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      氣候變化研究進(jìn)展 ?? 2008, Vol. 4 ?? Issue (003): 145-150.

      ? 氣候變化與水專(zhuān)欄 ? 上一篇    下一篇

      2050年前長(cháng)江流域地表水資源變化趨勢

      劉波 姜彤 任國玉 Klaus Fraedrich   

      1. 中國科學(xué)院南京地理與湖泊研究所 國家氣候中心 中國氣象局國家氣候中心
      • 收稿日期:2007-08-29 修回日期:2007-12-29 出版日期:2008-05-31 發(fā)布日期:2008-05-31
      • 通訊作者: 劉波

      Projected Surface Water Resource of the Yangtze River Basin Before 2050

      Liu Bo   

      1. Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences National Climate Center National Climate Center
      • Received:2007-08-29 Revised:2007-12-29 Online:2008-05-31 Published:2008-05-31
      • Contact: Liu Bo

      摘要: 利用ECHAM5/MPI-OM氣候模式預估2001-2050年長(cháng)江流域不同排放情景(SRES-A2,A1B,B1)下徑流深的變化,分析了長(cháng)江流域地表水資源量的時(shí)空變化特征。結果表明:3種排放情景下長(cháng)江流域多年平均地表水資源量相差不大,但不同排放情景下年際變化特征較為復雜,且變化趨勢有所不同。其中,A2高排放情景下地表水資源量呈緩慢減小的趨勢,A1B中等排放情景下變化趨勢不明顯,B1低排放情景下呈相對最為顯著(zhù)的增加趨勢。地表水資源量年代際變化波動(dòng)幅度也較大,2001-2030年3種情景下地表水資源量總體呈現下降特征,但從2030年起,則均表現出不同程度的增加,最高增幅達7.47%,其中尤以夏季和冬季增加顯著(zhù)。模式預估長(cháng)江流域未來(lái)水資源量仍保持目前水平,水資源空間分布不均勻特征仍較為突出。

      關(guān)鍵詞: 預估, 氣候變化, 地表水資源, 排放情景

      Abstract: Based on projected runoff depth of ECHAM5/MPI-OM climate model for the Yangtze River basin under different GHG emission scenarios (SRES-A2, A1B, B1) in 2001-2050, the temporal and spatial patterns of future surface water resource in the Yangtze River basin were analyzed. The results show that the long-term average annual surface water resources of the Yangtze River under three scenarios are similar, while interannual fluctuations are complicated with different trends. The surface water resource declines gradually in fluctuation under the A2 scenario, shows no obvious trend under the A1B scenario, and displays a relatively significant increasing trend under the B1 scenario. Decadal variations of the surface water resource are notable, showing an overall decline trend under all the three scenarios in 2001-2030, while an increase trend to varying extent after the 2030s, especially in summer and winter. The projected future water resource in the Yangtze River remains the current level, showing an evident spatially uneven feature.

      Key words: projection, climate change, surface water resource, GHG emission scenario, the Yangtze River basin

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