西北地区干、湿夏季的前期环流和水汽差异
DIFFERENCES IN CIRCULATION AND MOISTURE BETWEEN DRY AND WET YEARS IN NORTHWEST CHINA
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摘要: 用西北地区夏季 (6、7、8月) 共19个站降水量观测资料以及NCEP/ NCAR 1958~1997年再分析全球月平均网格点前期 (春季) 资料, 选取西北地区周边范围内夏季干、湿年的前期春季各个物理量场进行相关统计分析, 结果表明前期春季影响西北地区夏季干、湿的相关区域环流特征和水汽特征有显著差异。Abstract: In the context of summer rainfall observations of 19 stations in Northwest China and NCEP/NCAR global monthly mean reanalyzed grid data in spring from 1958 to 1997, correlative statistical analysis are performed on the related parameters in spring in the years of being dry or wet in summer in Northwest China and its nearby regions. Results show that in spring the circulation and moisture features of dry years in the related areas are significantly different from those of wet years.
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图 4 (a)、(b) 分别为西北夏季降水和前期春季500 hPa U、V风场的相关, (c)、(d) 分别为湿润、干旱夏季年的前期春季500 hPa风矢场的距平场 (单位:m/ s, 相关图中阴影说明同图 3)
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[1] 叶笃正, 高由禧, 青藏高原气象学.北京:科学出版社, 1979.278. [2] 白肇烨, 徐国昌.中国西北天气.北京:气象出版社, 1991. [3] 吴统文, 钱正安.夏季西北干旱区干、湿环流和高原动力影响差异的对比分析.高原气象, 1996, 15(4):387-396. http://www.cnki.com.cn/Article/CJFDTOTAL-GYQX604.000.htm [4] 吴统文, 钱正安.青藏高原北侧地区干湿年夏季环流差异的对比分析及高原的热力影响.气象学报, 1996, 54(5):558-568. http://www.cnki.com.cn/Article/CJFDTOTAL-QXXB605.004.htm [5] 吴统文, 钱正安, 吕世华.西北干旱气候形成的数值模拟研究--青藏高原隆升和初始环流场等的影响.大气科学, 1998, 22(5):753-762. http://www.cnki.com.cn/Article/CJFDTOTAL-DQXK805.009.htm [6] Broccoli A J S, Manabe S. The effecs of the orography on middle latatitude northern hemisphere dry climate. J Climate, 1992, 5(11):1181-1201. doi: 10.1175/1520-0442(1992)005<1181:TEOOOM>2.0.CO;2 [7] Yang S, Xu L. Linkage between Eurasian winter snow cover and Chinese summer rainfall: different from the snow-Indian monsoon circulation. Int J Climatol, 1994, (14): 739-750. [8] 中国气象局气象科学研究院主编.中国近百年旱涝分布图集.北京:地图出版社, 1981.