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2020年夏秋季北部湾SST异常特征及可能成因分析
作者:姚小娟1 2  张海燕1 2  李希茜1 2 
单位:1. 国家海洋局南海预报中心, 广东 广州 510300;
2. 自然资源部海洋环境探测技术与应用重点实验室, 广东 广州 510300
关键词:北部湾 海表温度异常 西太平洋副高 西北太平洋反气旋 厄尔尼诺 热带印度洋全区一致海温模态 全球气候变暖 
分类号:P731.11
出版年·卷·期(页码):2022·39·第四期(79-90)
摘要:
利用MISST海温资料、表层海温实测资料和ERA5再分析资料等,采用天气动力学分析方法,重点对2020年夏秋季北部湾海表温度异常特征及大尺度环流成因进行分析。结果表明:2020年夏秋季北部湾海域SST持续异常偏高,平均SST为历史同期最高。北部湾SST异常偏高与夏秋季西北太平洋大尺度大气环流异常密切相关,2020年夏秋季西太平洋副热带高压持续异常偏强偏西,低层异常反气旋环流长期维持在南海北部,北部湾下沉气流持续偏强,为北部湾SST持续异常偏高提供极为有利的大气环流条件。在全球气候变暖背景下,受前期中部型厄尔尼诺衰减与热带印度洋全区一致海温模态持续异常偏暖影响,2020年夏秋季西北太平洋反气旋持续偏强,使北部湾长期处于西太平洋副高控制下,加剧了北部湾SST异常增暖。
Using the Multi-sensor Improved Sea Surface Temperature (MISST) dataset, the in-situ sea surface temperature (SST) observation and the fifth generation ECMWF reanalysis for the global climate and weather (ERA5) reanalysis dataset, the characteristics of SST anomaly in Beibu Gulf and the possible causes of largescale circulation in the summer and autumn of 2020 are analyzed based on synoptic dynamics analyze method. The results show that the SST in Beibu Gulf in the summer and autumn of 2020 remains abnormally high, and the average SST is the highest in history during the same period. The abnormally high SST in Beibu Gulf is closely related to the large-scale atmospheric circulation anomaly in the northwest Pacific Ocean in summer and autumn. In the summer and autumn of 2020, the western Pacific subtropical high (WPSH) is abnormally stronger and tilts to the westward. The low-level anomalous anticyclonic circulation maintains in the northern South China Sea, and the downdraft in Beibu Gulf is constantly stronger, providing extremely favorable atmospheric circulation conditions for the persistent abnormally high SST in Beibu Gulf. In the context of global climate warming and under the influence of the decaying of CP-El Nino event and the persistent abnormally warm of the Indian Ocean basin warming mode (IOBW) in the tropical Indian Ocean, the anticyclones in the northwest Pacific Ocean continues to be stronger in the summer and autumn of 2020, which causes Beibu Gulf under the control of WPSH for a long period, and aggravates the abnormally high SST in Beibu Gulf.
参考文献:
[1] 于文泉.南海北部海面水温场的分析[J].海洋预报, 1987, 4(1):61-67. YU W Q. Analysis of sea surface temperature field for the northern South China Sea[J]. Marine Forecasts, 1987, 4(1):61-67.
[2] 樊博文,雷洁霞,樊彦国.基于GIS的南海海温时空过程分析研究[J].海洋科学, 2018, 42(4):36-42. FAN B W, LEI J X, FAN Y G. Study of spatial and temporal processes of sea temperature in the South China Sea based on GIS[J]. Marine Sciences, 2018, 42(4):36-42.
[3] 朱秀华,王卫强,周伟东,等.南海海面温度的年际模态及其与季风强迫的关系[J].热带海洋学报, 2003,22(4):42-50. ZHU X H, WANG W Q, ZHOU W D, et al. Interannual mode of sea surface temperature in relation to monsoon forcing in South China Sea[J]. Journal of Tropical Oceanography, 2003, 22(4):42-50.
[4] CHEN J M, LI T, SHIH C F. Fall persistence barrier of sea surface temperature in the South China sea associated with ENSO[J]. Journal of Climate, 2007, 20(2):158-172.
[5] 曾强,张耀存.西南季风爆发前后南海SST变化特征及影响因子分析[J].热带气象学报, 2008, 24(1):44-50. ZENG Q, ZHANG Y C. An analysis of SST variation during South China Sea Monsoon onset period in South China Sea[J]. Journal of Tropical Meteorology, 2008, 24(1):44-50.
[6] 梁卫,温之平,李秀珍,等.南海夏季风爆发前后南海海温之演变特征[J].热带气象学报, 2009, 25(S1):85-91. LIANG W, WEN Z P, LI X Z, et al. An analysis of SST variation during South China Sea Monsoon onset period in South China Sea[J]. Journal of Tropical Meteorology, 2009, 25(S1):85-91.
[7] WANG C Z, WANG W Q, WANG D X, et al. Interannual variability of the South China Sea associated with El Niño[J]. Journal of Geophysical Research Oceans, 2006, 111(C3):C03023, doi:10.1029/2005JC003333.
[8] TAN W, WANG X, WANG W Q, et al. Different responses of sea surface temperature in the South China Sea to various El Niño events during boreal Autumn[J]. Journal of Climate, 2016, 29(3):1127-1142.
[9] 罗琳,王东晓,刘赟,等.北部湾温度锋的季节与年际变化[J].热带海洋学报, 2003, 22(4):60-67. LUO L, WANG D X, LIU Y, et al. Seasonal and interannual variabilities of thermal fronts in Beibu Gulf, South China Sea[J]. Journal of Tropical Oceanography, 2003, 22(4):60-67.
[10] 牙韩争,高劲松,董德信.北部湾海表面温度变化特征及其影响因素分析[J].广西科学, 2015, 22(3):260-265. YA H Z, GAO J S, DONG D X. Analysis of variation characteristics and driving factors of sea surface temperature in Beibu Gulf[J]. Guangxi Sciences, 2015, 22(3):260-265.
[11] GODFREY S P. Surface fluxes and mixed layer heat and freshwater budgets in TOGA COARE[C]//Proc. Int. Scientific Conf. on the Tropical Ocean Global Atmosphere Program, Melbourne, Australia, World Meteorological Organization, 1995:464-468.
[12] SUI C H, LI X, LAU K M, et al. Multiscale air-sea interactions during TOGA COARE[J]. Monthly Weather Review, 1997, 125(4):448-462.
[13] KLEIN S A, SODEN B J, LAU N C. Remote sea surface temperature variations during ENSO:Evidence for a tropical atmospheric bridge[J]. Journal of Climate, 1999, 12(4):917-932.
[14] WANG B, WU R G, FU X H. Pacific-East Asian teleconnection:How does ENSO affect East Asian climate?[J]. Journal of Climate, 2000, 13(9):1517-1536.
[15] XIE S P, HU K M, HAFNER J, et al. Indian Ocean capacitor effect on Indo-western Pacific climate during the summer following El Niño[J]. Journal of Climate, 2009, 22(3):730-747.
[16] JIANG X W, YANG S, LI J P, et al. Variability of the Indian Ocean SST and its possible impact on summer western North Pacific anticyclone in the NCEP climate forecast system[J]. Climate Dynamics, 2013, 41(7-8):2199-2212.
[17] XIE S P, XIE Q, WANG D, et al. Summer upwelling in the South China Sea and its role in regional climate variations[J]. Journal of Geophysical Research:Oceans, 2003, 108(C8):3261.
[18] 谭军,周发琇,胡敦欣,等.南海海温异常与ENSO的相关性[J].海洋与湖沼, 1995, 26(4):377-382. TAN J, ZHOU F X, HU D X, et al. The correlation between SST anomaly in the South China Sea and ENSO[J]. Oceanologia et Limnologia Sinica, 1995, 26(4):377-382.
[19] 王银霞,隋俊鹏,曾纪胜,等.台风影响南海上层环流的统计分析研究[J].海洋预报, 2020, 37(4):15-20. WANG Y X, SUI J P, ZENG J S, et al. Influence of typhoons on the upper-layer circulation in the South China Sea[J]. Marine Forecasts, 2020, 37(4):15-20.
[20] WANG C Z, WANG X. Classifying El Niño Modoki I and II by Different Impacts on Rainfall in Southern China and Typhoon Tracks[J]. Journal of Climate, 2013, 26(4):1322-1338.
[21] WANG B, WU R G, LI T. Atmosphere-Warm Ocean Interaction and Its Impacts on Asian-Australian Monsoon Variation[J]. Journal of Climate, 2003, 16(8):1195-1211.
[22] YANG J L, LIU Q Y, XIE S P, et al. Impact of the Indian Ocean SST basin mode on the Asian summer monsoon[J]. Geophysical Research Letters, 2007, 34(2):L02708.
[23] WEISBERG R H, WANG C Z. A western pacific oscillator paradigm for the El Niño-Southern oscillation[J]. Geophysical Research Letters, 1997, 24(7):779-782.
[24] WANG C Z, WEISBERG R H, VIRMANI J I. Western pacific interannual variability associated with the El Niño-southern oscillation[J]. Journal of Geophysical Research Oceans, 1999, 104(C3):5131-5149.
[25] WANG X, WANG D X, ZHOU W, et al. Interdecadal modulation of the influence of La Niña events on Mei-Yu rainfall over the Yangtze River valley[J]. Advances in Atmospheric Sciences, 2012, 29(1):157-168.
[26] WANG X, WANG C Z. Different impacts of various El Niño events on the Indian Ocean dipole[J]. Climate Dynamics, 2014, 42(3-4):991-1005.
[27] IPCC, 2021:Summary for policymakers[M]//Masson-Delmotte V, Zhai P, Pirani A, et al. Climate Change 2021:The Physical Science Basis. Contribution of Working Group I to the Sixth Assessment Report of the Intergovernmental Panel on Climate Change. Cambridge:Cambridge University Press, 2021.
[28] 张丽萍.全球变暖背景下水循环变化对海洋环流及气候的影响[D].青岛:中国海洋大学, 2012. ZHANG L P. The impact of hydrological cycle changes on the ocean circulation and climate[D]. Qingdao:Ocean University of China, 2012.
[29] 黄雪松,黄梅丽.广西北部湾海岸带气候变化影响与适应对策[C]//中国气象局国家气候中心暨气候研究开放实验室2009年度学术年会论文集.北京:国家气候中心,中国气象局气候研究开放实验室, 2010:140-141. HUANG X S, HUANG M L. Impacts of climate change on the coastal zone of Guangxi Beibu Gulf and its adaptation countermeasures[C]//Proceedings of the 2009 Annual Academic Conference of the National Climate Center and Open Laboratory for Climate Research, China Meteorological Administration. Beijing:National Climate Center, Open Laboratory for Climate Research, China Meteorological Administration, 2010:140-141.
[30] 苏志,余纬东,黄理,等.北部湾海岸带的地理环境及其对气候的影响[J].气象研究与应用, 2009, 30(3):44-47. SU Z, YU W D, HUANG L, et al. Geographical environment of the Beibu Gulf coast and its impact on the climate[J]. Journal of Meteorological Research and Application, 2009, 30(3):44-47.
[31] 李华伟,王建华,黄建云.红河中下游流域气候变化特征分析[J].云南地理环境研究, 2011, 23(S1):1-7. LI H W, WANG J H, HUANG J Y. THe middie and lower reaches basin of Honghe climatic change characteristic analysis[J]. Yunnan Geographic Environment Research, 2011, 23(S1):1-7.
[32] 田义超,梁铭忠.北部湾沿海地区植被覆盖对气温和降水的旬响应特征[J].自然资源学报, 2016, 31(3):488-502. TIAN Y C, LIANG M Z. The NDVI characteristics of Vegetation and its ten-day response to temperature and precipitation in Beibu Gulf coastal region[J]. Journal of Natural Resources, 2016, 31(3):488-502.
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