Assessment of the response of the East Asian winter monsoon to ENSO‐like SSTAs in three U.S. CLIVAR Project models
ABSTRACT The simulated response of the East Asian winter monsoon ( EAWM ) to ENSO ‐like sea surface temperature anomalies ( SSTAs ) forcing in three U.S. Climate Variability and Predictability (U.S. CLIVAR ) Project models ( GFDL , CCM3 , and CCM3 .5) are evaluated. The time series of the ENSO ‐like...
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crwiley:10.1002/joc.4388 2024-09-15T17:36:29+00:00 Assessment of the response of the East Asian winter monsoon to ENSO‐like SSTAs in three U.S. CLIVAR Project models Hao, Xin Li, Fei Sun, Jianqi Wang, Huijun He, Shengping National Natural Science Foundation of China National Natural Science Foundation of China 2015 http://dx.doi.org/10.1002/joc.4388 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.4388 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.4388 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor International Journal of Climatology volume 36, issue 2, page 847-866 ISSN 0899-8418 1097-0088 journal-article 2015 crwiley https://doi.org/10.1002/joc.4388 2024-07-02T04:10:46Z ABSTRACT The simulated response of the East Asian winter monsoon ( EAWM ) to ENSO ‐like sea surface temperature anomalies ( SSTAs ) forcing in three U.S. Climate Variability and Predictability (U.S. CLIVAR ) Project models ( GFDL , CCM3 , and CCM3 .5) are evaluated. The time series of the ENSO ‐like pattern significantly correlates with the EAWM index for the period 1949–2004 based on the HadISST SST data set and the NCEP atmospheric reanalysis. Their correlation coefficient is −0.32 at the 95% confidence level. The warm (cold) phase of ENSO ‐like SSTAs is associated with a weakened (strengthened) Siberian High and an eastern‐positioned (western‐positioned) Aleutian Low, anomalous southerly (northerly) wind at 850 hPa and positive (negative) surface air temperature anomalies over East Asia and western North Pacific, while 300 hPa zonal wind anomalies emerge with a reduced (accelerated) East Asian jet stream. Further model examination reveals that the simulated response over East Asia forced by warm (cold) ENSO ‐like SSTAs in CCM3 and the three‐model ensemble corresponds to the weakened (strengthened) EAWM . The spatial correlation coefficients between the three‐model ensemble and observation in the atmospheric circulation and surface air temperature range from 0.15 to 0.80 at the 99% confidence level. This success in simulating relationship between ENSO ‐like SSTAs and EWAM using three‐model ensemble proposes a new idea for the EAWM prediction. Article in Journal/Newspaper aleutian low Wiley Online Library International Journal of Climatology 36 2 847 866 |
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Open Polar |
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Wiley Online Library |
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crwiley |
language |
English |
description |
ABSTRACT The simulated response of the East Asian winter monsoon ( EAWM ) to ENSO ‐like sea surface temperature anomalies ( SSTAs ) forcing in three U.S. Climate Variability and Predictability (U.S. CLIVAR ) Project models ( GFDL , CCM3 , and CCM3 .5) are evaluated. The time series of the ENSO ‐like pattern significantly correlates with the EAWM index for the period 1949–2004 based on the HadISST SST data set and the NCEP atmospheric reanalysis. Their correlation coefficient is −0.32 at the 95% confidence level. The warm (cold) phase of ENSO ‐like SSTAs is associated with a weakened (strengthened) Siberian High and an eastern‐positioned (western‐positioned) Aleutian Low, anomalous southerly (northerly) wind at 850 hPa and positive (negative) surface air temperature anomalies over East Asia and western North Pacific, while 300 hPa zonal wind anomalies emerge with a reduced (accelerated) East Asian jet stream. Further model examination reveals that the simulated response over East Asia forced by warm (cold) ENSO ‐like SSTAs in CCM3 and the three‐model ensemble corresponds to the weakened (strengthened) EAWM . The spatial correlation coefficients between the three‐model ensemble and observation in the atmospheric circulation and surface air temperature range from 0.15 to 0.80 at the 99% confidence level. This success in simulating relationship between ENSO ‐like SSTAs and EWAM using three‐model ensemble proposes a new idea for the EAWM prediction. |
author2 |
National Natural Science Foundation of China National Natural Science Foundation of China |
format |
Article in Journal/Newspaper |
author |
Hao, Xin Li, Fei Sun, Jianqi Wang, Huijun He, Shengping |
spellingShingle |
Hao, Xin Li, Fei Sun, Jianqi Wang, Huijun He, Shengping Assessment of the response of the East Asian winter monsoon to ENSO‐like SSTAs in three U.S. CLIVAR Project models |
author_facet |
Hao, Xin Li, Fei Sun, Jianqi Wang, Huijun He, Shengping |
author_sort |
Hao, Xin |
title |
Assessment of the response of the East Asian winter monsoon to ENSO‐like SSTAs in three U.S. CLIVAR Project models |
title_short |
Assessment of the response of the East Asian winter monsoon to ENSO‐like SSTAs in three U.S. CLIVAR Project models |
title_full |
Assessment of the response of the East Asian winter monsoon to ENSO‐like SSTAs in three U.S. CLIVAR Project models |
title_fullStr |
Assessment of the response of the East Asian winter monsoon to ENSO‐like SSTAs in three U.S. CLIVAR Project models |
title_full_unstemmed |
Assessment of the response of the East Asian winter monsoon to ENSO‐like SSTAs in three U.S. CLIVAR Project models |
title_sort |
assessment of the response of the east asian winter monsoon to enso‐like sstas in three u.s. clivar project models |
publisher |
Wiley |
publishDate |
2015 |
url |
http://dx.doi.org/10.1002/joc.4388 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fjoc.4388 https://rmets.onlinelibrary.wiley.com/doi/pdf/10.1002/joc.4388 |
genre |
aleutian low |
genre_facet |
aleutian low |
op_source |
International Journal of Climatology volume 36, issue 2, page 847-866 ISSN 0899-8418 1097-0088 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/joc.4388 |
container_title |
International Journal of Climatology |
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36 |
container_issue |
2 |
container_start_page |
847 |
op_container_end_page |
866 |
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1810489841427677184 |