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NCEP/NCAR再分析温度·位势高度和风速场资料在上对流层/下平流层的适用性评估(英文) 被引量:2

Applicability Evaluation of NCEP/NCAR Reanalysis Temperature,Geopotential Height and Wind Field Data in the Upper Troposphere and Lower Stratosphere
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摘要 利用全球169个探空站资料检验NCEP/NCAR再分析资料,分析全球(主要是陆地地区)上对流层互下平流层位势高度、温度以及风速场标准误差的分布特征。结果表明,再分析风速场资料标准误差分布主要受急流区的影响,在急流区与实际风场存在明显的差异;并且风速场标准误差的分布具有明显的冬夏季节差异,在海岸线附近平均偏差较大;再分析位势高度、温度场的标准误差高值区主要集中在东半球低纬地区(印度洋沿岸),标准误差分布与其平均偏差分布基本一致,所以标准误差可以由平均偏差很好地解释;再分析温度、位势高度资料内陆地区标准误差偏低,高值区主要沿海岸线分布,风速场平均误差在海岸线附近比较大,这与探空站数据的质量地区差异及陆地观测站密集、海洋观测站较少密切相关。 By using the data in 169 sounding stations over the world,NCEP/NCAR reanalysis data were tested,and the distribution characteristics of standard errors of geopotential height,temperature and wind speed field from the upper troposphere to the lower stratosphere over the world(most were the land zone) were analyzed.The results showed that the standard error distribution of reanalysis wind speed field data was mainly affected by the jet stream zone.There existed the obvious difference between the jet stream zone and the actual wind field.The distribution of standard error in the wind speed field had the obvious seasonal difference in winter,summer,and the average deviation was larger near the coastline.The high value zones of standard errors of reanalysis geopotential height and temperature field mainly concentrated in the low-latitude region in the Eastern Hemisphere(Indian Ocean coast).The distribution of standard error was basically consistent with average error.Therefore,the standard error could be explained well by the average error.The standard errors of reanalysis temperature and geopotential height data in the inland zone were lower.The high value zone mainly distributed along the coastline,and the average error of wind speed field was bigger near the coastline.It closely related to the quality of data in the sounding stations,the regional difference and the fact that the land observation stations were dense,and the ocean observation stations were fewer.
出处 《Meteorological and Environmental Research》 CAS 2010年第7期45-50,53,共7页 气象与环境研究(英文版)
基金 Supported by The National Key Basic Research Development Plan(2010CB428602)
关键词 NCEP/NCAR再分析资料 西风急流 标准误差 NCEP/NCAR reanalysis data Westerly jet stream Standard error China
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  • 1丁一汇,李崇银,何金海,陈隆勋,甘子钧,钱永甫,阎俊岳,王东晓,施平,方文东,许建平,李立.南海季风试验与东亚夏季风[J].气象学报,2004,62(5):561-586. 被引量:114
  • 2曾庆存,李崇银,黄荣辉,吴国雄,张邦林.大气环流季节和低频变化的动力学问题[J].自然科学进展(国家重点实验室通讯),1994,4(5):532-542. 被引量:1
  • 3张东凌,何卷雄,左瑞亭,曾庆存.季风指数及其年际变化II·南海夏季风分量动能强度指数及其年际变化[J].气候与环境研究,2005,10(3):333-341. 被引量:4
  • 4竺可桢.东南季风与中国之雨量[J].地理学报,1934,1(1):1-27.
  • 5涂长望 黄士松.中国夏季风之进退[J].气象学报,1944,18:81-92.
  • 6陶诗言 朱文妹 等.论梅雨的年际变异[J].大气科学,1988,:13-21.
  • 7Pedelaborde P. The Monsoons (Tr. by M. J. Clegg).London: Methuen, 1963. 196 pp.
  • 8Webster P J, Yang S. Monsoon and ENSO: Selectively interactive systems. Quart. J. Roy. Meteor. Soc., 1992,118:877~926.
  • 9Goswami B N, Krishnamurthy V, Annamalai H. A broad scale circulation index for the interannual variability of the Indian summer monsoon. Quart. J. Roy. Meteor. Soc.,1999, 125:611~633.
  • 10Shukla J, Paolino D A. The Southern Oscillation and longrange forecasting of the summer monsoon rainfall over India. Mon. Wea. Rev. , 1983, 111:1830~1837.

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