干旱气象
榦旱氣象
간한기상
GANSU METEOROLOGY
2012年
1期
27-33
,共7页
张翠华%张文煜%卞韬%韩军彩
張翠華%張文煜%卞韜%韓軍綵
장취화%장문욱%변도%한군채
地面温度%变化特征%气候突变%变化周期
地麵溫度%變化特徵%氣候突變%變化週期
지면온도%변화특정%기후돌변%변화주기
ground temperature%various characteristics%abrupt change%period
利用石家庄地区5个观测站1961~2010年逐日地面温度观测数据,分析讨论了该地区地面温度平均值、最高值、最低值和日较差的变化特征以及地面温度的气候突变和变化周期。结果表明:从年代际变化情况看,平均地面温度振动幅度最小,地面温度日较差振动幅度最大,平均地面温度和最低地面温度呈显著增加趋势,最高地面温度呈显著降低趋势,地面温度日较差呈现显著减小趋势;从年和季节变化情况看,地面温度日较差年和各季节变率最大,平均地面温度冬季增温趋势显著,夏季呈降温趋势,最高地面温度年和各季节呈降温趋势,夏、秋季降温趋势显著,最低地面温度年和各季节呈显著增温趋势,冬季增温趋势最为显著,地面温度日较差年和各季节均呈显著减小趋势,冬季减小趋势最为显著;平均地面温度和最低地面温度没有发生突变现象,最高地面温度2000年代初期明显降温为一突变现象,东南部平原平均地面温度1990年代初期明显升温为一突变现象,其他各地没有发生突变现象;平均地面温度存在准20 a和6~8 a周期,最高地面温度存在准16 a和准6 a周期,最低地面温度存在准24 a和10~15 a周期。
利用石傢莊地區5箇觀測站1961~2010年逐日地麵溫度觀測數據,分析討論瞭該地區地麵溫度平均值、最高值、最低值和日較差的變化特徵以及地麵溫度的氣候突變和變化週期。結果錶明:從年代際變化情況看,平均地麵溫度振動幅度最小,地麵溫度日較差振動幅度最大,平均地麵溫度和最低地麵溫度呈顯著增加趨勢,最高地麵溫度呈顯著降低趨勢,地麵溫度日較差呈現顯著減小趨勢;從年和季節變化情況看,地麵溫度日較差年和各季節變率最大,平均地麵溫度鼕季增溫趨勢顯著,夏季呈降溫趨勢,最高地麵溫度年和各季節呈降溫趨勢,夏、鞦季降溫趨勢顯著,最低地麵溫度年和各季節呈顯著增溫趨勢,鼕季增溫趨勢最為顯著,地麵溫度日較差年和各季節均呈顯著減小趨勢,鼕季減小趨勢最為顯著;平均地麵溫度和最低地麵溫度沒有髮生突變現象,最高地麵溫度2000年代初期明顯降溫為一突變現象,東南部平原平均地麵溫度1990年代初期明顯升溫為一突變現象,其他各地沒有髮生突變現象;平均地麵溫度存在準20 a和6~8 a週期,最高地麵溫度存在準16 a和準6 a週期,最低地麵溫度存在準24 a和10~15 a週期。
이용석가장지구5개관측참1961~2010년축일지면온도관측수거,분석토론료해지구지면온도평균치、최고치、최저치화일교차적변화특정이급지면온도적기후돌변화변화주기。결과표명:종년대제변화정황간,평균지면온도진동폭도최소,지면온도일교차진동폭도최대,평균지면온도화최저지면온도정현저증가추세,최고지면온도정현저강저추세,지면온도일교차정현현저감소추세;종년화계절변화정황간,지면온도일교차년화각계절변솔최대,평균지면온도동계증온추세현저,하계정강온추세,최고지면온도년화각계절정강온추세,하、추계강온추세현저,최저지면온도년화각계절정현저증온추세,동계증온추세최위현저,지면온도일교차년화각계절균정현저감소추세,동계감소추세최위현저;평균지면온도화최저지면온도몰유발생돌변현상,최고지면온도2000년대초기명현강온위일돌변현상,동남부평원평균지면온도1990년대초기명현승온위일돌변현상,기타각지몰유발생돌변현상;평균지면온도존재준20 a화6~8 a주기,최고지면온도존재준16 a화준6 a주기,최저지면온도존재준24 a화10~15 a주기。
Based on the daily ground temperature observation data of 5 stations in Shijiazhuang from 1961 to 2010,the variation characteristics of average,maximum,minimum and diurnal ranges of ground temperature were analyzed.The results show that the amplitude of average ground temperature was minimum but maximum for diurnal range,and the average and minimum value of ground temperature presented significant warming trend,but the diurnal range and maximum of ground temperature decreased obviously from decadal trend.The annual and seasonal change showed that the amplitude of ground temperature daily range was maximum,mean value of ground temperature in winter increased significantly but decreased in summer,and maximum value of ground temperature decreased,especially in summer and autumn,but minimum value of ground temperature increased obviously especially in winter,The average and minimum value of ground temperature had no abrupt phenomenon,but the maximum of groud temperature had an abrupt cooling change at the early stage of the 2000s,and in southeast region of Shijiazhuang mean ground temperature had an abrupt warming change in early stage of the 1990s.The mean ground temperature had variation period of 6-8 years and 20 years,and 6 years and 16 years for the maximum ground temperature,as well as 10-15 years and 24 years for minimum ground temperature.