Interdecadal Change of the Winter-Spring Tropospheric Temperature Over Asia and its Impact on the South China Sea Summer Monsoon Onset

Junli You,Si Gao,Maoqiu Jian,Jingjiu Cai

doi:10.3389/feart.2020.599447

Abstract

The interdecadal change of the winter-spring tropospheric temperature over Asia and its impact on the South China Sea summer monsoon (SCSSM) onset are investigated in this study. The SCSSM onset experiences a significant advance around the mid-1990s, which is attributed to the positive interdecadal anomaly of meridional temperature gradient in the mid-upper troposphere in May over the South China Sea monsoon region. This positive interdecadal anomaly can be traced back to the previous winter and spring, mainly associated with the mid-upper tropospheric warming in the East Asian subtropics. During the interdecadal anomalous seasonal evolution of the East Asian subtropical mid-upper tropospheric temperature, advection of the warm temperature anomaly by climatological mean wind overtakes the effects of anomalous adiabatic cooling and diabatic cooling, leading to a net interdecadal seasonal warming in winter. In spring, the adiabatic heating caused by the interdecadal anomalous subsidence flow cannot offset the effects of interdecadal anomalous cold advection and diabatic cooling, resulting in a net interdecadal seasonal cooling. However, the interdecadal seasonal cooling in spring is not strong enough to offset the interdecadal seasonal warming in winter, preserving an interdecadal mid-upper tropospheric warming over the subtropical East Asia in late spring. This interdecadal warming provides a favorable condition for the interdecadal advance of the SCSSM onset. Both observational analyses and numerical experiments suggest that the interdecadal change of atmospheric thermodynamic processes in winter−spring is related to the interdecadal warming in the tropical western Pacific. The enhanced convection and condensation heating over the regions from the South China Sea to the Philippines, forced by the tropical western Pacific warming, stimulates an anomalous anticyclone in the upper troposphere and warming in the whole troposphere over the subtropical East Asia.

Highlights

The South China Sea (SCS) is located in the center of the AsianAustralian monsoon system, connecting the Indian Ocean and the Pacific
Some studies suggested that the relationship between the SCS summer monsoon (SCSSM) onset and the precipitation over eastern China is regulated by the thermal state of the western Pacific warm pool
This study has examined the interdecadal change of the mid-upper tropospheric temperature over Asian monsoon region during winter and spring and its connection with the interdecadal advance of the SCSSM onset around 1993/94

Summary

INTRODUCTION

The South China Sea (SCS) is located in the center of the AsianAustralian monsoon system, connecting the Indian Ocean and the Pacific. The sustained positive interdecadal MTG anomalies over the SCS monsoon region during winter to spring, which is primarily attributed to the prominent interdecadal warming of intermonthly temperature changes from November to December and from January to February over the East Asian subtropics, FIGURE 5 | Epochal differences (K) of the seasonal mean temperature (left panel) and the inter-seasonal change of temperature (right panel) in the 500–200 hPa layer. The distinct positive MTG anomalies in the mid-upper troposphere over the SCS monsoon region are well simulated qualitatively in winter and spring, with more obvious warming over the subtropical East Asia than over the Maritime Continent, which is beneficial to the interdecadal advance of the SCSSM onset. This may account for the differences between the simulation and the observation

SUMMARY AND DISCUSSION

Findings

DATA AVAILABILITY STATEMENT