东北师大学报(自然科学版)
東北師大學報(自然科學版)
동북사대학보(자연과학판)
JOURNAL OF NORTHEAST NORMAL UNIVERSITY(NATURAL SCIENCE EDITION)
2009年
4期
134-138
,共5页
靳英华%廉士欢%周道玮%徐金斌%彭聪
靳英華%廉士歡%週道瑋%徐金斌%彭聰
근영화%렴사환%주도위%서금빈%팽총
全球气候变化%空气相对湿度%温度%降水%风速%半干旱区
全毬氣候變化%空氣相對濕度%溫度%降水%風速%半榦旱區
전구기후변화%공기상대습도%온도%강수%풍속%반간한구
global climate change%air relative humidity%temperature%precipitation%wind speed%semiarid region
为揭示全球气候变化下半干旱区空气相对湿度的变化规律,利用线性回归分析、多元线性相关分析以及M-K检验法对吉林省西部5个站点的1953年以来的相对湿度、气温、降水和风速资料进行了研究.结果表明:相对湿度的年变化曲线呈双峰型,相对湿度的最大值出现在8月,次大值出现在1月,最小值出现在4月,次小值出现在10月.夏、秋季的相对湿度较大,而春、冬季的相对湿度较小.近50年,年平均相对湿度及春、夏、秋、冬四季的相对湿度在波动中下降,下降趋势不显著;但是9月和10月的平均相对湿度下降显著.影响相对湿度变化的主要因子是温度和降水,风速也起一定的作用.相对湿度的变化与温度和风速变化呈负相关关系,与降水变化呈正相关关系.
為揭示全毬氣候變化下半榦旱區空氣相對濕度的變化規律,利用線性迴歸分析、多元線性相關分析以及M-K檢驗法對吉林省西部5箇站點的1953年以來的相對濕度、氣溫、降水和風速資料進行瞭研究.結果錶明:相對濕度的年變化麯線呈雙峰型,相對濕度的最大值齣現在8月,次大值齣現在1月,最小值齣現在4月,次小值齣現在10月.夏、鞦季的相對濕度較大,而春、鼕季的相對濕度較小.近50年,年平均相對濕度及春、夏、鞦、鼕四季的相對濕度在波動中下降,下降趨勢不顯著;但是9月和10月的平均相對濕度下降顯著.影響相對濕度變化的主要因子是溫度和降水,風速也起一定的作用.相對濕度的變化與溫度和風速變化呈負相關關繫,與降水變化呈正相關關繫.
위게시전구기후변화하반간한구공기상대습도적변화규률,이용선성회귀분석、다원선성상관분석이급M-K검험법대길림성서부5개참점적1953년이래적상대습도、기온、강수화풍속자료진행료연구.결과표명:상대습도적년변화곡선정쌍봉형,상대습도적최대치출현재8월,차대치출현재1월,최소치출현재4월,차소치출현재10월.하、추계적상대습도교대,이춘、동계적상대습도교소.근50년,년평균상대습도급춘、하、추、동사계적상대습도재파동중하강,하강추세불현저;단시9월화10월적평균상대습도하강현저.영향상대습도변화적주요인자시온도화강수,풍속야기일정적작용.상대습도적변화여온도화풍속변화정부상관관계,여강수변화정정상관관계.
To reveal the semiarid regions of the air relative humidity changes under global climate change, linear regression analysis, multiple linear correlation analysis, and the Mann-Kendall test are used to study on the relative humidity, temperature, precipitation and wind speed data of the five sites in the western Jilin Province from 1953 to 2002. The results show that:the past 50 years, change trend of the annual average and seasonal relative humidity is fluctuant decreasing, and it is not significant; however, in September and October, change trend of the average relative humidity is significant decreasing. The changes of the relative humidity is the double-peak curve type in a year, the maximum relative humidity is in the August, the second largest relative humidity is in the January, the minimum appears in the April, and the smaller one is in October. The relative humidity of the summer and autumn is higher, but the relative humidity of the spring and winter is smaller. Changes of the temperature and precipitation are the main factor to relative humidity change, and the wind speed also plays certain role. Changes of temperature and wind speed are positive correlated with relative humidity change and change of precipitation is negative correlated with relative humidity change.