气象与减灾研究
氣象與減災研究
기상여감재연구
METEOROLOGY AND DISASTER REDUCTION RESEARCH
2015年
1期
66-72
,共7页
雾日数%时空分布%海拔%地形
霧日數%時空分佈%海拔%地形
무일수%시공분포%해발%지형
fog days%spatial and temporal distribution%characteristic%landform
利用1960—2012年江西省89个气象站逐日雾的观测资料以及高速交通气象站的能见度观测资料,采用经验正交函数(EOF)方法,分析了江西省雾日数的时空分布特征。结果表明,江西省雾日数的空间分布特征与江西的地形地貌密切相关,分布特点总体是高海拔地区或山区雾日数多,丘陵平原湖泊地区雾日数少。雾日数最多的季节为冬季,其次为秋季和春季;20世纪70年代中期至80年代中期雾日数明显偏多,21世纪以来雾日数呈明显减少的趋势。雾日数的年际变化受地形的影响较大,高海拔地区或山区雾日数变化比丘陵平原湖泊地区的要大,属于雾日数异常敏感区域;在20世纪60年代至80年代中期表现为丘陵、平原、湖泊等地区的雾日数偏少,高海拔地区或山区的雾日数偏多,80年代以后则呈相反的分布型式。
利用1960—2012年江西省89箇氣象站逐日霧的觀測資料以及高速交通氣象站的能見度觀測資料,採用經驗正交函數(EOF)方法,分析瞭江西省霧日數的時空分佈特徵。結果錶明,江西省霧日數的空間分佈特徵與江西的地形地貌密切相關,分佈特點總體是高海拔地區或山區霧日數多,丘陵平原湖泊地區霧日數少。霧日數最多的季節為鼕季,其次為鞦季和春季;20世紀70年代中期至80年代中期霧日數明顯偏多,21世紀以來霧日數呈明顯減少的趨勢。霧日數的年際變化受地形的影響較大,高海拔地區或山區霧日數變化比丘陵平原湖泊地區的要大,屬于霧日數異常敏感區域;在20世紀60年代至80年代中期錶現為丘陵、平原、湖泊等地區的霧日數偏少,高海拔地區或山區的霧日數偏多,80年代以後則呈相反的分佈型式。
이용1960—2012년강서성89개기상참축일무적관측자료이급고속교통기상참적능견도관측자료,채용경험정교함수(EOF)방법,분석료강서성무일수적시공분포특정。결과표명,강서성무일수적공간분포특정여강서적지형지모밀절상관,분포특점총체시고해발지구혹산구무일수다,구릉평원호박지구무일수소。무일수최다적계절위동계,기차위추계화춘계;20세기70년대중기지80년대중기무일수명현편다,21세기이래무일수정명현감소적추세。무일수적년제변화수지형적영향교대,고해발지구혹산구무일수변화비구릉평원호박지구적요대,속우무일수이상민감구역;재20세기60년대지80년대중기표현위구릉、평원、호박등지구적무일수편소,고해발지구혹산구적무일수편다,80년대이후칙정상반적분포형식。
Based on the 1960-2012 daily fog data from 89 meteorological stations in Jiangxi province and the visibility data from traffic weather stations along Jiangxi Taijing freeway , the temporal and spatial distribution of seasonal fog days was discussed by using the empirical orthogonal function (EOF) method. The results showed that the spatial distribution of foggy days in Jiangxi was closely related to the local landform condition. Generally, more fog days occurred in high altitude or mountainous areas, while less fog days appeared in hilly, plain and lake areas. The highest number of seasonal fog days occurred in winter, followed by in spring and autumn. More fog days occurred abnormally during the middle 1970s-the middle 1980s, however, from the beginning of this century, fog days decreased significantly. The analyses of EOF showed that compared with that in hilly, plain and lake areas, the interannual variation of fog days in Jiangxi was largely effected in high altitude or mountainous areas. During 1960s to the mid-1980s, the fog days in hilly area, plain and lake areas presented lower probability, and higher probability in high altitude or mountainous areas. However, it showed the opposite distribution pattern after 1980s.