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      氣候變化研究進(jìn)展 ?? 2010, Vol. 6 ?? Issue (04): 277-283.

      ? 氣候系統(tǒng)變化 ? 上一篇    下一篇

      1956-2007年河南省降水和水資源變化及評(píng)估

      顧萬龍,王記芳,竹磊磊   

      1. 河南省氣候中心
      • 收稿日期:2009-09-04 修回日期:2009-12-22 出版日期:2010-07-30 發(fā)布日期:2010-07-30
      • 通訊作者: 竹磊磊

      Changes in Precipitation and Water Resources in Henan Province in 1956-2007

      • Received:2009-09-04 Revised:2009-12-22 Online:2010-07-30 Published:2010-07-30

      摘要: 利用河南省103個(gè)氣象站的降水量和各省轄市的水資源資料,分析了河南省1956-2007年降水和水資源變化特點(diǎn),對(duì)降水資源量和水資源量進(jìn)行了豐枯評(píng)估;分別采用線性相關(guān)法和產(chǎn)水系數(shù)法以降水量估算水資源量,并對(duì)估算效果進(jìn)行了對(duì)比分析。結(jié)果表明:1) 52年來河南省年降水資源量呈不明顯的減少趨勢(shì),減少速率為2.32億m3/10a;省內(nèi)不同區(qū)域降水資源量的變化趨勢(shì)不太一致,豫北、豫西和豫中為減少趨勢(shì),豫東、豫西南和豫南呈不同程度的增加趨勢(shì)。2) 52年來全省水資源總量呈減少趨勢(shì),減少速率為10.85億m3/10a,大于降水資源量的減少速率,省內(nèi)各區(qū)域水資源量均呈弱減少趨勢(shì),減少速率為豫西最大,豫北次之,豫中最少;全省水資源總量的年代際變化特點(diǎn)與降水資源量基本一致。3) 水資源總量與降水量關(guān)系密切,用年降水量估算水資源總量,平均相對(duì)誤差為10%~22%;將線性相關(guān)法和產(chǎn)水系數(shù)法兩種估算模式分別用于不同豐枯程度年景的估算,可減小估算誤差。

      關(guān)鍵詞: 河南, 降水, 水資源, 估算

      Abstract: Based on the precipitation data of 103 meteorological stations and the water resource data of 18 provincial cities in Henan Province, the spatial distribution and change characteristics of precipitation and water resources in the whole province in 1956-2007 were analyzed, and the wet/dry years of precipitation and water resources were also assessed. The water resources were estimated from the precipitation data by using the linear correlation method and the water-producing coefficient method, respectively; and their precisions were compared and analyzed. The results indicate that: 1) the annual precipitation resource for the whole province showed an overally slowly decreasing trend with the rate of 2.32×108 m3/10a in recent 50 years; however, the precipitation resource is not spatially uniform, and it exhibited decreasing trends in north, west and central Henan Province, but increasing trends in the rest sub-regions of the province. 2) The total water resource for the whole province showed a decreasing trend with the rate of 10.85×108 m3/10a, which is larger than the decreasing rate of precipitation; it showed a slight decreasing trend in all sub-regions of the province, the reduction is the most obvious in west Henan, next in north Henan, and least in central Henan. The decadal change characteristics of water resource are basically similar to those of precipitation resource. 3) There appears a good relationship between total water resource and annual precipitation, and the mean error of the annual total water resource estimated from annual precipitation is about 10%-22%. The estimation error might be diminished if the water-producing coefficient method is used to anomalous high/low water flow years, the linear correlation method for other years, respectively.

      Key words: Henan Province, precipitation, water resources, estimation, evaluation

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