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Advances in Meteorology - Volume 2015 2015, Article ID 483970, 10 pages -

Research Article

Chinese Academy of Meteorological Sciences, Beijing 100081, China

Meteorological Bureau, Hebei 050011, China

State Key Laboratory of Satellite Ocean Environment Dynamics, Second Institute of Oceanography, State Oceanic Administration, Hangzhou 310012, China

Received 12 March 2015; Revised 26 June 2015; Accepted 22 July 2015

Academic Editor: Andrea Montani

Copyright © 2015 Yafei Wang et al. This is an open access article distributed under the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.


Using station precipitation and reanalysis data, we examined the evolution of the large-scale circulations associated with the heavy rainfall event that occurred around July 21, 2012 721 heavy rainfall. This study focuses on a role that the large-scale circulations named -the Okhotsk-Japan OKJ circulation pattern- played in causing the heavy rainfall case. We found that the 721 heavy rainfall occurred under a background of the OKJ circulation that persisted for about 10 days. However, the pattern was different from the normal OKJ circulation, for this circulation pattern accompanied a blocking high between the Ural Mountains and the Baikal Lake. This difference resulted from the seasonal change of the basic flow. The related Rossby wave propagated eastward during the persisting period of the dominated OKJ pattern. This caused the development of a low-pressure system around the Baikal Lake and the weakening of a ridge around the Okhotsk Sea. The slow evolution of the OKJ circulation created a favorable environment for the moisture transport to northern China, assisting in the generation of the 721 heavy rainfall.

Author: Yafei Wang, Jianzhao Qin, and Lijuan Zhu



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