Long‐Term Trend of the Tropical Pacific Trade Winds Under Global Warming and Its Causes

Journal of Geophysical Research: Oceans - Tập 124 Số 4 - Trang 2626-2640 - 2019
Yang Li1, Quanliang Chen1, Xiaoran Liu2, Jianping Li3, Nan Xing4, Fei Xie5, Juan Feng5, Xin Zhou1, Hongke Cai1, Zhenglin Wang1
1College of Atmospheric Science, Plateau Atmosphere and Environment Key Laboratory of Sichuan Province, Chengdu University of Information Technology, Chengdu, China
2Chongqing Climate Center, Chongqing, China
3Key Laboratory of Physical Oceanography/Institute for Advanced Ocean Studies, Ocean University of China and Qingdao National Laboratory for Marine Science and Technology, Qingdao, China
4Beijing Municipal Weather Forecast Center, Beijing, China
5College of Global Change and Earth System Sciences, Beijing Normal University, Beijing, China

Tóm tắt

AbstractThe recent intensification of trade winds over the tropical Pacific is the strongest ever observed in the past hundred years. This strengthening trend is of great interest in recent research, but the causes are still unclear. Using two relatively long‐term surface wind data sets, the present research shows that there is an overall strengthening trend of the trades in the western equatorial Pacific and an overall weakening trend in the eastern equatorial Pacific. This long‐term trend pattern can be primarily attributed to the cold tongue mode (CTM) rather than to the impact of El Niño–Southern Oscillation (ENSO), El Niño Modoki, or Interdecadal Pacific Oscillation (IPO). The CTM, the second empirical orthogonal function mode of the sea surface temperature anomalies (SSTA) in the tropical Pacific, represents a strong long‐term trend of tropical Pacific background state under global warming. According to the Gill‐Matsuno theory, the easterly winds over the western equatorial Pacific are induced by the equatorial Pacific cooling and warming SSTA associated with the CTM, while the westerly winds over the eastern equatorial Pacific is primarily due to the eastern equatorial Pacific cooling SSTA associated with the CTM. Ultimately, an alternative explanation of past and future changes of the trades is expected to lead to improved understanding of the global climatic impacts of the enhanced trades in tropical Pacific under global warming.

Từ khóa


Tài liệu tham khảo

10.1175/1520-0442(2004)017<2399:NAAOE>2.0.CO;2

10.1029/2006JC003798

10.1002/grl.50382

10.1175/1520-0469(1989)046<1687:IVIATA>2.0.CO;2

10.1175/1520-0493(1969)097<0163:ATFTEP>2.3.CO;2

10.1002/2014GL060257

10.1175/1520-0442(1999)012<1990:TENOSD>2.0.CO;2

10.1126/science.275.5302.957

10.1038/ngeo2399

10.1175/1520-0442(1996)009<2190:AODT>2.0.CO;2

10.1002/2017GL074622

10.1038/ngeo868

10.1175/2009JCLI2735.1

10.1002/qj.776

10.1175/2009JCLI2982.1

10.1007/s00382-014-2303-5

10.1002/2014JD022221

10.1002/2013JD021395

10.1175/JCLI-D-13-00359.1

10.1038/nclimate2106

10.1029/2010JD015160

10.1175/JCLI-D-12-00298.1

10.1175/JCLI-D-14-00334.1

10.1029/2010JC006695

10.1002/qj.49710644905

10.2151/jmsj.81.533

10.1175/JCLI3990.1

10.1007/s00382-015-2525-1

10.1175/1520-0469(1997)054<0811:AEORPF>2.0.CO;2

10.1175/1520-0469(1997)054<0830:AEORPF>2.0.CO;2

10.1029/2002GL016356

10.1175/2008JCLI2309.1

10.1002/grl.51007

10.1175/2009JCLI2936.1

10.1038/nature12534

10.1175/2008JCLI2624.1

10.1029/2005GL022738

10.1007/s00382-018-4194-3

10.1038/nclimate1840

10.1007/s00704-011-0463-3

10.1002/joc.2328

Li J. P., 2013, Progress in air‐land‐sea interactions in Asia and their role in global and Asian climate change (in Chinese), Chinese Journal of Atmospheric Sciences, 37, 518

10.1002/2013GL057877

10.1007/s00382-008-0465-8

10.1175/JCLI-D-11-00613.1

10.1002/2017JC013052

10.1002/2015JC010814

10.1002/2014GL059989

10.1175/JCLI-D-15-0398.1

10.2151/jmsj1965.44.1_25

10.1029/2011GL048275

10.1007/s00382-011-1047-8

10.1029/2011JD017187

10.1175/JCLI-D-15-0556.1

10.1029/2012JC008031

10.1029/2002JD002670

10.1029/2010GL046031

10.1175/JCLI-D-12-00601.1

10.2151/jmsj.2013-608

10.1007/s00382-014-2135-3

10.1175/1520-0442(1997)010<0521:ODTAAR>2.0.CO;2

10.1080/01621459.1968.10480934

10.1007/s00382-012-1484-z

10.1038/nclimate1591

10.1175/1520-0469(1988)045<3283:ADAOFE>2.0.CO;2

10.1126/science.272.5265.1148

10.1038/nclimate2996

10.1029/2011GL047364

Theil H., 1950, A rank‐invariant method of linear and polynomial regression analysis, Proc. Kon. Ned. Adad. V. Wetensch. A, 53, 386

10.1038/19505

10.1175/1520-0477(1997)078<2771:TDOENO>2.0.CO;2

10.1002/2013EF000165

10.1029/95GL03602

10.1029/2008EO090002

10.1038/nature04744

10.1175/JCLI3896.1

10.1007/s00382-011-1266-z

10.1088/1748-9326/11/12/124026

10.1088/1748-9326/aa9005

10.1175/JCLI-D-15-0825.1

Xing N., 2014, Response of the tropical atmosphere to isolated equatorially asymmetric heating, Chinese Journal of Atmospheric Sciences, 38, 1147

10.1002/2014JC009979

10.1007/s00703-017-0556-3

10.1175/JCLI-D-16-0434.1

10.1038/nature08316

10.1175/JCLI-D-16-0349.1

10.2151/jmsj.2011-510

10.1002/2014GL060130

10.1175/JCLI-D-12-00851.1

10.1029/2010JC006501

10.1175/JCLI-D-17-0815.1

10.1002/2014GL062125

10.1002/2016GL071636

10.1002/joc.5262

10.1175/JCLI-D-15-0170.1

10.1175/JCLI-D-14-00515.1