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刘海文, 丁一汇. 华北汛期降水月内时间尺度周期振荡的年代际变化分析[J]. 大气科学, 2011, 35(1): 157-167. DOI: 10.3878/j.issn.1006-9895.2011.01.13
引用本文: 刘海文, 丁一汇. 华北汛期降水月内时间尺度周期振荡的年代际变化分析[J]. 大气科学, 2011, 35(1): 157-167. DOI: 10.3878/j.issn.1006-9895.2011.01.13
Liu Haiwen, Ding Yihui. Analysis on the Interdecadal Change of Submonthly Time Scales Oscillation of Precipitation over North China during Rainy Seasons and Its Cause[J]. Chinese Journal of Atmospheric Sciences, 2011, 35(1): 157-167. DOI: 10.3878/j.issn.1006-9895.2011.01.13
Citation: Liu Haiwen, Ding Yihui. Analysis on the Interdecadal Change of Submonthly Time Scales Oscillation of Precipitation over North China during Rainy Seasons and Its Cause[J]. Chinese Journal of Atmospheric Sciences, 2011, 35(1): 157-167. DOI: 10.3878/j.issn.1006-9895.2011.01.13

华北汛期降水月内时间尺度周期振荡的年代际变化分析

Analysis on the Interdecadal Change of Submonthly Time Scales Oscillation of Precipitation over North China during Rainy Seasons and Its Cause

  • 摘要: 利用中国740站逐日降水资料和NCEP/NCAR逐日再分析资料, 使用小波分析等方法, 对华北汛期降水的月内时间尺度周期振荡的年代际变化及其原因进行了分析。结果表明: 由于西太平洋副热带高压和华北夏季风的月内时间尺度周期振荡存在显著的年代际变化, 使得华北汛期降水在两个不同阶段, 存在着显著不同的月内时间尺度的周期振荡。在华北汛期降水偏多阶段, 华北在整个汛期从开始到结束, 都存在单一的、 显著的3~8 d天气时间尺度的周期振荡高频降水; 华北日降水量具有典型的单峰结构, 汛期日降水于7月下旬达到最大, 随后逐步减弱, 遵循着 “7下8上” 之规律。华北汛期降水偏少阶段, 显著的天气时间尺度的高频降水, 直到7月中旬才开始出现, 出现时间较迟; 7月22日以后, 华北汛期日降水又存在着3~8 d和10~20 d两种时间尺度周期振荡的叠加; 日降水值于7月上旬出现次极大值, 随后降水有所减弱, 到8月上旬出现最大值, 随后降水再减弱, 显示出一定的低频振荡特征; 而且在7月26日至8月6日期间, 10~20 d低频降水又以负位相开始, 正位相结束, 这些都表现出和降水偏多阶段 “7下8上” 之规律不一样的特点。

     

    Abstract: Based on the daily precipitation data from 740 stations in China and NCEP/NCAR reanalysis daily datasets, the interdecadal change of submonthly time scales oscillation of precipitation over North China during rainy seasons and its cause are analyzed by means of the wavelet analysis method. Some results are discovered as follows: There exists significantly different submonthly timescales oscillation for the rainfall over North China during rainy seasons in the two different interdecadal periods due to interdecadal change of the western Pacific subtropical high and submonthly timescale oscillation of North China summer monsoon. There exists a significant high frequency rainfall with the 3-8-day synoptic timescale periodic oscillation in the flood period from the beginning to ending of the rainy season over North China. The daily rainfall over North China has a typical single-peak structure, which reaches the maximum in the last ten days of July and decreases gradually. The daily rainfall over North China obeys the rule which daily rainfall over North China frequently occurs in the last ten days of July and the first ten days of August. However, the distinct synoptic timescale high frequency rainfall does not take place until mid-July, which appears little later, and there is superimposition of 3-8-day synoptic timescale and 10-20-day timescale periodic oscillation for the daily rainfall over North China after 22 July. The daily rainfall over North China reaches the sub-maximum in the early ten days of July and decreases a little, then it reaches the maximum in the early ten days of August and decreases again, which shows a characteristic of low frequency oscillation. Furthermore, the low frequency precipitation begins with a negative phase and ends with a positive phase from 26 July to 6 August, which displays the different characteristics from the laws during the flood period that the peak rainfall over North China during the rainy season takes place in the last ten days of July and the first ten days of August.

     

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