On the Relationship Between the Stratospheric Quasi-Biennial Oscillation and Summer Precipitation in Northern China

被引:12
|
作者
Hu, Jinggao [1 ]
Gao, Xiang [1 ]
Ren, Rongcai [1 ,2 ]
Luo, Jingjia [1 ,3 ]
Deng, Jiechun [1 ]
Xu, Haiming [1 ]
机构
[1] Nanjing Univ Informat Sci & Technol, Key Lab Meteorol Disaster, Minist Educ KLME,Collaborat Innovat Ctr Forecast, Joint Int Res Lab Climate & Environm Change ILCEC, Nanjing, Peoples R China
[2] Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing, Peoples R China
[3] Nanjing Univ Informat Sci & Technol, Inst Climate & Applicat Res ICAR, Nanjing, Peoples R China
关键词
stratospheric quasi-biennial oscillation; North and Northeastern China; meridional zonal-wind dipole; Japan Sea high; MADDEN-JULIAN OSCILLATION; WINTER; CIRCULATION; TROPOSPHERE; MODULATION; MONSOON; CYCLE; ENSO; QBO;
D O I
10.1029/2021GL097687
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
This paper reports that there has been a significant relationship between the quasi-biennial oscillation (QBO) in zonal wind at 50 hPa in summer and precipitation in August in northern China since the late 1970s. The correlation coefficient between them reaches up to -0.61 during 1979-2018. Associated with the easterly (westerly) phase of the QBO, there is a meridional dipole pattern of zonal wind from the stratosphere to troposphere over the Northwest Pacific in August with the easterly (westerly) anomalies in 25-50 degrees N and westerly (easterly) anomalies in 50-65 degrees N. This meridional zonal-wind dipole favors the strengthening (weakening) of the tropospheric Japan Sea high in the QBO easterly (westerly) phase, causing an increase (decrease) of the water vapor transportation from the Northwest Pacific to northern China and thus more (less) precipitation in these regions. The finding of this study has import implications for predicting the summer precipitation in northern China in the future.
引用
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页数:9
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