以唐山11个观测站数据资料为基础,采用气候统计方法,分析了不同区县平均年降水量的变化特征。并从年、季、月等不同时间尺度分析了各区县近50年降水平均相对变率。结果显示:近30年平均年降水量较历年平均年降水量减少8.5%~22.4%,其中沿海地区减少最多,主要作物生长季降水量减少幅度没有超过10%。在年份尺度上,降水变率为20.1%~33.0%之间,降水相对变率从东部沿海向西北逐渐减少;在季节尺度上,春、夏、秋、冬季节降水变率范围分别为57%~68%、38%~48%、24%~31%、37%~42%,春季为降水变率最大的季节;在月份尺度上,1月、12月降水变率最大,超过100%,5~9月是降水变率最少的月份,范围为40%~60%,其中7~8月均在40%左右,其余月份为60%~90%。
Abstract
Using climatic statistical methods, based on the data of 11 observation stations in Tangshan, the change characteristic of annual precipitation of different districts was analyzed. And from different angle of year, quarter and month, the rate of average relative precipitation of different districts was analyzed nearly 50 years. The results showed that: Over the past 30 years, the average annual precipitation reduces 8.5%~22.4% than the average annual rainfall. The reduction of coastal areas is most, but reduced extent of precipitation in the main crop growing season did not exceed 10%. At the year angle, the change rate of precipitation is 20.1%~3.0%, and the relative change rate of precipitation is gradually decreasing from the eastern coastal areas to the northwest. At the quarter angle, the change rate of precipitation of spring, summer, autumn and winter is 57%~8%、38%~8%、24%~1%、37%~2% respectively, the change rate of precipitation of spring is most. At the month angle, the change rate of precipitation in January and December is most, more than 100%. The change rate of precipitation May to September is least, the change range is 40%~60%, the change range of July-August is about 40%, and the other is 60%~90%.
关键词
时间尺度;降水变率;降水量
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Key words
multiple temporal scales;change rate of precipitation;precipitation
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参考文献
[1]Mirza MQ,Warrick RA,Ericksen NJ,etal. Trends and persistence in precipitationin the Ganges,Brahmaputra and Meghnariver basins [J].Hydrology Sciences Journal,1998,43(6):845-858.
[2]Goovaerts P. Geostatisical approaches for in corporation elevation into the spatial interpolation of rainfall[J]. Hydrology Sciences Journal,2000,(228):113-129.
[3]严中伟.华北降水年代际振荡及其与全球温度变化的联系[J].应用气象学报,1999,10(增刊):16-22
[4]丁锋,周顺武.近50年青岛夏季降水变化趋势及其可能原因[J].气象,2005,30(5):3-7.
[5]钟中,胡轶佳,闵锦忠.中国降水年际和年代际变率对空间尺度的敏感性[J].地球物理学报2007,50(5):1330-1336.
[6]薛峰,王会军,何金海.马斯克林高压和澳大利亚高压的年际变化及其对东亚夏季降水的影响[J].科学通报,2003,48(3):287-291.
[7]Ropelewski C F, Halpert M S.Global and regional scale Precipitation on associated with EINino Southern Oscillation. Mon. Wea .Rev.,1987,115:1606-1626.
[8]Webster PJ,Yang S.Monsoon and ENSO:selectively interactive system. Quar. J.Roy. Meteor. Soc.,1992,118:877-926.
[9]JuJ,Slingo J. The Asian summer mosoon and ENSO. Quart. J. Roy .Meteor. Soc.,1995,121:1133-1168.
[10]陆日宇.华北汛期降水量年际变化与赤道东太平洋海温[J].科学通报,2005,50(11):1131-1135.
[11]张天宇,程炳岩,王记芳,等.华北雨季降水集中度和集中期时空变化特征[J].高原气象,2007,26(4):843-853.
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