沙漠与绿洲气象
沙漠與綠洲氣象
사막여록주기상
DESERT AND OASIS METEOROLOGY
2014年
2期
59-64
,共6页
极端高温%极端低温%时空变化%山西
極耑高溫%極耑低溫%時空變化%山西
겁단고온%겁단저온%시공변화%산서
extreme high temperature%extreme low temperature%spatial and temporal character-istics%Shanxi
利用山西省61个气象站点逐日最高温度、最低温度资料,采用百分位值定义法、Mann原Kendall突变检验法和Morlet小波变换等方法,分析了山西省近50 a极端温度事件年均发生频率的时空特征,结果表明:1961年以来,山西省极端高温事件年均发生频率呈显著增加趋势,趋势为6.1 d/10 a,与此同时,极端低温事件年均发生频率呈显著减少趋势,且极端气温事件的变化存在明显的区域差异;极端高温和极端低温年均发生频率均发生了突变现象,变化趋势均在20世纪90年代以来更加显著;极端高温和极端低温事件年均发生频率均呈显著波动变化,在整个研究期间极端高温存在5~6a、4~8a显著周期,极端低温存在4~5a显著周期。
利用山西省61箇氣象站點逐日最高溫度、最低溫度資料,採用百分位值定義法、Mann原Kendall突變檢驗法和Morlet小波變換等方法,分析瞭山西省近50 a極耑溫度事件年均髮生頻率的時空特徵,結果錶明:1961年以來,山西省極耑高溫事件年均髮生頻率呈顯著增加趨勢,趨勢為6.1 d/10 a,與此同時,極耑低溫事件年均髮生頻率呈顯著減少趨勢,且極耑氣溫事件的變化存在明顯的區域差異;極耑高溫和極耑低溫年均髮生頻率均髮生瞭突變現象,變化趨勢均在20世紀90年代以來更加顯著;極耑高溫和極耑低溫事件年均髮生頻率均呈顯著波動變化,在整箇研究期間極耑高溫存在5~6a、4~8a顯著週期,極耑低溫存在4~5a顯著週期。
이용산서성61개기상참점축일최고온도、최저온도자료,채용백분위치정의법、Mann원Kendall돌변검험법화Morlet소파변환등방법,분석료산서성근50 a겁단온도사건년균발생빈솔적시공특정,결과표명:1961년이래,산서성겁단고온사건년균발생빈솔정현저증가추세,추세위6.1 d/10 a,여차동시,겁단저온사건년균발생빈솔정현저감소추세,차겁단기온사건적변화존재명현적구역차이;겁단고온화겁단저온년균발생빈솔균발생료돌변현상,변화추세균재20세기90년대이래경가현저;겁단고온화겁단저온사건년균발생빈솔균정현저파동변화,재정개연구기간겁단고온존재5~6a、4~8a현저주기,겁단저온존재4~5a현저주기。
Based on the 61 meteorological stations’ data of daily maximum temperature and minimum temperature in Shanxi province and using percentile values defineition method,Mann-Kendall mutationg test and wavelet analysis method,the spatial and temporal characteristics of extreme temperature events were studied for the recent 50 years in Shanxi Province. The results showed that annual extreme high temperature frequency have been increasing since 1961 and its trend was 6.1 d/10 a,while there was a decreasing trend in extreme low temperature frequency. Meantime, there were obvious spatial variations in both annual extreme high and low temperature frequency. For the recent 50 years,the abruptions were found in all stations in both annual extreme high and low temperature frequency and their trends were more significant since 1990s. In addition, fluctuation changes were found with a 5~6 years and 4~8 years period in annual extreme high temperature and 4~5 years period in low temperature.