中国东部及西北太平洋地区边界层高度变化特征  

Variation Characteristics of the Atmospheric Boundary Layer Height in Eastern China and Northwest Pacific

作　　者：李玉鹏 李吉 杨旭 于杰 申燕玲 高梦竹 Li Yupeng;Li Ji;Yang Xu;Yu Jie;Shen Yanling;Gao Mengzhu(Meteorological Administration Basin Heavy Rainfall Key Laboratory/Hubei Key Laboratory for Heavy Rain Monitoring and Warning Research,Institute of Heavy Rain,CMA,Wuhan 430205,China;Jilin Provincial Key Laboratory of Changbai Mountain Meteorology&Climate Change,Institute of Meteorological Sciences of Jilin Province,Changchun 130062,China;Jilin Provincial Meteorological Observatory,Changchun 130062,China;Key Laboratory for Disaster Prevention and Mitigation in Qinghai Province,Qinghai Institute of Meteorological Science,Xining 810001,China;Heilongjiang Provincial Meteorological Observatory,Harbin 150001,China)

机构地区：[1]中国气象局流域强降水重点开放实验室/暴雨监测预警湖北省重点实验室中国气象局武汉暴雨研究所,武汉430205 [2]长白山气象与气候变化吉林省重点实验室吉林省气象科学研究所,长春130062 [3]吉林省气象台,长春130062 [4]青海省防灾减灾重点实验室青海省气象科学研究所,西宁810001 [5]黑龙江省气象台,哈尔滨150001

出　　处：《气象与环境科学》2024年第2期1-8,共8页Meteorological and Environmental Sciences

基　　金：中国气象局流域强降水重点开放实验室基金(2023BHR-Y12);国家重点研发计划专题(2017YFC0212304、2017YFC0212302)。

摘　　要：利用19792019年ERA5逐月大气边界层高度(ABLH,Atmospheric boundary layer height)资料,采用气候态分析、距平分析、极值分析、经验正交(EOF)分析及小波分析等方法,研究了中国东部及西北太平洋区域大气边界层高度的变化特征。结果表明:(1)太阳辐射对边界层高度有重要影响,边界层高度的季节变化存在显著的海陆差异,大陆(海洋)上,夏季时边界层高度最高(低),而在冬季时最低(高)。(2)边界层高度的海陆差异随季节改变,春秋季海陆差异较小,冬夏季时最明显。(3)大陆上边界层高度极大值出现在夏半年的月份,极小值出现在冬半年的月份;海洋上的相反。(4)41年边界层高度场的EOF分析得到两个模态,第一模态表现为南北经向和海陆差异,第二模态为自西北至东南的“+-+-”相位分布,第一模态的时间系数以3~7 a的周期最显著,第二模态同时存在4~7 a和9~11 a的振荡周期。This paper investigates the atmospheric boundary layer height(ABLH)in eastern China and the northwest Pacific region using the ERA5 monthly ABLH data from 1979 to 2019,as well as the methods of climatological state analysis,anomaly analysis,extreme value analysis,Empirical Orthogonal Function(EOF),and wavelet analysis.The study results show that:(1)Solar radiation has an important impact on ABLH.There are significant differences between land and ocean in the seasonal changes of ABLH.The ABLH is the highest(lowest)on land(ocean)in summer,and are lowest(highest)in winter.(2)Land-ocean difference of boundary layer height varies with the changes of seasons,and the difference is smaller in spring and autumn,but significant in summer and winter.(3)The maximum value of the boundary layer height on land appears in the summer half year,while the minimum is in the winter half year.However,the situation over the ocean is opposite.(4)Two modes are obtained through studying the EOF analysis of 41-year boundary layer heights.The first mode is the north-south meridional difference and the land-sea difference,and the second mode has a“+-+-”distribution from northwest to southeast.The time coefficient of the first mode is most significant with a period of 37 years;and second mode has both oscillation periods of 47 years and 911 years.

关 键 词：大气边界层高度 季节变化 周期性 EOF 

分 类 号：P421.31[天文地球—大气科学及气象学]