The possible influence of tropical Pacific subsurface temperature anomalies on summer precipitation in eastern China
Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /Nat...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Li, Liping [verfasserIn] |
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| Format: |
Artikel |
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| Sprache: |
Englisch |
| Erschienen: |
2015 |
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| Rechteinformationen: |
Nutzungsrecht: © 2014 Royal Meteorological Society |
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| Schlagwörter: |
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| Systematik: |
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| Übergeordnetes Werk: |
Enthalten in: International journal of climatology - Chichester [u.a.] : Wiley, 1989, 35(2015), 9, Seite 2441-2450 |
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| Übergeordnetes Werk: |
volume:35 ; year:2015 ; number:9 ; pages:2441-2450 |
| Links: |
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| DOI / URN: |
10.1002/joc.4134 |
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| 520 | |a Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. | ||
| 540 | |a Nutzungsrecht: © 2014 Royal Meteorological Society | ||
| 650 | 4 | |a East Asian circulations | |
| 650 | 4 | |a interannual variations | |
| 650 | 4 | |a Summer precipitation in China | |
| 650 | 4 | |a subsurface temperature | |
| 650 | 4 | |a tropical Pacific | |
| 700 | 1 | |a Wang, Chao |4 oth | |
| 700 | 1 | |a Fu, Xiouhua |4 oth | |
| 700 | 1 | |a Liu, Yanju |4 oth | |
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10.1002/joc.4134 doi PQ20160617 (DE-627)OLC1968540466 (DE-599)GBVOLC1968540466 (PRQ)c2114-95312bf3c49c99e7f25955604f480c093d20b3076cd3f34cf157c86ba150e8f93 (KEY)0104704320150000035000902441possibleinfluenceoftropicalpacificsubsurfacetemper DE-627 ger DE-627 rakwb eng 550 DNB RA 1000 AVZ rvk Li, Liping verfasserin aut The possible influence of tropical Pacific subsurface temperature anomalies on summer precipitation in eastern China 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. Nutzungsrecht: © 2014 Royal Meteorological Society East Asian circulations interannual variations Summer precipitation in China subsurface temperature tropical Pacific Wang, Chao oth Fu, Xiouhua oth Liu, Yanju oth Enthalten in International journal of climatology Chichester [u.a.] : Wiley, 1989 35(2015), 9, Seite 2441-2450 (DE-627)130763128 (DE-600)1000947-4 (DE-576)023035773 0899-8418 nnns volume:35 year:2015 number:9 pages:2441-2450 http://dx.doi.org/10.1002/joc.4134 Volltext http://onlinelibrary.wiley.com/doi/10.1002/joc.4134/abstract http://search.proquest.com/docview/1696045208 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_2003 GBV_ILN_4012 GBV_ILN_4311 RA 1000 AR 35 2015 9 2441-2450 |
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10.1002/joc.4134 doi PQ20160617 (DE-627)OLC1968540466 (DE-599)GBVOLC1968540466 (PRQ)c2114-95312bf3c49c99e7f25955604f480c093d20b3076cd3f34cf157c86ba150e8f93 (KEY)0104704320150000035000902441possibleinfluenceoftropicalpacificsubsurfacetemper DE-627 ger DE-627 rakwb eng 550 DNB RA 1000 AVZ rvk Li, Liping verfasserin aut The possible influence of tropical Pacific subsurface temperature anomalies on summer precipitation in eastern China 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. Nutzungsrecht: © 2014 Royal Meteorological Society East Asian circulations interannual variations Summer precipitation in China subsurface temperature tropical Pacific Wang, Chao oth Fu, Xiouhua oth Liu, Yanju oth Enthalten in International journal of climatology Chichester [u.a.] : Wiley, 1989 35(2015), 9, Seite 2441-2450 (DE-627)130763128 (DE-600)1000947-4 (DE-576)023035773 0899-8418 nnns volume:35 year:2015 number:9 pages:2441-2450 http://dx.doi.org/10.1002/joc.4134 Volltext http://onlinelibrary.wiley.com/doi/10.1002/joc.4134/abstract http://search.proquest.com/docview/1696045208 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_2003 GBV_ILN_4012 GBV_ILN_4311 RA 1000 AR 35 2015 9 2441-2450 |
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10.1002/joc.4134 doi PQ20160617 (DE-627)OLC1968540466 (DE-599)GBVOLC1968540466 (PRQ)c2114-95312bf3c49c99e7f25955604f480c093d20b3076cd3f34cf157c86ba150e8f93 (KEY)0104704320150000035000902441possibleinfluenceoftropicalpacificsubsurfacetemper DE-627 ger DE-627 rakwb eng 550 DNB RA 1000 AVZ rvk Li, Liping verfasserin aut The possible influence of tropical Pacific subsurface temperature anomalies on summer precipitation in eastern China 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. Nutzungsrecht: © 2014 Royal Meteorological Society East Asian circulations interannual variations Summer precipitation in China subsurface temperature tropical Pacific Wang, Chao oth Fu, Xiouhua oth Liu, Yanju oth Enthalten in International journal of climatology Chichester [u.a.] : Wiley, 1989 35(2015), 9, Seite 2441-2450 (DE-627)130763128 (DE-600)1000947-4 (DE-576)023035773 0899-8418 nnns volume:35 year:2015 number:9 pages:2441-2450 http://dx.doi.org/10.1002/joc.4134 Volltext http://onlinelibrary.wiley.com/doi/10.1002/joc.4134/abstract http://search.proquest.com/docview/1696045208 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_2003 GBV_ILN_4012 GBV_ILN_4311 RA 1000 AR 35 2015 9 2441-2450 |
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10.1002/joc.4134 doi PQ20160617 (DE-627)OLC1968540466 (DE-599)GBVOLC1968540466 (PRQ)c2114-95312bf3c49c99e7f25955604f480c093d20b3076cd3f34cf157c86ba150e8f93 (KEY)0104704320150000035000902441possibleinfluenceoftropicalpacificsubsurfacetemper DE-627 ger DE-627 rakwb eng 550 DNB RA 1000 AVZ rvk Li, Liping verfasserin aut The possible influence of tropical Pacific subsurface temperature anomalies on summer precipitation in eastern China 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. Nutzungsrecht: © 2014 Royal Meteorological Society East Asian circulations interannual variations Summer precipitation in China subsurface temperature tropical Pacific Wang, Chao oth Fu, Xiouhua oth Liu, Yanju oth Enthalten in International journal of climatology Chichester [u.a.] : Wiley, 1989 35(2015), 9, Seite 2441-2450 (DE-627)130763128 (DE-600)1000947-4 (DE-576)023035773 0899-8418 nnns volume:35 year:2015 number:9 pages:2441-2450 http://dx.doi.org/10.1002/joc.4134 Volltext http://onlinelibrary.wiley.com/doi/10.1002/joc.4134/abstract http://search.proquest.com/docview/1696045208 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_2003 GBV_ILN_4012 GBV_ILN_4311 RA 1000 AR 35 2015 9 2441-2450 |
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10.1002/joc.4134 doi PQ20160617 (DE-627)OLC1968540466 (DE-599)GBVOLC1968540466 (PRQ)c2114-95312bf3c49c99e7f25955604f480c093d20b3076cd3f34cf157c86ba150e8f93 (KEY)0104704320150000035000902441possibleinfluenceoftropicalpacificsubsurfacetemper DE-627 ger DE-627 rakwb eng 550 DNB RA 1000 AVZ rvk Li, Liping verfasserin aut The possible influence of tropical Pacific subsurface temperature anomalies on summer precipitation in eastern China 2015 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. Nutzungsrecht: © 2014 Royal Meteorological Society East Asian circulations interannual variations Summer precipitation in China subsurface temperature tropical Pacific Wang, Chao oth Fu, Xiouhua oth Liu, Yanju oth Enthalten in International journal of climatology Chichester [u.a.] : Wiley, 1989 35(2015), 9, Seite 2441-2450 (DE-627)130763128 (DE-600)1000947-4 (DE-576)023035773 0899-8418 nnns volume:35 year:2015 number:9 pages:2441-2450 http://dx.doi.org/10.1002/joc.4134 Volltext http://onlinelibrary.wiley.com/doi/10.1002/joc.4134/abstract http://search.proquest.com/docview/1696045208 GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-GEO SSG-OPC-GGO GBV_ILN_22 GBV_ILN_2003 GBV_ILN_4012 GBV_ILN_4311 RA 1000 AR 35 2015 9 2441-2450 |
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In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. 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possible influence of tropical pacific subsurface temperature anomalies on summer precipitation in eastern china |
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The possible influence of tropical Pacific subsurface temperature anomalies on summer precipitation in eastern China |
| abstract |
Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. |
| abstractGer |
Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. |
| abstract_unstemmed |
Using NCEP (National Centers for Environmental Prediction) GODAS (Global Ocean Data Assimilation System) monthly subsurface temperature ( SsT ) from 1980 to 2009, a 3‐D four‐step model was established to categorize the SsT interannual variations in the tropical Pacific. In combination with NCEP /National Center for Atmospheric Research ( NCAR ) reanalysis 850‐hPa wind field and 160 stations' precipitation data in China, an intimate connection between the tropical Pacific SsT and eastern China summer precipitation anomalies is discovered by examining the time‐lagged and simultaneous correlations among the interannual anomalies of SsT in the tropical Pacific, the 850‐hPa wind pattern and summer rainfall in China. In previous winter, if the SsT in the tropical Pacific indicates an El Niño‐type anomaly, an anticyclonic circulation anomaly over the East Asian coast, South China Sea and east of Taiwan along with a cyclonic circulation anomaly over the Japanese archipelago emerges in following summer. At the same time, a cyclonic circulation and an anticyclonic circulation prevail over the Lake Baikal and Kuril Islands in the high latitude. These combined circulation patterns facilitate the southward transport of cold air from high latitude and northward transport of warm and moist air through the western edge of the subtropical high. The meet between two air masses results in significantly abundant anomalous precipitation in the Sichuan Basin, Dongting and Poyang Lake Basin, and possibly deficit precipitation occurs over the Hetao region and lower Yellow River Basin, northern Zhejiang, as well as the coastal region of southern China and southern Yunnan. These findings offer a very useful predictive power for eastern China summer precipitation based on tropical Pacific SsT status in previous winter and subsequent developments of SsT and East Asian large‐scale circulations. |
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