Atmospheric pressure
; Atmospheric temperature
; Atmospheric thermodynamics
; Climate change
; Climatology
; Heat storage
; Pressure gradient
; Surface properties
; Temperature
; Atmospheric circulation
; Climate variability
; Correlation coefficient
; East Asian winter monsoon
; Interannual variability
; Large pressure gradients
; Surface air temperatures
; Surface temperature anomalies
; Fighter aircraft
; air temperature
; air-sea interaction
; annual variation
; Arctic Oscillation
; atmospheric circulation
; climate variation
; El Nino-Southern Oscillation
; monsoon
; temperature anomaly
; winter
; China
; Pacific Ocean
; Pacific Ocean (Northwest)
英文摘要:
This study investigates the variations and feedback attributions of changes in surface temperature between strong and weak East Asian winter monsoons. The variations of winter-mean surface air temperature are dominated by two distinct principal modes that account for 70.9% of the total variance. The first mode features high correlation with the high-latitude atmospheric circulation, including a correlation coefficient of -0.53 with the Arctic Oscillation in January, and the second mode is significantly linked to El Niño-Southern Oscillation, with a correlation coefficient of -0.37. The surface temperature anomalies of each mode are decomposed into partial temperature anomalies resulting from radiative and nonradiative feedback processes by applying a coupled climate feedback-response analysis method to quantify contributions from thermodynamic and dynamic processes. Results indicate that the surface cooling associated with both modes is mainly attributed to the nonradiative feedback processes of atmospheric dynamics and surface sensible heating and to the radiative feedback processes of water vapor and clouds. The first mode exhibits a deep barotropic anomalous high that weakens the high-latitude westerly jet stream but strengthens the midlatitude westerly jet stream. This circulation feature traps cold and dry air over northern East Asia. For the second mode, the ocean and land heat storage processes induce a large thermal gradient over eastern China and the northwestern Pacific, resulting in a large pressure gradient. Northerly anomalies further reinforce the pressure gradient, which favors cold air intruding southward into the tropics.
资助项目:
NSFC, National Natural Science Foundation of China
; NSFC, National Natural Science Foundation of China
; NSFC, National Natural Science Foundation of China
; NSFC, National Natural Science Foundation of China
; NSFC, National Natural Science Foundation of China
School of Atmospheric Sciences, Sun Yat-sen University, Guangzhou, China; Guangdong Province Key Laboratory for Climate Change and Natural Disaster Studies, Sun Yat-sen University, Guangzhou, China; Institute of Earth Climate and Environment System, Sun Yat-sen University, Guangzhou, China
Recommended Citation:
Li Y.,Yang S.. Feedback attributions to the dominant modes of East Asian winter monsoon variations[J]. Journal of Climate,2017-01-01,30(3)