Decadal Variability of Global Ocean Significant Wave Height

被引:0
作者
ZHENG Chongwei [1 ,2 ,3 ]
ZHOU Lin [1 ]
SHI Weilai [1 ,4 ]
LI Xin [1 ]
HUANG Chaofan [1 ]
机构
[1] College of Meteorology and Oceanography, People’s Liberation Army University of Science&Technology
[2] National Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics (LASG), Institute of Atmospheric Physics, the Chinese Academy of Sciences
[3] Dalian Naval Academy
[4] Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, Nanjing University of Information Science & Technology
基金
中国国家自然科学基金;
关键词
global ocean; significant wave height; long-term trend; regional differences; seasonal differences; dominant season;
D O I
暂无
中图分类号
P731.2 [海洋动力学];
学科分类号
0707 ;
摘要
This paper presents the long-term climate changes of significant wave height(Hs) in 1958–2001 over the entire global ocean using the 45-year European Centre for Medium-Range Weather Forecasts(ECMWF) Reanalysis(ERA-40) wave data. The linear trends in Hs and regional and seasonal differences of the linear trends for Hs were calculated. Results show that the Hs exhibits a significant increasing trend of about 4.6 cm decade-1 in the global ocean as a whole over the last 44 years. The Hs changes slowly during the periods 1958–1974 and 1980–1991, while it increases consistently during the periods 1975–1980 and 1995–1998. The Hs reaches its lowest magnitude in 1975, with annual average wave height about 2 m. In 1992, the Hs has the maximum value of nearly 2.60 m. The Hs in most ocean waters has a significant increasing trend of 2–14 cm decade-1 over the last 44 years. The linear trend exhibits great regional differences. Areas with strong increasing trend of Hs are mainly distributed in the westerlies of the southern Hemisphere and the northern Hemisphere. Only some small areas show obvious decreasing in Hs. The long-term trend of Hs in DJF(December, January, February) and MAM(March, April, May) is much more stronger than that in JJA(June, July, August) and SON(September, October, November). The linear trends of the Hs in different areas are different in different seasons; for instance, the increasing trend of Hs in the westerlies of the Pacific Ocean mainly appears in MAM and DJF.
引用
收藏
页码:778 / 782
页数:5
相关论文
共 17 条
[1]  
Variation of the wave energy and significant wave height in the China Sea and adjacent waters. ZHENG Chongwei,LI Chongyin. Renewable and Sustainable Energy Reviews . 2015
[2]  
100-year return value estimates for ocean wind speed and significant wave height from the ERA-40 data. Caires, Sofia,Sterl, A. Journal of Climatology . 2005
[3]  
Wave climate variability in the North-East Atlantic Ocean over the last six decades[J] . Guillaume Dodet,Xavier Bertin,Rui Taborda. &nbspOcean Modelling . 2009 (3)
[4]   A Global View on the Wind Sea and Swell Climate and Variability from ERA-40 [J].
Semedo, Alvaro ;
Suselj, Kay ;
Rutgersson, Anna ;
Sterl, Andreas .
JOURNAL OF CLIMATE, 2011, 24 (05) :1461-1479
[5]  
Waves and Climate Changeon the Australian Coast. M.A.Hemer,J.A.Church,J.R.Hunter. Journal ofCoastal Research . 2007
[6]  
Assessing the China Sea wind energy and wave energy resources from 1988 to 2009[J] . Chong-wei Zheng,Jing Pan,Jia-xun Li. &nbspOcean Engineering . 2013
[7]  
A significant increase in wave height in the North Atlantic Ocean over the 20th century[J] . Xavier Bertin,Elizabeth Prouteau,Camille Letetrel. &nbspGlobal and Planetary Change . 2013
[8]  
Variation of the wave energy and significant wave height in the China Sea and adjacent waters[J] . Chong Wei Zheng,Chong Yin Li. &nbspRenewable and Sustainable Energy Reviews . 2015
[9]   Interaction between Anomalous Winter Monsoon in East Asia and EI Nino Events [J].
李崇银 .
AdvancesinAtmosphericSciences, 1990, (01) :36-46
[10]  
The Interannual Variability of East Asian Winter Monsoon and Its Relation to the Summer Monsoon[J]. 陈文,Han-F.Graf,黄荣辉. Advances in Atmospheric Sciences. 2000(01)