global changes in extreme wave conditions by 2100, as a result of projected climate change. We generate a synthetic dataset from an ensemble of wave models forced by independent climate simulation winds, enhancing statistical confidence associated with projected changes in extreme wave conditions. Under two IPCC representative greenhouse gas emission scenarios (RCP4.5 and RCP8.5), we find that the magnitude of a 1 in 100-year significant wave height (H-s) event increases by 5 to 15% over the Southern Ocean by the end of the 21st century, compared to the 1979-2005 period. The North Atlantic shows a decrease at low to mid latitudes to (approximate to 5 to 15%) and an increase at high latitudes (approximate to 10%). The extreme significant wave height in the North Pacific increases at high latitudes by 5 to 10%. The ensemble approach used here allows statistical confidence in projected changes of extremes.
引用
收藏
页数:9
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