主办单位:中国气象局沈阳大气环境研究所
国际刊号:ISSN 1673-503X
国内刊号:CN 21-1531/P

Journal of Meteorology and Environment ›› 2021, Vol. 37 ›› Issue (5): 63-71.doi: 10.3969/j.issn.1673-503X.2021.05.010

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Analysis of spatio-temporal variation characteristics and atmospheric circulation factors of precipitation in early and mid-summer in Northeast China

Yi-tong LIN1,2,3(),Chun-yu ZHAO1,2,3,Yi-he FANG2,3,*(),Qian LI2,3,Xiao FANG4,Xuan LI5,Lin-lin SUN6,Rong LIN2   

  1. 1. Institute of Atmospheric Environment, China Meteorological Administration, Shenyang 110166, China
    2. Shenyang Regional Climate Center, Shenyang 110166, China
    3. Key Opening Laboratory for Northeast China Cold Vertex Research, Shenyang 110166, China
    4. Liaoning Meteorological Information Center, Shenyang 110166, China
    5. Chaoyang Meteorological Service, Chaoyang 122000, China
    6. Panjin Meteorological Service, Panjin 124000, China
  • Received:2020-08-07 Online:2021-10-30 Published:2021-11-01
  • Contact: Yi-he FANG E-mail:476601374@qq.com;49954570@qq.com

Abstract:

Based on the daily precipitation data of 245 weather stations in Northeast China from 1961 to 2019, the temporal and spatial characteristics of precipitation in early summer (June) and mid-summer (July and August) in Northeast China were analyzed using EOF, cumulative anomaly, moving t-test, Wavelet analysis, and correlation analysis methods. The results show that precipitation in mid-summer in Northeast China are mainly concentrated in the southeast, and more precipitation is distributed in the north and northeast in early summer. The first and fourth modes of EOF in early and mid-summer are consistent across the whole area and feature a change of negative-positive-negative (positive-negative-positive) from north to south, respectively. There are two abrupt changes of precipitation in early summer in 1972 and 1995 and three abrupt changes in mid-summer precipitation in 1966, 1983, and 1998, respectively. There are prominent quasi-6-year and quasi-3-year oscillation periods in mid-summer precipitation in northeast China from the 1980s to 1990s and late 1990s, respectively. The main oscillation period of midsummer precipitation is about 12 years, and the interannual scale oscillation period for 3-4 years appears after the 1990s. With investigating the characteristics of circulation field related to precipitation on time division, it is found that the influence of Northeast Cold Vortex on the precipitation in early summer is enhanced, and the impact factors of precipitation in mid-summer transforms from the Western Pacific subtropical high to the mid-latitude westerlies system, indicating a new characteristic.

Key words: Mutation, Periodic characteristics, Atmospheric circulation configuration

CLC Number: