The Interannual Variations of Summer Precipitation in the Northern Indian Ocean Associated with ENSO
Using rainfall data from the Global Precipita- tion Climatology Project （GPCP）, NOAA extended reconstruction sea surface temperature （ERSST）, and NCEP/NCAR reanalysis, this study investigates the interannual variation of summer rainfall southwest of the Indian Peninsula and the northeastern Bay of B...
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| container_title | Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao |
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| creator | Ya-Li, Yang Du, Yan Yan-Ling, Wu Huang, Gang Yong-Sheng, Zhang |
| description | Using rainfall data from the Global Precipita- tion Climatology Project （GPCP）, NOAA extended reconstruction sea surface temperature （ERSST）, and NCEP/NCAR reanalysis, this study investigates the interannual variation of summer rainfall southwest of the Indian Peninsula and the northeastern Bay of Bengal associated with ENSO. The composite study indicates a decreased summer rainfall southwest of the Indian Penin- sula and an increase in the northeastern Bay of Bengal during the developing phase, but vice versa during the decay phase of E1 Nifio. Further regression analysis dem- onstrates that abnormal rainfall in the above two regions is controlled by different mechanisms. Southwest of the Indian Peninsula, the precipitation anomaly is related to local convection and water vapor flux in the decay phase of E1 Nifio. The anomalous cyclone circulation at the lower troposphere helps strengthen rainfall. In the northeastern Bay of Bengal, the anomalous rainfall depends on the strength of the Indian southwest summer monsoon （ISSM）. A strong/weak ISSM in the developing/decay phase of E1 Nifio can bring more/less water vapor to strengthen/weaken the local summer precipitation. |
| doi_str_mv | 10.1080/16742834.2012.11447014 |
| format | Article |
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The composite study indicates a decreased summer rainfall southwest of the Indian Penin- sula and an increase in the northeastern Bay of Bengal during the developing phase, but vice versa during the decay phase of E1 Nifio. Further regression analysis dem- onstrates that abnormal rainfall in the above two regions is controlled by different mechanisms. Southwest of the Indian Peninsula, the precipitation anomaly is related to local convection and water vapor flux in the decay phase of E1 Nifio. The anomalous cyclone circulation at the lower troposphere helps strengthen rainfall. In the northeastern Bay of Bengal, the anomalous rainfall depends on the strength of the Indian southwest summer monsoon （ISSM）. A strong/weak ISSM in the developing/decay phase of E1 Nifio can bring more/less water vapor to strengthen/weaken the local summer precipitation.</description><identifier>ISSN: 1674-2834</identifier><identifier>EISSN: 2376-6123</identifier><identifier>DOI: 10.1080/16742834.2012.11447014</identifier><language>eng</language><publisher>Beijing: Routledge</publisher><subject>Atmospheric precipitations ; Climatology ; Convection ; Cyclones ; Decay ; El Nino ; El Nino phenomena ; ENSO ; Hydrologic data ; Indian summer monsoon ; interannual variability ; Precipitation ; Rain ; Rainfall ; Regression analysis ; Sea surface ; Sea surface temperature ; Southern Oscillation ; Summer ; Troposphere ; Water vapor ; Water vapour ; 北印度洋 ; 夏季降水 ; 夏季降雨 ; 孟加拉湾 ; 年际变化 ; 西南季风 ; 降水异常</subject><ispartof>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2012, Vol.5 (4), p.301-305</ispartof><rights>Institute of Atmospheric Physics, Chinese Academy of Sciences 2012</rights><rights>Institute of Atmospheric Physics, Chinese Academy of Sciences. 2012</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c415t-8e8f35fb435e6934024c18483f365ee01758ff9fe9859ae44973af88c01eb1803</citedby><cites>FETCH-LOGICAL-c415t-8e8f35fb435e6934024c18483f365ee01758ff9fe9859ae44973af88c01eb1803</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/89435X/89435X.jpg</thumbnail><linktopdf>$$Uhttps://www.tandfonline.com/doi/pdf/10.1080/16742834.2012.11447014$$EPDF$$P50$$Ginformaworld$$H</linktopdf><linktohtml>$$Uhttps://www.tandfonline.com/doi/full/10.1080/16742834.2012.11447014$$EHTML$$P50$$Ginformaworld$$H</linktohtml><link.rule.ids>314,776,780,4010,27479,27900,27901,27902,59116,59117</link.rule.ids><linktorsrc>$$Uhttps://www.tandfonline.com/doi/abs/10.1080/16742834.2012.11447014$$EView_record_in_Taylor_&_Francis$$FView_record_in_$$GTaylor_&_Francis</linktorsrc></links><search><creatorcontrib>Ya-Li, Yang</creatorcontrib><creatorcontrib>Du, Yan</creatorcontrib><creatorcontrib>Yan-Ling, Wu</creatorcontrib><creatorcontrib>Huang, Gang</creatorcontrib><creatorcontrib>Yong-Sheng, Zhang</creatorcontrib><title>The Interannual Variations of Summer Precipitation in the Northern Indian Ocean Associated with ENSO</title><title>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao</title><addtitle>Atmospheric and Oceanic Science Letters</addtitle><description>Using rainfall data from the Global Precipita- tion Climatology Project （GPCP）, NOAA extended reconstruction sea surface temperature （ERSST）, and NCEP/NCAR reanalysis, this study investigates the interannual variation of summer rainfall southwest of the Indian Peninsula and the northeastern Bay of Bengal associated with ENSO. The composite study indicates a decreased summer rainfall southwest of the Indian Penin- sula and an increase in the northeastern Bay of Bengal during the developing phase, but vice versa during the decay phase of E1 Nifio. Further regression analysis dem- onstrates that abnormal rainfall in the above two regions is controlled by different mechanisms. Southwest of the Indian Peninsula, the precipitation anomaly is related to local convection and water vapor flux in the decay phase of E1 Nifio. The anomalous cyclone circulation at the lower troposphere helps strengthen rainfall. In the northeastern Bay of Bengal, the anomalous rainfall depends on the strength of the Indian southwest summer monsoon （ISSM）. A strong/weak ISSM in the developing/decay phase of E1 Nifio can bring more/less water vapor to strengthen/weaken the local summer precipitation.</description><subject>Atmospheric precipitations</subject><subject>Climatology</subject><subject>Convection</subject><subject>Cyclones</subject><subject>Decay</subject><subject>El Nino</subject><subject>El Nino phenomena</subject><subject>ENSO</subject><subject>Hydrologic data</subject><subject>Indian summer monsoon</subject><subject>interannual variability</subject><subject>Precipitation</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Regression analysis</subject><subject>Sea surface</subject><subject>Sea surface temperature</subject><subject>Southern Oscillation</subject><subject>Summer</subject><subject>Troposphere</subject><subject>Water vapor</subject><subject>Water vapour</subject><subject>北印度洋</subject><subject>夏季降水</subject><subject>夏季降雨</subject><subject>孟加拉湾</subject><subject>年际变化</subject><subject>西南季风</subject><subject>降水异常</subject><issn>1674-2834</issn><issn>2376-6123</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2012</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>BENPR</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqFkE1rwjAYx8PYYOL8CiNj57q8tU2PIm4TRAe6XUNsE420iSaV4bdfOnXXXZ7_4fm_wA-AR4yGGHH0grOcEU7ZkCBMhhgzliPMbkCP0DxLMkzoLeh1pqRz3YNBCDuEEKYkyxHtgWq1VXBqW-WltUdZwy_pjWyNswE6DZfHplEefnhVmr1pfx_QWNjG1Nz5KN7GeGWkhYtSxTsKwZWxQVXw27RbOJkvFw_gTss6qMFF--DzdbIavyezxdt0PJolJcNpm3DFNU31mtFUZQVliLASc8applmqFMJ5yrUutCp4WkjFWJFTqTkvEVZrzBHtg-dz7967w1GFVuzc0ds4KQjBKaFFLIuu7OwqvQvBKy323jTSnwRGooMqrlBFB1Vcocbg6Bw0VjvfyG_n60q08lQ7ryO_0gRB_-14uoxvnd0cjN38rTOSI0Q4oT-kE4gH</recordid><startdate>2012</startdate><enddate>2012</enddate><creator>Ya-Li, Yang</creator><creator>Du, Yan</creator><creator>Yan-Ling, Wu</creator><creator>Huang, Gang</creator><creator>Yong-Sheng, Zhang</creator><general>Routledge</general><general>KeAi Publishing Communications Ltd</general><scope>2RA</scope><scope>92L</scope><scope>CQIGP</scope><scope>W94</scope><scope>~WA</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TN</scope><scope>7XB</scope><scope>8FK</scope><scope>8G5</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H96</scope><scope>HCIFZ</scope><scope>L.G</scope><scope>M2O</scope><scope>MBDVC</scope><scope>PCBAR</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><scope>Q9U</scope></search><sort><creationdate>2012</creationdate><title>The Interannual Variations of Summer Precipitation in the Northern Indian Ocean Associated with ENSO</title><author>Ya-Li, Yang ; Du, Yan ; Yan-Ling, Wu ; Huang, Gang ; Yong-Sheng, Zhang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c415t-8e8f35fb435e6934024c18483f365ee01758ff9fe9859ae44973af88c01eb1803</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2012</creationdate><topic>Atmospheric precipitations</topic><topic>Climatology</topic><topic>Convection</topic><topic>Cyclones</topic><topic>Decay</topic><topic>El Nino</topic><topic>El Nino phenomena</topic><topic>ENSO</topic><topic>Hydrologic data</topic><topic>Indian summer monsoon</topic><topic>interannual variability</topic><topic>Precipitation</topic><topic>Rain</topic><topic>Rainfall</topic><topic>Regression analysis</topic><topic>Sea surface</topic><topic>Sea surface temperature</topic><topic>Southern Oscillation</topic><topic>Summer</topic><topic>Troposphere</topic><topic>Water vapor</topic><topic>Water vapour</topic><topic>北印度洋</topic><topic>夏季降水</topic><topic>夏季降雨</topic><topic>孟加拉湾</topic><topic>年际变化</topic><topic>西南季风</topic><topic>降水异常</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Ya-Li, Yang</creatorcontrib><creatorcontrib>Du, Yan</creatorcontrib><creatorcontrib>Yan-Ling, Wu</creatorcontrib><creatorcontrib>Huang, Gang</creatorcontrib><creatorcontrib>Yong-Sheng, Zhang</creatorcontrib><collection>中文科技期刊数据库</collection><collection>中文科技期刊数据库-CALIS站点</collection><collection>中文科技期刊数据库-7.0平台</collection><collection>中文科技期刊数据库-自然科学</collection><collection>中文科技期刊数据库- 镜像站点</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Oceanic Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest One Sustainability</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>Research Library</collection><collection>Research Library (Corporate)</collection><collection>Earth, Atmospheric & Aquatic Science Database</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><collection>ProQuest Central Basic</collection><jtitle>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext_linktorsrc</fulltext></delivery><addata><au>Ya-Li, Yang</au><au>Du, Yan</au><au>Yan-Ling, Wu</au><au>Huang, Gang</au><au>Yong-Sheng, Zhang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>The Interannual Variations of Summer Precipitation in the Northern Indian Ocean Associated with ENSO</atitle><jtitle>Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao</jtitle><addtitle>Atmospheric and Oceanic Science Letters</addtitle><date>2012</date><risdate>2012</risdate><volume>5</volume><issue>4</issue><spage>301</spage><epage>305</epage><pages>301-305</pages><issn>1674-2834</issn><eissn>2376-6123</eissn><abstract>Using rainfall data from the Global Precipita- tion Climatology Project （GPCP）, NOAA extended reconstruction sea surface temperature （ERSST）, and NCEP/NCAR reanalysis, this study investigates the interannual variation of summer rainfall southwest of the Indian Peninsula and the northeastern Bay of Bengal associated with ENSO. The composite study indicates a decreased summer rainfall southwest of the Indian Penin- sula and an increase in the northeastern Bay of Bengal during the developing phase, but vice versa during the decay phase of E1 Nifio. Further regression analysis dem- onstrates that abnormal rainfall in the above two regions is controlled by different mechanisms. Southwest of the Indian Peninsula, the precipitation anomaly is related to local convection and water vapor flux in the decay phase of E1 Nifio. The anomalous cyclone circulation at the lower troposphere helps strengthen rainfall. In the northeastern Bay of Bengal, the anomalous rainfall depends on the strength of the Indian southwest summer monsoon （ISSM）. A strong/weak ISSM in the developing/decay phase of E1 Nifio can bring more/less water vapor to strengthen/weaken the local summer precipitation.</abstract><cop>Beijing</cop><pub>Routledge</pub><doi>10.1080/16742834.2012.11447014</doi><tpages>5</tpages><oa>free_for_read</oa></addata></record> |
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| identifier | ISSN: 1674-2834 |
| ispartof | Atmospheric and oceanic science letters = Daqi-he-haiyang-kexue-kuaibao, 2012, Vol.5 (4), p.301-305 |
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| language | eng |
| recordid | cdi_crossref_primary_10_1080_16742834_2012_11447014 |
| source | Taylor & Francis Open Access |
| subjects | Atmospheric precipitations Climatology Convection Cyclones Decay El Nino El Nino phenomena ENSO Hydrologic data Indian summer monsoon interannual variability Precipitation Rain Rainfall Regression analysis Sea surface Sea surface temperature Southern Oscillation Summer Troposphere Water vapor Water vapour 北印度洋 夏季降水 夏季降雨 孟加拉湾 年际变化 西南季风 降水异常 |
| title | The Interannual Variations of Summer Precipitation in the Northern Indian Ocean Associated with ENSO |
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