气象与环境学报
氣象與環境學報
기상여배경학보
JOURNAL OF METEOROLOGY AND ENVIRONMENT
2015年
2期
108-111
,共4页
大气边界层%逆温%频率%厚度%强度
大氣邊界層%逆溫%頻率%厚度%彊度
대기변계층%역온%빈솔%후도%강도
Atmospheric boundary layer%Inversion%Frequency%Thickness%Intensity
针对污染气象条件对大气环境影响的问题,利用2010—2012年成都地区探空资料的温度数据,系统研究了成都地区逆温的结构及分布特征。结果表明:2010—2012年成都地区整体以贴地逆温出现频率最高、厚度最大及强度最强,其次为低悬逆温和高悬逆温。不同类型逆温出现的频率、厚度及强度也存在一定的季节差异,贴地逆温春季出现频率最高,厚度最大,其他各季差异不显著;冬季逆温最强,夏季最弱。3类逆温的日变化明显,08时逆温出现的频率和厚度普遍大于20时,且08时逆温强度大于20时。分析成都地区大气边界层逆温层特征,对了解成都地区污染物扩散规律具有重要的意义。
針對汙染氣象條件對大氣環境影響的問題,利用2010—2012年成都地區探空資料的溫度數據,繫統研究瞭成都地區逆溫的結構及分佈特徵。結果錶明:2010—2012年成都地區整體以貼地逆溫齣現頻率最高、厚度最大及彊度最彊,其次為低懸逆溫和高懸逆溫。不同類型逆溫齣現的頻率、厚度及彊度也存在一定的季節差異,貼地逆溫春季齣現頻率最高,厚度最大,其他各季差異不顯著;鼕季逆溫最彊,夏季最弱。3類逆溫的日變化明顯,08時逆溫齣現的頻率和厚度普遍大于20時,且08時逆溫彊度大于20時。分析成都地區大氣邊界層逆溫層特徵,對瞭解成都地區汙染物擴散規律具有重要的意義。
침대오염기상조건대대기배경영향적문제,이용2010—2012년성도지구탐공자료적온도수거,계통연구료성도지구역온적결구급분포특정。결과표명:2010—2012년성도지구정체이첩지역온출현빈솔최고、후도최대급강도최강,기차위저현역온화고현역온。불동류형역온출현적빈솔、후도급강도야존재일정적계절차이,첩지역온춘계출현빈솔최고,후도최대,기타각계차이불현저;동계역온최강,하계최약。3류역온적일변화명현,08시역온출현적빈솔화후도보편대우20시,차08시역온강도대우20시。분석성도지구대기변계층역온층특정,대료해성도지구오염물확산규률구유중요적의의。
For the problem of the pollution meteorological conditions influencing atmospheric environment,struc-ture distribution characteristics of temperature inversion in Chengdu were analyzed based on temperature of sound-ing data from 2010 to 2012.The results show that surface inversion during 2010-2012 in Chengdu area as a whole has the highest frequency,the largest thickness and the strongest intensity,and then low-hung temperature inversion and high-hung temperature inversion follow.Frequency,thickness and intensity of temperature inversion of differ-ent types have a certain seasonal difference.For surface inversion,its frequency and thickness is the largest in spring and there is no significant difference in other seasons.In general,intensity of temperature inversion is the strongest in winter and weakest in summer.Diurnal variation of inversion of three types is obvious,and frequency and thickness of inversion is greater at 08:00 than at 20:00,so is intensity of inversion.Analysis of characteristic of atmospheric boundary layer inversion in Chengdu area is of important significance to understand diffusion of pollutant in this region.