| 两广地区夏季降水异常与澳大利亚东侧海温异常的联系及可能机制 |
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| 引用本文： | 霍利微,张福颖,王易.两广地区夏季降水异常与澳大利亚东侧海温异常的联系及可能机制[J].大气科学学报,2018,41(2):220-227. |
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| 作者姓名： | 霍利微 张福颖 王易 |
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| 作者单位： | 南京信息工程大学气象灾害教育部重点实验室/气象灾害预报预警与评估协同创新中心;江苏省气象台 |
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| 基金项目： | 江苏省气象局2017年面上项目（KM201702）；江苏省自然科学基金资助项目（BK20160956）；南京信息工程大学人才启动项目（2015r035；2014r006） |
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| 摘 要： | 广东省和广西壮族自治区(两广地区)夏季降水时空分布很不均匀,存在显著的年际变化。利用站点观测降水资料、海洋及大气再分析资料,研究了近40 a两广地区夏季降水年际异常与澳大利亚东侧海温异常的联系及机理。在年际时间尺度上,两广夏季降水异常与澳大利亚东侧的海温异常存在显著的负相关关系。当澳大利亚东侧海温异常偏高时,一方面,部分水汽由热带中太平洋向澳大利亚东侧海区辐合,部分沿西太平洋副热带高压边缘向东亚地区输送,两广地区为水汽辐散区域,另一方面,澳大利亚东侧海区的对流活动增强,该地区上空的上升运动异常增强,通过"大气桥"遥相关使得海洋性大陆地区的异常上升运动增强,从而加强了东亚地区的局地Hadley环流,使得两广地区下沉运动增强,二者共同作用致使两广地区夏季干旱少雨;反之亦然。
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| 关 键 词： | 两广地区 夏季降水 澳大利亚东侧 海温异常 年际变化 |
| 收稿时间： | 2016/7/7 0:00:00 |
| 修稿时间： | 2016/12/20 0:00:00 |
Connections of summer anomalous precipitation in Guangdong and Guangxi regions with SST anomalies east of Australia and associated mechanism |
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| HUO Liwei,ZHANG Fuying and WANG Yi.Connections of summer anomalous precipitation in Guangdong and Guangxi regions with SST anomalies east of Australia and associated mechanism[J].大气科学学报,2018,41(2):220-227. |
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| Authors: | HUO Liwei ZHANG Fuying and WANG Yi |
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| Institution: | Key Laboratory of Meteorological Disaster, Ministry of Education(KLME)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Diasters(CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, China;Key Laboratory of Meteorological Disaster, Ministry of Education(KLME)/Collaborative Innovation Center on Forecast and Evaluation of Meteorological Diasters(CIC-FEMD), Nanjing University of Information Science & Technology, Nanjing 210044, China;Jiangsu Meteorological Observatory, Nanjing 210008, China |
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| Abstract: | The summer precipitation in Guangdong Province and Guangxi Zhuang Autonomous Region(hereafter GG region) with uneven temporal-spatial distribution has significant interannual variability.Using the observational station precipitation data,the marine and atmospheric reanalysis data,connections between precipitation(PGG) anomaly in GG region and sea surface temperature(SST) anomaly east of Australia during boreal summer in recent 40 years are investigated.Results show that PGG has a significant negative correlation with SST anomaly east of Australia on the interannual time scale.On the one hand,during the period of positive SST anomaly east of Australia,part of water vapor from the tropical central Pacific converges east of Australia,and another part of water vapor transfers to East Asia along the edge of western Pacific subtropical high.The anomalous moisture divergence is found over GG region.On the other hand,accompanied by the enhancement of convection east of Australia,the anomalous ascending is strengthened.Through the "Atmospheric Bridge" teleconnection,anomalous ascending is enhanced in the Maritime Continent,which strengthens the local Hadley circulation in East Asia and the anomalous descending in GG region.The water vapor transport and atmospheric circulation anomalies during the period of positive SST anomaly east of Australia are unfavorable to PGG,and vice versa. |
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| Keywords: | Guangdong and Guangxi provinces summer precipitation east of Australia sea surface temperature anomaly interannual variability |
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