Differences and Links between the East Asian and South Asian Summer Monsoon Systems: Characteristics and Variability
This paper analyzes the differences in the characteristics and spatio–temporal variabilities of summertime rainfall and water vapor transport between the East Asian summer monsoon(EASM) and South Asian summer monsoon(SASM) systems. The results show obvious differences in summertime rainfall characte...
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description | This paper analyzes the differences in the characteristics and spatio–temporal variabilities of summertime rainfall and water vapor transport between the East Asian summer monsoon(EASM) and South Asian summer monsoon(SASM) systems. The results show obvious differences in summertime rainfall characteristics between these two monsoon systems. The summertime rainfall cloud systems of the EASM show a mixed stratiform and cumulus cloud system, while cumulus cloud dominates the SASM. These differences may be caused by differences in the vertical shear of zonal and meridional circulations and the convergence of water vapor transport fluxes. Moreover, the leading modes of the two systems' summertime rainfall anomalies also differ in terms of their spatiotemporal features on the interannual and interdecadal timescales. Nevertheless, several close links with respect to the spatiotemporal variabilities of summertime rainfall and water vapor transport exist between the two monsoon systems. The first modes of summertime rainfall in the SASM and EASM regions reveal a significant negative correlation on the interannual and the interdecadal timescales. This close relationship may be linked by a meridional teleconnection in the regressed summertime rainfall anomalies from India to North China through the southeastern part over the Tibetan Plateau, which we refer to as the South Asia/East Asia teleconnection pattern of Asian summer monsoon rainfall. The authors wish to dedicate this paper to Prof. Duzheng YE, and commemorate his 100 thanniversary and his great contributions to the development of atmospheric dynamics. |
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The results show obvious differences in summertime rainfall characteristics between these two monsoon systems. The summertime rainfall cloud systems of the EASM show a mixed stratiform and cumulus cloud system, while cumulus cloud dominates the SASM. These differences may be caused by differences in the vertical shear of zonal and meridional circulations and the convergence of water vapor transport fluxes. Moreover, the leading modes of the two systems' summertime rainfall anomalies also differ in terms of their spatiotemporal features on the interannual and interdecadal timescales. Nevertheless, several close links with respect to the spatiotemporal variabilities of summertime rainfall and water vapor transport exist between the two monsoon systems. The first modes of summertime rainfall in the SASM and EASM regions reveal a significant negative correlation on the interannual and the interdecadal timescales. This close relationship may be linked by a meridional teleconnection in the regressed summertime rainfall anomalies from India to North China through the southeastern part over the Tibetan Plateau, which we refer to as the South Asia/East Asia teleconnection pattern of Asian summer monsoon rainfall. The authors wish to dedicate this paper to Prof. Duzheng YE, and commemorate his 100 thanniversary and his great contributions to the development of atmospheric dynamics.</description><identifier>ISSN: 0256-1530</identifier><identifier>EISSN: 1861-9533</identifier><identifier>DOI: 10.1007/s00376-017-7008-3</identifier><language>eng</language><publisher>Heidelberg: Science Press</publisher><subject>Anomalies ; Atmospheric dynamics ; Atmospheric Sciences ; Climate change ; Cloud systems ; Clouds ; Cumulus clouds ; Dynamics ; Earth and Environmental Science ; Earth Sciences ; East Asian monsoon ; Fluxes ; Geophysics/Geodesy ; Meteorology ; Modes ; Monsoon rainfall ; Monsoons ; Original Paper ; Plateaus ; Rain ; Rainfall ; Rainfall anomalies ; Rainfall measurement ; Regression analysis ; Summer ; Summer monsoon ; Teleconnections ; Transport ; Variability ; Vertical shear ; Water vapor ; Water vapor transport ; Water vapour ; Wind ; 东亚夏季风 ; 南亚季风 ; 可变性 ; 夏季降水异常 ; 季风系统 ; 时空变化 ; 水汽输送通量 ; 特征和</subject><ispartof>Advances in atmospheric sciences, 2017-10, Vol.34 (10), p.1204-1218</ispartof><rights>Chinese National Committee for International Association of Meteorology and Atmospheric Sciences, Institute of Atmospheric Physics, Science Press and Springer-Verlag GmbH Germany 2017</rights><rights>Advances in Atmospheric Sciences is a copyright of Springer, 2017.</rights><rights>Copyright © Wanfang Data Co. Ltd. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c377t-f5bccec847ee7434a6e61bf5e87b4d69794fb8975035e177de0fea7a4fb886bc3</citedby><cites>FETCH-LOGICAL-c377t-f5bccec847ee7434a6e61bf5e87b4d69794fb8975035e177de0fea7a4fb886bc3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Uhttp://image.cqvip.com/vip1000/qk/84334X/84334X.jpg</thumbnail><linktopdf>$$Uhttps://link.springer.com/content/pdf/10.1007/s00376-017-7008-3$$EPDF$$P50$$Gspringer$$H</linktopdf><linktohtml>$$Uhttps://link.springer.com/10.1007/s00376-017-7008-3$$EHTML$$P50$$Gspringer$$H</linktohtml><link.rule.ids>314,776,780,27903,27904,41467,42536,51297</link.rule.ids></links><search><creatorcontrib>Huang, Ronghui</creatorcontrib><creatorcontrib>Liu, Yong</creatorcontrib><creatorcontrib>Du, Zhencai</creatorcontrib><creatorcontrib>Chen, Jilong</creatorcontrib><creatorcontrib>Huangfu, Jingliang</creatorcontrib><title>Differences and Links between the East Asian and South Asian Summer Monsoon Systems: Characteristics and Variability</title><title>Advances in atmospheric sciences</title><addtitle>Adv. Atmos. Sci</addtitle><addtitle>Advances in Atmospheric Sciences</addtitle><description>This paper analyzes the differences in the characteristics and spatio–temporal variabilities of summertime rainfall and water vapor transport between the East Asian summer monsoon(EASM) and South Asian summer monsoon(SASM) systems. The results show obvious differences in summertime rainfall characteristics between these two monsoon systems. The summertime rainfall cloud systems of the EASM show a mixed stratiform and cumulus cloud system, while cumulus cloud dominates the SASM. These differences may be caused by differences in the vertical shear of zonal and meridional circulations and the convergence of water vapor transport fluxes. Moreover, the leading modes of the two systems' summertime rainfall anomalies also differ in terms of their spatiotemporal features on the interannual and interdecadal timescales. Nevertheless, several close links with respect to the spatiotemporal variabilities of summertime rainfall and water vapor transport exist between the two monsoon systems. The first modes of summertime rainfall in the SASM and EASM regions reveal a significant negative correlation on the interannual and the interdecadal timescales. This close relationship may be linked by a meridional teleconnection in the regressed summertime rainfall anomalies from India to North China through the southeastern part over the Tibetan Plateau, which we refer to as the South Asia/East Asia teleconnection pattern of Asian summer monsoon rainfall. The authors wish to dedicate this paper to Prof. Duzheng YE, and commemorate his 100 thanniversary and his great contributions to the development of atmospheric dynamics.</description><subject>Anomalies</subject><subject>Atmospheric dynamics</subject><subject>Atmospheric Sciences</subject><subject>Climate change</subject><subject>Cloud systems</subject><subject>Clouds</subject><subject>Cumulus clouds</subject><subject>Dynamics</subject><subject>Earth and Environmental Science</subject><subject>Earth Sciences</subject><subject>East Asian monsoon</subject><subject>Fluxes</subject><subject>Geophysics/Geodesy</subject><subject>Meteorology</subject><subject>Modes</subject><subject>Monsoon rainfall</subject><subject>Monsoons</subject><subject>Original Paper</subject><subject>Plateaus</subject><subject>Rain</subject><subject>Rainfall</subject><subject>Rainfall anomalies</subject><subject>Rainfall measurement</subject><subject>Regression analysis</subject><subject>Summer</subject><subject>Summer monsoon</subject><subject>Teleconnections</subject><subject>Transport</subject><subject>Variability</subject><subject>Vertical shear</subject><subject>Water vapor</subject><subject>Water vapor transport</subject><subject>Water vapour</subject><subject>Wind</subject><subject>东亚夏季风</subject><subject>南亚季风</subject><subject>可变性</subject><subject>夏季降水异常</subject><subject>季风系统</subject><subject>时空变化</subject><subject>水汽输送通量</subject><subject>特征和</subject><issn>0256-1530</issn><issn>1861-9533</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2017</creationdate><recordtype>article</recordtype><sourceid>BENPR</sourceid><recordid>eNp9kc1uEzEUhS1UJNLSB-huRFcshtrjsa9nWaXlRwpiUWBreZzrxGnjaWynJTwKz8I78Qp1mAhYsbKu9Z1zpHMIOWP0DaMULhKlHGRNGdRAqar5MzJhSrK6E5wfkQlthKyZ4PQFOU5pVeiOKzYhD1feOYwYLKbKhHk18-E2VT3mR8RQ5SVW1ybl6jJ5E34DN8M2Lw_3zXa9xlh9HEIahnLuUsZ1-vXzRzVdmmhsxuhT9na0_mqiN72_83n3kjx35i7h6eE9IV_eXn-evq9nn959mF7OassBcu1Eby1a1QIitLw1EiXrnUAFfTuXHXSt61UHgnKBDGCO1KEBs_9Vsrf8hLwefR9NcCYs9GrYxlAS9Xxz-231XWNTKisNUlXY85G9j8Nmiyn_hVnXlLpAibZQbKRsHFKK6PR99GsTd5pRvZ9Cj1Po4qv3U2heNM2oSYUNC4z_OP9H9OoQtBzCYlN0f5IkcKpkI4A_AXM4ma4</recordid><startdate>20171001</startdate><enddate>20171001</enddate><creator>Huang, Ronghui</creator><creator>Liu, Yong</creator><creator>Du, Zhencai</creator><creator>Chen, Jilong</creator><creator>Huangfu, Jingliang</creator><general>Science Press</general><general>Springer Nature B.V</general><general>Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100190, China</general><general>State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics, Chinese Academy of Science, Beijing 100029, China</general><general>Institute of Earth Sciences, University of Chinese Academy of Sciences, Beijing 100049, China%Center for Monsoon System Research, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100190, China</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>7TG</scope><scope>7XB</scope><scope>88F</scope><scope>88I</scope><scope>8FK</scope><scope>ABUWG</scope><scope>AEUYN</scope><scope>AFKRA</scope><scope>ATCPS</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>H96</scope><scope>HCIFZ</scope><scope>KL.</scope><scope>L.G</scope><scope>M1Q</scope><scope>M2P</scope><scope>PATMY</scope><scope>PCBAR</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PYCSY</scope><scope>Q9U</scope><scope>2B.</scope><scope>4A8</scope><scope>92I</scope><scope>93N</scope><scope>PSX</scope><scope>TCJ</scope></search><sort><creationdate>20171001</creationdate><title>Differences and Links between the East Asian and South Asian Summer Monsoon Systems: Characteristics and Variability</title><author>Huang, Ronghui ; 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Atmos. Sci</stitle><addtitle>Advances in Atmospheric Sciences</addtitle><date>2017-10-01</date><risdate>2017</risdate><volume>34</volume><issue>10</issue><spage>1204</spage><epage>1218</epage><pages>1204-1218</pages><issn>0256-1530</issn><eissn>1861-9533</eissn><abstract>This paper analyzes the differences in the characteristics and spatio–temporal variabilities of summertime rainfall and water vapor transport between the East Asian summer monsoon(EASM) and South Asian summer monsoon(SASM) systems. The results show obvious differences in summertime rainfall characteristics between these two monsoon systems. The summertime rainfall cloud systems of the EASM show a mixed stratiform and cumulus cloud system, while cumulus cloud dominates the SASM. These differences may be caused by differences in the vertical shear of zonal and meridional circulations and the convergence of water vapor transport fluxes. Moreover, the leading modes of the two systems' summertime rainfall anomalies also differ in terms of their spatiotemporal features on the interannual and interdecadal timescales. Nevertheless, several close links with respect to the spatiotemporal variabilities of summertime rainfall and water vapor transport exist between the two monsoon systems. The first modes of summertime rainfall in the SASM and EASM regions reveal a significant negative correlation on the interannual and the interdecadal timescales. This close relationship may be linked by a meridional teleconnection in the regressed summertime rainfall anomalies from India to North China through the southeastern part over the Tibetan Plateau, which we refer to as the South Asia/East Asia teleconnection pattern of Asian summer monsoon rainfall. The authors wish to dedicate this paper to Prof. Duzheng YE, and commemorate his 100 thanniversary and his great contributions to the development of atmospheric dynamics.</abstract><cop>Heidelberg</cop><pub>Science Press</pub><doi>10.1007/s00376-017-7008-3</doi><tpages>15</tpages></addata></record> |
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subjects | Anomalies Atmospheric dynamics Atmospheric Sciences Climate change Cloud systems Clouds Cumulus clouds Dynamics Earth and Environmental Science Earth Sciences East Asian monsoon Fluxes Geophysics/Geodesy Meteorology Modes Monsoon rainfall Monsoons Original Paper Plateaus Rain Rainfall Rainfall anomalies Rainfall measurement Regression analysis Summer Summer monsoon Teleconnections Transport Variability Vertical shear Water vapor Water vapor transport Water vapour Wind 东亚夏季风 南亚季风 可变性 夏季降水异常 季风系统 时空变化 水汽输送通量 特征和 |
title | Differences and Links between the East Asian and South Asian Summer Monsoon Systems: Characteristics and Variability |
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