Editorial Type:
Article
Article Type:
Research Article

Air–Sea Interaction over the Subtropical North Pacific during the ENSO Transition Phase

Wei Wu Research Center for Monsoon and Environment, and Department of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, and Bureau of Meteorology, Huizhou, China

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Zhiping Wen Research Center for Monsoon and Environment, and Department of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, China

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Renguang Wu Institute of Space and Earth Information Science, and Department of Physics, The Chinese University of Hong Kong, Hong Kong, China

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Tongmei Wang Research Center for Monsoon and Environment, and Department of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, China

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Print Publication:
15 Nov 2011
DOI:
https://doi.org/10.1175/2011JCLI3820.1
Page(s):
5772–5785
Restricted access

Abstract

In the present study, monthly mean objectively analyzed air–sea fluxes (OAFlux) and NCEP–Department of Energy (DOE) reanalysis datasets are employed to investigate air–sea interaction over the subtropical North Pacific during the El Niño–Southern Oscillation (ENSO) transition phase. A coupled low-frequency mode is identified, for which surface net heat flux and atmospheric circulation changes are strongly coupled during the ENSO transition phase. This mode features anomalous cooling (warming) and low-level anomalous cyclonic (anticyclonic) circulation over the subtropical North Pacific. When this mode is prominent, the atmospheric circulation anomalies lead to SST cooling (warming) through surface heat flux anomalies associated with increases (decreases) in the sea–air temperature and humidity differences induced by anomalous cold (warm) advection. In turn, positive heat flux anomalies induce more surface heating, and the SST cooling (warming) causes less (more) deep convective heating. The anomalous surface heating and deep convective heating contribute significantly to anomalous circulation through the thermal adaptation mechanism (adaptation of atmospheric circulation to vertical differential heating). This positive feedback favors the maintenance of these anomalous winds over the subtropical North Pacific.

Corresponding author address: Prof. Zhiping Wen, Research Center for Monsoon and Environment, Dept. of Atmospheric Sciences, Sun Yat-sen University, Guangzhou 510275, China. E-mail: eeswzp@mail.sysu.edu.cn

Abstract

In the present study, monthly mean objectively analyzed air–sea fluxes (OAFlux) and NCEP–Department of Energy (DOE) reanalysis datasets are employed to investigate air–sea interaction over the subtropical North Pacific during the El Niño–Southern Oscillation (ENSO) transition phase. A coupled low-frequency mode is identified, for which surface net heat flux and atmospheric circulation changes are strongly coupled during the ENSO transition phase. This mode features anomalous cooling (warming) and low-level anomalous cyclonic (anticyclonic) circulation over the subtropical North Pacific. When this mode is prominent, the atmospheric circulation anomalies lead to SST cooling (warming) through surface heat flux anomalies associated with increases (decreases) in the sea–air temperature and humidity differences induced by anomalous cold (warm) advection. In turn, positive heat flux anomalies induce more surface heating, and the SST cooling (warming) causes less (more) deep convective heating. The anomalous surface heating and deep convective heating contribute significantly to anomalous circulation through the thermal adaptation mechanism (adaptation of atmospheric circulation to vertical differential heating). This positive feedback favors the maintenance of these anomalous winds over the subtropical North Pacific.

Corresponding author address: Prof. Zhiping Wen, Research Center for Monsoon and Environment, Dept. of Atmospheric Sciences, Sun Yat-sen University, Guangzhou 510275, China. E-mail: eeswzp@mail.sysu.edu.cn
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