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Decadal Modulation of Precipitation Patterns over Eastern China by Sea Surface Temperature Anomalies
by
Wu, Peili
, Fan, Xingang
, Yang, Zong-Liang
, Xu, Zhongfeng
, Ma, Zhuguo
, Yang, Qing
in
Annual precipitation
/ Anomalies
/ Anticyclonic circulation
/ Atlantic Oscillation
/ Atmospheric circulation
/ Atmospheric circulation anomalies
/ Atmospheric circulation models
/ Atmospheric General Circulation Models
/ Circulation
/ Cold
/ Dipoles
/ Drought
/ El Nino
/ El Nino phenomena
/ El Nino-Southern Oscillation event
/ Flooding
/ General circulation
/ Geology
/ Greenhouse gases
/ Laboratories
/ Lower troposphere
/ Migration
/ Monsoons
/ Ocean temperature
/ Physics
/ Precipitation
/ Precipitation anomalies
/ Precipitation patterns
/ Rain
/ Sea surface
/ Sea surface temperature
/ Sea surface temperature anomalies
/ Southern Oscillation
/ Studies
/ Surface temperature
/ Temperature anomalies
/ Temperature effects
/ Troposphere
/ Variability
/ Wind
/ Winds
2017
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Decadal Modulation of Precipitation Patterns over Eastern China by Sea Surface Temperature Anomalies
by
Wu, Peili
, Fan, Xingang
, Yang, Zong-Liang
, Xu, Zhongfeng
, Ma, Zhuguo
, Yang, Qing
in
Annual precipitation
/ Anomalies
/ Anticyclonic circulation
/ Atlantic Oscillation
/ Atmospheric circulation
/ Atmospheric circulation anomalies
/ Atmospheric circulation models
/ Atmospheric General Circulation Models
/ Circulation
/ Cold
/ Dipoles
/ Drought
/ El Nino
/ El Nino phenomena
/ El Nino-Southern Oscillation event
/ Flooding
/ General circulation
/ Geology
/ Greenhouse gases
/ Laboratories
/ Lower troposphere
/ Migration
/ Monsoons
/ Ocean temperature
/ Physics
/ Precipitation
/ Precipitation anomalies
/ Precipitation patterns
/ Rain
/ Sea surface
/ Sea surface temperature
/ Sea surface temperature anomalies
/ Southern Oscillation
/ Studies
/ Surface temperature
/ Temperature anomalies
/ Temperature effects
/ Troposphere
/ Variability
/ Wind
/ Winds
2017
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Decadal Modulation of Precipitation Patterns over Eastern China by Sea Surface Temperature Anomalies
by
Wu, Peili
, Fan, Xingang
, Yang, Zong-Liang
, Xu, Zhongfeng
, Ma, Zhuguo
, Yang, Qing
in
Annual precipitation
/ Anomalies
/ Anticyclonic circulation
/ Atlantic Oscillation
/ Atmospheric circulation
/ Atmospheric circulation anomalies
/ Atmospheric circulation models
/ Atmospheric General Circulation Models
/ Circulation
/ Cold
/ Dipoles
/ Drought
/ El Nino
/ El Nino phenomena
/ El Nino-Southern Oscillation event
/ Flooding
/ General circulation
/ Geology
/ Greenhouse gases
/ Laboratories
/ Lower troposphere
/ Migration
/ Monsoons
/ Ocean temperature
/ Physics
/ Precipitation
/ Precipitation anomalies
/ Precipitation patterns
/ Rain
/ Sea surface
/ Sea surface temperature
/ Sea surface temperature anomalies
/ Southern Oscillation
/ Studies
/ Surface temperature
/ Temperature anomalies
/ Temperature effects
/ Troposphere
/ Variability
/ Wind
/ Winds
2017
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Decadal Modulation of Precipitation Patterns over Eastern China by Sea Surface Temperature Anomalies
Journal Article
Decadal Modulation of Precipitation Patterns over Eastern China by Sea Surface Temperature Anomalies
2017
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Overview
Annual precipitation anomalies over eastern China are characterized by a north–south dipole pattern, referred to as the “southern flooding and northern drought” pattern (SF/ND), fluctuating on decadal time scales. Previous research has suggested possible links with oceanic forcing, but the underlying physical mechanisms by which sea surface temperature (SST) variability impacts the dipole pattern remains unclear. Idealized atmospheric general circulation model experiments conducted by the U.S. CLIVAR Drought Working Group are used to investigate the role of historical SST anomalies associated with Pacific El Niño–Southern Oscillation (ENSO)-like and the Atlantic multidecadal oscillation (AMO) patterns in this dipole pattern. The results show that the Pacific SST pattern plays a dominant role in driving the decadal variability of this dipole pattern and the associated atmospheric circulation anomalies, whereas the Atlantic SST pattern contributes to a much lesser degree. The direct atmospheric response to the Pacific SST pattern is a large-scale cyclonic or anticyclonic circulation anomaly in the lower troposphere occupying the entire northern North Pacific. During the warm phase of the Pacific SST pattern, it is cyclonic with northwesterly wind anomalies over northern China pushing the monsoon front to the south and consequently SF/ND. During the cold phase of the Pacific SST pattern, the circulation anomaly reverses with southeasterly winds over northern China allowing the monsoon front and the associated rainband to migrate northward, resulting in southern drought and northern flooding. The Atlantic SST pattern plays a supplementary role, enhancing the dipole pattern when the Pacific SST and Atlantic SST patterns are in opposite phases and weakening it when the phases are the same.
Publisher
American Meteorological Society
Subject
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