Analysis of the interannual variations and influencing factors of wind speed anomalies over the Beijing–Tianjin–Hebei region  

作　　者：ZHOU Bai-Yu ZHENG Fei ZHU Jiang 

机构地区：[1]International Center for Climate and Environment Science (ICCES ), Institute of Atmospheric Physics, Chinese Academy of Sciences [2]College of Earth Science, University of Chinese Academy of Sciences (UCAS)

出　　处：《Atmospheric and Oceanic Science Letters》2017年第4期312-318,共7页大气和海洋科学快报（英文版）

基　　金：supported by the National Natural Science Foundation of China[grant number 41176014]

摘　　要：The wind field plays a decisive role in haze generation and dissipation processes over the Beijing- Tianjin-Hebei （BTH） region. Although geographically the BTH region is under the influence of the East Asian winter monsoon （EAWM）, this study finds that common indices of the EAWM cannot adequately describe the actual wind speed changes in the BTH region.Thus, observational data are used to analyze the interannual variations of the winter wind field over the BTH region. The results show that the average winter wind speed is 2.0 m s-1, with a slight rate of decline of 0.01 m s-1 yr-1. In most cases, strong-wind years correspond to negative sea surface temperature （SST） anomalies over the tropical Pacific, whereas weak-wind years correspond to positive SST anomalies. Moreover, correlation and composite analyses show that the interannual variability is affected by multiple factors, including the following： （1） the pressure gradient in the high and middle latitudes of the Northern Hemisphere, as in strong-wind years the pressure gradient helps cold air move from high latitudes to middle latitudes; （2） the skin temperature in Eurasia, as low skin temperature in Eurasia in strong-wind years is conducive to the accumulation of cold air; and （3） the SST of the tropical Pacific east of the Philippines, as in strong-wind years the high temperature of this area affects the BTH region through anticyclonic activity and associated tropical circulation systems.风场对京津冀地区雾霾的产生和消散起着决定性作用。本文利用站点观测数据,研究了京津冀地区冬季风场的年际变化及其影响因素。研究表明,京津冀地区的冬季平均风速为2.0 m s^(-1),每年降幅为0.01 m s^(-1)。大多数情况下,强风年对应热带太平洋东部的负海温异常,而弱风年份相反。此外,京津冀地区冬季风场的年际变化还受到包括北半球中高纬度气压梯度、欧亚大陆地表温度、菲律宾东部热带太平洋海面温度等多重因素的影响。

关 键 词：Interannual variation winterwind field Beijing-Tianjin-Hebei region 

分 类 号：P425[天文地球—大气科学及气象学]