咸阳师范学院学报
鹹暘師範學院學報
함양사범학원학보
JOURNAL OF XIANYANG TEACHERS COLLEGE
2011年
4期
78-83
,共6页
曹兴%荆海亮%李辉%张军%向导
曹興%荊海亮%李輝%張軍%嚮導
조흥%형해량%리휘%장군%향도
达坂城%气候变化%突变%大风%规律
達坂城%氣候變化%突變%大風%規律
체판성%기후변화%돌변%대풍%규률
Dabancheng%climate change%abrupt%Sstrong wind%regulation
利用达坂城气象站1981—2010年逐年气温、降水和大风资料,分析了近30年来气温、降水及大风的年、季变化特征,结果表明:年均气温总体呈上升趋势,线性倾向率为0.33℃/10a,年内气温的季节变化存在差异,秋季增温明显,春夏季次之;降水量线性倾向率为9.44mm/10a,气候变湿显著,降水年际变率较大且季节分配不均;Mann—Kendall突变检验表明,气温在1991年发生一次突变,变暖趋势显著,降水在1986年发生由少向多的突变过程;大风日数、平均风速呈现波动下降过程,大风日数线性趋向率为-30.5d/10a,平均风速递减率为-0.76(m/s)/10a,春季大风发生频率最高,为33%,静风频率为10.32%;主导风向以偏西风(WNW)和东南风(SE)为主。
利用達坂城氣象站1981—2010年逐年氣溫、降水和大風資料,分析瞭近30年來氣溫、降水及大風的年、季變化特徵,結果錶明:年均氣溫總體呈上升趨勢,線性傾嚮率為0.33℃/10a,年內氣溫的季節變化存在差異,鞦季增溫明顯,春夏季次之;降水量線性傾嚮率為9.44mm/10a,氣候變濕顯著,降水年際變率較大且季節分配不均;Mann—Kendall突變檢驗錶明,氣溫在1991年髮生一次突變,變暖趨勢顯著,降水在1986年髮生由少嚮多的突變過程;大風日數、平均風速呈現波動下降過程,大風日數線性趨嚮率為-30.5d/10a,平均風速遞減率為-0.76(m/s)/10a,春季大風髮生頻率最高,為33%,靜風頻率為10.32%;主導風嚮以偏西風(WNW)和東南風(SE)為主。
이용체판성기상참1981—2010년축년기온、강수화대풍자료,분석료근30년래기온、강수급대풍적년、계변화특정,결과표명:년균기온총체정상승추세,선성경향솔위0.33℃/10a,년내기온적계절변화존재차이,추계증온명현,춘하계차지;강수량선성경향솔위9.44mm/10a,기후변습현저,강수년제변솔교대차계절분배불균;Mann—Kendall돌변검험표명,기온재1991년발생일차돌변,변난추세현저,강수재1986년발생유소향다적돌변과정;대풍일수、평균풍속정현파동하강과정,대풍일수선성추향솔위-30.5d/10a,평균풍속체감솔위-0.76(m/s)/10a,춘계대풍발생빈솔최고,위33%,정풍빈솔위10.32%;주도풍향이편서풍(WNW)화동남풍(SE)위주。
Using the observed temperature, precipitation and strong wind dams from the Da- bancheng Meteorology Station during the period from 1981 to 2010, this paper analyzed the annual and seasonal changes of the metrological factors during the last 30 years. The results show that: During the last 30 years, the temperature had a trend of increasing and the rate was 0. 33 ℃/10a. The change of temperature in a year showed seasonal disparities that it had aobvious trend of increasing in autumn, following by spring and summer. And the increasing rate of precipitation was 9.44mm/10a. The precipitation had obvious variations in inter-annual and the seasonal change of precipitation was distinctive. The Mann-Kendall test shows that: the annual mean temperature exhibited an obvious increase trend in the recent 30 years, and an abrupt temperature change happened in 1991 ;an abrupt change from less to more of annual precipitation occurred in 1986; The strong wind days and average wind speed show a wave decreased during 30 years, the decreasing rate of them were-30.5d/10a,-0.76 (m/s)/10a, The highest frequency of the strong wind happened in spring, the rate was 33%, and Static Wkxd was 10,32%;Dominant wind direction is WNW and SE.