气象与环境学报
氣象與環境學報
기상여배경학보
JOURNAL OF METEOROLOGY AND ENVIRONMENT
2014年
3期
71-77
,共7页
霾%小波分析%气象条件%大气逆温
霾%小波分析%氣象條件%大氣逆溫
매%소파분석%기상조건%대기역온
Haze%Wavelet analysis%Meteorological conditions%Temperature inversion
利用1980-2011年江西省83个常规站和南昌、赣州两个探空站的观测资料,对江西省霾的气候特征及其与气象条件的关系进行了分析。结果表明:近32 a江西省霾日总体呈上升趋势;霾日的季节、年际和年代际变化明显,秋冬季多(12月最多)春夏季少(7月最少),4a左右和8a左右的年际变化周期显著,年代际变化主要为15 a左右的变化周期;江西霾日空间分布不均,呈现中北部多,南部及山区少的分布形势。霾与地面风速、大气逆温、海平面气压、降水量和相对湿度密切相关,低风速、大气逆温、高气压、高湿度和少降雨有利于霾天气的发生,反之,高风速、低气压、低湿度和多降雨不利于霾天气的发生。
利用1980-2011年江西省83箇常規站和南昌、贛州兩箇探空站的觀測資料,對江西省霾的氣候特徵及其與氣象條件的關繫進行瞭分析。結果錶明:近32 a江西省霾日總體呈上升趨勢;霾日的季節、年際和年代際變化明顯,鞦鼕季多(12月最多)春夏季少(7月最少),4a左右和8a左右的年際變化週期顯著,年代際變化主要為15 a左右的變化週期;江西霾日空間分佈不均,呈現中北部多,南部及山區少的分佈形勢。霾與地麵風速、大氣逆溫、海平麵氣壓、降水量和相對濕度密切相關,低風速、大氣逆溫、高氣壓、高濕度和少降雨有利于霾天氣的髮生,反之,高風速、低氣壓、低濕度和多降雨不利于霾天氣的髮生。
이용1980-2011년강서성83개상규참화남창、공주량개탐공참적관측자료,대강서성매적기후특정급기여기상조건적관계진행료분석。결과표명:근32 a강서성매일총체정상승추세;매일적계절、년제화년대제변화명현,추동계다(12월최다)춘하계소(7월최소),4a좌우화8a좌우적년제변화주기현저,년대제변화주요위15 a좌우적변화주기;강서매일공간분포불균,정현중북부다,남부급산구소적분포형세。매여지면풍속、대기역온、해평면기압、강수량화상대습도밀절상관,저풍속、대기역온、고기압、고습도화소강우유리우매천기적발생,반지,고풍속、저기압、저습도화다강우불리우매천기적발생。
Based on the observation data from 83 meteorological stations and radiosounde stations at Nanchang and Ganzhou of Jiangxi province during 1980-2011,the climate characteristics of haze days and its relationship with meteorological elements were analyzed.The results show that the haze days are in an upward trend in the past 32 years and have significant inter-annual and inter-decadal variations.A larger number of haze days occur in autumn and winter with the maximum number happened in December and smaller number appears in spring and summer with the minimum number in July,respectively.There are significant 4-year and 8-year cycles for annual haze days and 15-year cycle for inter-decadal variation.The spatial distributions of haze days are inhomogeneous in Jiangxi province with a larger number in the north and smaller in the south and mountain area.It is found that the low wind speed,temperature inversion,high pressure,high humidity and less rainfall are favourable conditions to the occurrence of haze.Conversely,the high wind speed,low pressure,low humidity and abundant rainfall are not fa-vourable.