Sea surface temperature anomalies in the South China Sea during mature phase of ENSO
Based on the 18-year （1993-2010） National Centers for Environmental Prediction optimum interpolation sea surface temperature （SST） and simple ocean data assimilation datasets, this study investigated the patterns of the SST anomalies （SSTAs） that occurred in the South China Sea （SCS） during the matu...
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| Published in | Chinese journal of oceanology and limnology Vol. 34; no. 3; pp. 577 - 584 |
|---|---|
| Main Author | |
| Format | Journal Article |
| Language | English |
| Published |
Heidelberg
Science Press
01.05.2016
Springer Nature B.V |
| Subjects | |
| Online Access | Get full text |
| ISSN | 0254-4059 2096-5508 1993-5005 2523-3521 |
| DOI | 10.1007/s00343-016-4290-3 |
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| Abstract | Based on the 18-year （1993-2010） National Centers for Environmental Prediction optimum interpolation sea surface temperature （SST） and simple ocean data assimilation datasets, this study investigated the patterns of the SST anomalies （SSTAs） that occurred in the South China Sea （SCS） during the mature phase of the E1 Nifio/Southem Oscillation. The most dominant characteristic was that of the out- of-phase variation between southwestern and northeastern parts of the SCS, which was influenced primarily by the net surface heat flux and by horizontal thermal advection. The negative SSTA in the northeastern SCS was caused mainly by the loss of heat to the atmosphere and because of the cold-water advection from the western Pacific through the Luzon Strait during E1 Nifio episodes. Conversely, it was found that the anomalous large-scale atmospheric circulation and weakened western boundary current during E1 Nifio episodes led to the development of the positive SSTA in the southwestern SCS. |
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| AbstractList | Based on the 18-year (1993–2010) National Centers for Environmental Prediction optimum interpolation sea surface temperature (SST) and simple ocean data assimilation datasets, this study investigated the patterns of the SST anomalies (SSTAs) that occurred in the South China Sea (SCS) during the mature phase of the El Niño/Southern Oscillation. The most dominant characteristic was that of the outof-phase variation between southwestern and northeastern parts of the SCS, which was influenced primarily by the net surface heat flux and by horizontal thermal advection. The negative SSTA in the northeastern SCS was caused mainly by the loss of heat to the atmosphere and because of the cold-water advection from the western Pacific through the Luzon Strait during El Niño episodes. Conversely, it was found that the anomalous large-scale atmospheric circulation and weakened western boundary current during El Niño episodes led to the development of the positive SSTA in the southwestern SCS. Based on the 18-year （1993-2010） National Centers for Environmental Prediction optimum interpolation sea surface temperature （SST） and simple ocean data assimilation datasets, this study investigated the patterns of the SST anomalies （SSTAs） that occurred in the South China Sea （SCS） during the mature phase of the E1 Nifio/Southem Oscillation. The most dominant characteristic was that of the out- of-phase variation between southwestern and northeastern parts of the SCS, which was influenced primarily by the net surface heat flux and by horizontal thermal advection. The negative SSTA in the northeastern SCS was caused mainly by the loss of heat to the atmosphere and because of the cold-water advection from the western Pacific through the Luzon Strait during E1 Nifio episodes. Conversely, it was found that the anomalous large-scale atmospheric circulation and weakened western boundary current during E1 Nifio episodes led to the development of the positive SSTA in the southwestern SCS. Based on the 18-year (1993-2010) National Centers for Environmental Prediction optimum interpolation sea surface temperature (SST) and simple ocean data assimilation datasets, this study investigated the patterns of the SST anomalies (SSTAs) that occurred in the South China Sea (SCS) during the mature phase of the El Nino/Southern Oscillation. The most dominant characteristic was that of the outof-phase variation between southwestern and northeastern parts of the SCS, which was influenced primarily by the net surface heat flux and by horizontal thermal advection. The negative SSTA in the northeastern SCS was caused mainly by the loss of heat to the atmosphere and because of the cold-water advection from the western Pacific through the Luzon Strait during El Nino episodes. Conversely, it was found that the anomalous large-scale atmospheric circulation and weakened western boundary current during El Nino episodes led to the development of the positive SSTA in the southwestern SCS. |
| Author | 丘福文 潘爱军 张善武 查晶 孙豪为 |
| AuthorAffiliation | Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China |
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| CitedBy_id | crossref_primary_10_1029_2019JC015405 crossref_primary_10_1007_s00343_018_7013_0 crossref_primary_10_1007_s11160_025_09927_w crossref_primary_10_3390_jmse11122360 crossref_primary_10_1016_j_jmarsys_2022_103799 crossref_primary_10_3389_fmars_2023_1234772 crossref_primary_10_1007_s00382_021_05968_6 crossref_primary_10_1007_s13131_019_1496_1 |
| Cites_doi | 10.1080/0143116042000192376 10.1175/1520-0477(1996)077<0437:TNYRP>2.0.CO;2 10.1016/j.dynatmoce.2010.07.002 10.1016/j.dsr.2009.03.008 10.1007/s11802-013-2169-x 10.1175/1520-0442(2000)013<1517:PEATHD>2.0.CO;2 10.5194/adgeo-14-219-2008 10.1175/2007MWR1978.1 10.1175/1520-0442(2004)017<3644:CLSTPA>2.0.CO;2 10.1175/2008JCLI2590.1 10.1175/1520-0442(1999)012<0917:RSSTVD>2.0.CO;2 10.1175/1520-0442(1994)007<0929:IGSSTA>2.0.CO;2 10.1016/j.jmarsys.2012.03.010 10.1016/S0079-6611(96)00010-9 10.1029/2003JC002179 10.1029/2003JC001867 10.1016/j.gloplacha.2006.08.001 10.1175/1520-0485(2000)030<0311:ASODAA>2.0.CO;2 10.1029/2005JC003276 10.1029/97JC00982 10.1175/2008JCLI2544.1 10.1002/2013JD021095 |
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| Notes | Based on the 18-year （1993-2010） National Centers for Environmental Prediction optimum interpolation sea surface temperature （SST） and simple ocean data assimilation datasets, this study investigated the patterns of the SST anomalies （SSTAs） that occurred in the South China Sea （SCS） during the mature phase of the E1 Nifio/Southem Oscillation. The most dominant characteristic was that of the out- of-phase variation between southwestern and northeastern parts of the SCS, which was influenced primarily by the net surface heat flux and by horizontal thermal advection. The negative SSTA in the northeastern SCS was caused mainly by the loss of heat to the atmosphere and because of the cold-water advection from the western Pacific through the Luzon Strait during E1 Nifio episodes. Conversely, it was found that the anomalous large-scale atmospheric circulation and weakened western boundary current during E1 Nifio episodes led to the development of the positive SSTA in the southwestern SCS. sea surface temperature （SST）; anomalies; E1 Nifio/Southern Oscillation （ENSO）; South China Sea （SCS） 37-1150/P QIU Fuwen, PAN Aijun, ZHANG Shanwu,CHA Jing, SUN Haowei （Third Institute of Oceanography, State Oceanic Administration, Xiamen 361005, China） ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14 content type line 23 |
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| PublicationTitle | Chinese journal of oceanology and limnology |
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| PublicationYear | 2016 |
| Publisher | Science Press Springer Nature B.V |
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| SubjectTerms | Advection Anomalies Atmospheric circulation Data assimilation Data collection Earth and Environmental Science Earth Sciences El Nino El Nino phenomena ENSO Heat flux Heat transfer Interpolation Marine Oceanography Oceans Phase variations Philippines Physics prediction Sea surface Sea surface temperature South China Sea Southern Oscillation Surface temperature surface water temperature Temperature Temperature anomalies Water temperature 南中国海 南海东北部 厄尔尼诺事件 大气环流异常 成熟阶段 海表温度异常 海表面温度 |
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| Title | Sea surface temperature anomalies in the South China Sea during mature phase of ENSO |
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