干旱气象
榦旱氣象
간한기상
GANSU METEOROLOGY
2014年
1期
99-107
,共9页
白松竹%陈真%庄晓翠%王磊
白鬆竹%陳真%莊曉翠%王磊
백송죽%진진%장효취%왕뢰
阿勒泰地区%集中度%集中期
阿勒泰地區%集中度%集中期
아륵태지구%집중도%집중기
precipitation concentration degree(PCD)%precipitation concentration period(PCP)%Altay
利用1961~2010年阿勒泰地区冬季台站降水资料,计算并分析了阿勒泰地区降雪集中度和集中期的时空变化特征。结果表明:降雪集中度(PCD)和集中期(PCP)能够定量表征降雪量在时空场上的非均一性。阿勒泰地区降雪平均集中度为0.27,平均集中期为第7.8候(12月上旬)。平均集中度和集中期空间分布不均匀,东部的降雪集中度和集中期较西部大。Morlet小波分析表明,阿勒泰地区降雪集中度和集中期存在各自的年际尺度周期变化。通过降雪量与集中度和集中期的合成分析表明,多雪年集中度较少雪年偏小,集中期较少雪年偏早。
利用1961~2010年阿勒泰地區鼕季檯站降水資料,計算併分析瞭阿勒泰地區降雪集中度和集中期的時空變化特徵。結果錶明:降雪集中度(PCD)和集中期(PCP)能夠定量錶徵降雪量在時空場上的非均一性。阿勒泰地區降雪平均集中度為0.27,平均集中期為第7.8候(12月上旬)。平均集中度和集中期空間分佈不均勻,東部的降雪集中度和集中期較西部大。Morlet小波分析錶明,阿勒泰地區降雪集中度和集中期存在各自的年際呎度週期變化。通過降雪量與集中度和集中期的閤成分析錶明,多雪年集中度較少雪年偏小,集中期較少雪年偏早。
이용1961~2010년아륵태지구동계태참강수자료,계산병분석료아륵태지구강설집중도화집중기적시공변화특정。결과표명:강설집중도(PCD)화집중기(PCP)능구정량표정강설량재시공장상적비균일성。아륵태지구강설평균집중도위0.27,평균집중기위제7.8후(12월상순)。평균집중도화집중기공간분포불균균,동부적강설집중도화집중기교서부대。Morlet소파분석표명,아륵태지구강설집중도화집중기존재각자적년제척도주기변화。통과강설량여집중도화집중기적합성분석표명,다설년집중도교소설년편소,집중기교소설년편조。
Based on observed winter precipitation data in Altay region from 1961 to 2010,the temporal and spatial variations of precipi-tation concentration degree (PCD)and precipitation concentration period (PCP)were caculated and analyzed.The results show that the snow PCD and PCP could characterize quantitatively the heterogeneity of snowfall in space and temporal field.The averaged PCD in Altay region was 0.27,and the averaged PCP was the 7.8 pentad (in early December).The averaged PCD and PCP distributed une-venly,and they were higher in east than that in west region.The periods of PCD and PCP in Altay region were given out by Morlet wavelet transformation,which showed there was a significant periodic change of PCD and PCP at inter-annual scale.The PCD in snowy years was less than that in less snowfall years,and the PCP in snowy years was earlier than that in less snowfall years.