Respective impacts of the East Asian winter monsoon and ENSO on winter rainfall in China
Using station rainfall observations and the ERA‐40 reanalysis, this study investigates respective impacts of the East Asian winter monsoon (EAWM) and El Niño‐Southern Oscillation (ENSO) on winter (November–March) rainfall in China by removing the interdependence between the EAWM and ENSO using a lin...
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| Veröffentlicht in: | Journal of Geophysical Research. B. Solid Earth 2010-01, Vol.115 (D2), p.n/a |
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| creator | Zhou, Lian-Tong Wu, Renguang |
| description | Using station rainfall observations and the ERA‐40 reanalysis, this study investigates respective impacts of the East Asian winter monsoon (EAWM) and El Niño‐Southern Oscillation (ENSO) on winter (November–March) rainfall in China by removing the interdependence between the EAWM and ENSO using a linear regression. It is found that circulation and temperature anomalies over the tropics and midlatitude North Pacific are mainly induced by ENSO, and those over the midlatitude Asia are closely linked to the EAWM. The warm ENSO induced lower‐level southwesterly winds deflect from the southeast coast of China, and thus, the influence of ENSO on winter rainfall is mainly in southern China. The lower‐level southerly winds associated with a weak EAWM penetrate northward over eastern China, and thus, the EAWM influences winter rainfall in eastern China. |
| doi_str_mv | 10.1029/2009JD012502 |
| format | Article |
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It is found that circulation and temperature anomalies over the tropics and midlatitude North Pacific are mainly induced by ENSO, and those over the midlatitude Asia are closely linked to the EAWM. The warm ENSO induced lower‐level southwesterly winds deflect from the southeast coast of China, and thus, the influence of ENSO on winter rainfall is mainly in southern China. The lower‐level southerly winds associated with a weak EAWM penetrate northward over eastern China, and thus, the EAWM influences winter rainfall in eastern China.</description><identifier>ISSN: 0148-0227</identifier><identifier>ISSN: 2169-897X</identifier><identifier>EISSN: 2156-2202</identifier><identifier>EISSN: 2169-8996</identifier><identifier>DOI: 10.1029/2009JD012502</identifier><language>eng</language><publisher>Washington, DC: Blackwell Publishing Ltd</publisher><subject>Asian ; Atmosphere ; Atmospheric sciences ; Climate change ; Earth ; Earth sciences ; Earth, ocean, space ; EAWM ; El Nino ; ENSO ; Exact sciences and technology ; Geophysics ; Latitude ; Marine ; Monsoons ; Oscillations ; Rainfall ; Regression ; Southern Oscillation ; Stations ; Tropical environments ; Tropics ; Winter</subject><ispartof>Journal of Geophysical Research. B. 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B. Solid Earth</title><addtitle>J. Geophys. Res</addtitle><description>Using station rainfall observations and the ERA‐40 reanalysis, this study investigates respective impacts of the East Asian winter monsoon (EAWM) and El Niño‐Southern Oscillation (ENSO) on winter (November–March) rainfall in China by removing the interdependence between the EAWM and ENSO using a linear regression. It is found that circulation and temperature anomalies over the tropics and midlatitude North Pacific are mainly induced by ENSO, and those over the midlatitude Asia are closely linked to the EAWM. The warm ENSO induced lower‐level southwesterly winds deflect from the southeast coast of China, and thus, the influence of ENSO on winter rainfall is mainly in southern China. The lower‐level southerly winds associated with a weak EAWM penetrate northward over eastern China, and thus, the EAWM influences winter rainfall in eastern China.</description><subject>Asian</subject><subject>Atmosphere</subject><subject>Atmospheric sciences</subject><subject>Climate change</subject><subject>Earth</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>EAWM</subject><subject>El Nino</subject><subject>ENSO</subject><subject>Exact sciences and technology</subject><subject>Geophysics</subject><subject>Latitude</subject><subject>Marine</subject><subject>Monsoons</subject><subject>Oscillations</subject><subject>Rainfall</subject><subject>Regression</subject><subject>Southern Oscillation</subject><subject>Stations</subject><subject>Tropical environments</subject><subject>Tropics</subject><subject>Winter</subject><issn>0148-0227</issn><issn>2169-897X</issn><issn>2156-2202</issn><issn>2169-8996</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2010</creationdate><recordtype>article</recordtype><sourceid>8G5</sourceid><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><sourceid>GNUQQ</sourceid><sourceid>GUQSH</sourceid><sourceid>M2O</sourceid><recordid>eNqN0stuEzEUBuARAqlR6Y4HsJCALhiwj-_LKgmB0ovUloLYWB7Ho7pMPMGeUPr2OEoVIRah3liWv_NbPjpV9YLgdwSDfg8Y6-MJJsAxPKlGQLioATA8rUaYMFVjALlXHeR8i8tiXDBMRtW3C5-X3g3hl0dhsbRuyKhv0XDj0dTmAR3lYCO6C3HwCS36mPs-IhvnaHp2eY767VWyIba261CIaHwTon1ePSvn7A8e9v3qy4fp1fhjfXI--zQ-Oqkd10LUjFJoiOa6wVrPpZLO8XnLpGuE5pRL3syVB4WxdQ32VLdEMOeU88op37SW7ldvNrnL1P9c-TyYRcjOd52Nvl9lIznjXDOhi3y9U1LBSg85_y8EQgkhUhR4uBMSqQRRWJNH0PI4AOVYFvryH3rbr1IsTTRKYOCUASvo7Qa51OecfGuWKSxsujcEm_U8mL_nofBXD5k2O9u1yUYX8rYGgHOsyDqWbtxd6Pz9zkxzPLuYEC71-nP1pirkwf_eVtn0wwhJJTdfz2bmlJxef55cg_lO_wBkJc7M</recordid><startdate>20100126</startdate><enddate>20100126</enddate><creator>Zhou, Lian-Tong</creator><creator>Wu, Renguang</creator><general>Blackwell Publishing Ltd</general><general>American Geophysical Union</general><scope>BSCLL</scope><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>3V.</scope><scope>7TG</scope><scope>7UA</scope><scope>7XB</scope><scope>8FD</scope><scope>8FE</scope><scope>8FG</scope><scope>8FK</scope><scope>8G5</scope><scope>ABJCF</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>ARAPS</scope><scope>ATCPS</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>BGLVJ</scope><scope>BHPHI</scope><scope>BKSAR</scope><scope>C1K</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>F1W</scope><scope>FR3</scope><scope>GNUQQ</scope><scope>GUQSH</scope><scope>H8D</scope><scope>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L6V</scope><scope>L7M</scope><scope>M2O</scope><scope>M7S</scope><scope>MBDVC</scope><scope>P5Z</scope><scope>P62</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PTHSS</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>7TN</scope><scope>7SM</scope></search><sort><creationdate>20100126</creationdate><title>Respective impacts of the East Asian winter monsoon and ENSO on winter rainfall in China</title><author>Zhou, Lian-Tong ; Wu, Renguang</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c5966-4332b1959b099d787cc5df47cb6953575bd8e2800acb0e39f164cc8ce8c8ebfa3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2010</creationdate><topic>Asian</topic><topic>Atmosphere</topic><topic>Atmospheric sciences</topic><topic>Climate change</topic><topic>Earth</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>EAWM</topic><topic>El Nino</topic><topic>ENSO</topic><topic>Exact sciences and technology</topic><topic>Geophysics</topic><topic>Latitude</topic><topic>Marine</topic><topic>Monsoons</topic><topic>Oscillations</topic><topic>Rainfall</topic><topic>Regression</topic><topic>Southern Oscillation</topic><topic>Stations</topic><topic>Tropical environments</topic><topic>Tropics</topic><topic>Winter</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Zhou, Lian-Tong</creatorcontrib><creatorcontrib>Wu, Renguang</creatorcontrib><collection>Istex</collection><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>ProQuest Central (Corporate)</collection><collection>Meteorological & Geoastrophysical Abstracts</collection><collection>Water Resources Abstracts</collection><collection>ProQuest Central (purchase pre-March 2016)</collection><collection>Technology Research Database</collection><collection>ProQuest SciTech Collection</collection><collection>ProQuest Technology Collection</collection><collection>ProQuest Central (Alumni) (purchase pre-March 2016)</collection><collection>Research Library (Alumni Edition)</collection><collection>Materials Science & Engineering Collection</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>Advanced Technologies & Aerospace Collection</collection><collection>Agricultural & Environmental Science Collection</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>Technology Collection</collection><collection>Natural Science Collection</collection><collection>Earth, Atmospheric & Aquatic Science Collection</collection><collection>Environmental Sciences and Pollution Management</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>ProQuest Central Student</collection><collection>Research Library Prep</collection><collection>Aerospace Database</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>SciTech Premium Collection</collection><collection>Meteorological & Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><collection>ProQuest Engineering Collection</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Research Library</collection><collection>Engineering Database</collection><collection>Research Library (Corporate)</collection><collection>Advanced Technologies & Aerospace Database</collection><collection>ProQuest Advanced Technologies & Aerospace Collection</collection><collection>Environmental Science Database</collection><collection>Earth, Atmospheric & Aquatic Science 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>Engineering Collection</collection><collection>Environmental Science Collection</collection><collection>ProQuest Central Basic</collection><collection>Oceanic Abstracts</collection><collection>Earthquake Engineering Abstracts</collection><jtitle>Journal of Geophysical Research. B. Solid Earth</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Zhou, Lian-Tong</au><au>Wu, Renguang</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Respective impacts of the East Asian winter monsoon and ENSO on winter rainfall in China</atitle><jtitle>Journal of Geophysical Research. B. Solid Earth</jtitle><addtitle>J. Geophys. Res</addtitle><date>2010-01-26</date><risdate>2010</risdate><volume>115</volume><issue>D2</issue><epage>n/a</epage><issn>0148-0227</issn><issn>2169-897X</issn><eissn>2156-2202</eissn><eissn>2169-8996</eissn><abstract>Using station rainfall observations and the ERA‐40 reanalysis, this study investigates respective impacts of the East Asian winter monsoon (EAWM) and El Niño‐Southern Oscillation (ENSO) on winter (November–March) rainfall in China by removing the interdependence between the EAWM and ENSO using a linear regression. It is found that circulation and temperature anomalies over the tropics and midlatitude North Pacific are mainly induced by ENSO, and those over the midlatitude Asia are closely linked to the EAWM. The warm ENSO induced lower‐level southwesterly winds deflect from the southeast coast of China, and thus, the influence of ENSO on winter rainfall is mainly in southern China. The lower‐level southerly winds associated with a weak EAWM penetrate northward over eastern China, and thus, the EAWM influences winter rainfall in eastern China.</abstract><cop>Washington, DC</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1029/2009JD012502</doi><tpages>11</tpages><oa>free_for_read</oa></addata></record> |
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| subjects | Asian Atmosphere Atmospheric sciences Climate change Earth Earth sciences Earth, ocean, space EAWM El Nino ENSO Exact sciences and technology Geophysics Latitude Marine Monsoons Oscillations Rainfall Regression Southern Oscillation Stations Tropical environments Tropics Winter |
| title | Respective impacts of the East Asian winter monsoon and ENSO on winter rainfall in China |
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