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      氣候變化研究進展 ?? 2008, Vol. 4 ?? Issue (003): 167-172.

      ? 研究短論 ? 上一篇    下一篇

      21世紀黃河流域上中游地區(qū)氣候變化趨勢分析

      劉綠柳 劉兆飛 徐宗學   

      1. 中國氣象局國家氣候中心; 北京師范大學
      • 收稿日期:2007-11-20 修回日期:2008-01-16 出版日期:2008-05-31 發(fā)布日期:2008-05-31
      • 通訊作者: 劉綠柳 劉兆飛

      Trends of Climate Change for the Upper-Middle Reaches of the Yellow River in the 21st Century

      Liu Luliu, LIU Zhaofei   

      1. National Climate Center, China Meteorological Administration; College of Water Sciences, Beijing Normal University
      • Received:2007-11-20 Revised:2008-01-16 Online:2008-05-31 Published:2008-05-31
      • Contact: Liu Luliu, LIU Zhaofei

      摘要: 氣候變化預估常用的全球氣候模式(GCM)難以提供區(qū)域或更小尺度上可靠的逐日氣候要素序列,針對這一問題,應用統(tǒng)計降尺度模型(statistical downscaling model,SDSM)將HadCM3的模擬數(shù)據(jù)(包括A2、B2兩種情景)處理為具有較高可信度的逐日站點序列。以1961-1990年為基準期,分析了21世紀黃河流域上中游地區(qū)未來最高氣溫、最低氣溫與年降水量的變化。在A2、B2兩種氣候變化情景下,日最高氣溫、日最低氣溫均呈升高趨勢;但A2的變化較顯著,日最高氣溫的升高趨勢在景泰站最明顯,日最低氣溫的升高趨勢在河曲站最顯著。流域平均的年降水量變化范圍為-18.2%~13.3%。A2情景下降水量增加和減少的面積基本相等,寶雞站降水量增加最多;B2情景下大部分區(qū)域降水減少,西峰鎮(zhèn)降水量減少最顯著。

      關鍵詞: 黃河流域, 統(tǒng)計降尺度, 最高氣溫, 最低氣溫

      Abstract: Considering the lack of spatial and temporal accuracy, poor reliability of global climate models (GCM) at regional or local scale, a statistical downscaling model (SDSM) is used to generate daily weather data. With SDSM, the daily series of HadCM3 outputs under the A2 and B2 scenarios were downscaled to the stations. The future trends of annual precipitation, daily maximum (TMAX) and mininum temperatures (TMIN) in the upper-middle reaches of the Yellow River were analyzed on the basis of the reference period of 1961-1990. Daily TMAX and TMIN both show increasing trends under the A2 and B2 scenarios, but the increment is more distinct under the A2 scenario. The increasing trends of TMAX at Jingtai station and TMIN at Hequ station are the most remarkable. The increment in annual precipitation in the basin ranges from -18.2% to 13.3%. Under the A2 scenario, the areas with an increasing trend and a decreasing trend are almost equal, and the largest increment occurs at Baoji station. Under the B2 scenario, the annual precipitation shows a decreasing trend in most parts of the basin, and the largest reduction appears at Xifengzhen station.

      Key words: the Yellow River basin, statistical downscaling, maximum temperature, minimum temperature, precipitation

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