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      氣候變化研究進(jìn)展 ?? 2010, Vol. 6 ?? Issue (06): 391-397.

      ? 氣候系統(tǒng)變化 ?    下一篇

      2050年前南水北調(diào)中線工程水源區(qū)地表徑流的變化趨勢(shì)

      張利平1,胡志芳2,秦琳琳3,曾思棟3   

      1. 1. 武漢大學(xué)水利水電學(xué)院
        2. 中國(guó)科學(xué)院地理科學(xué)與資源研究所
        3. 武漢大學(xué)水資源與水電工程科學(xué)國(guó)家重點(diǎn)實(shí)驗(yàn)室
      • 收稿日期:2009-12-29 修回日期:2010-03-04 出版日期:2010-11-30 發(fā)布日期:2010-12-10
      • 通訊作者: 張利平 E-mail:zlpwhu@sina.com
      • 基金資助:
        自然科學(xué)基金

      Surface Runoff Changes in the Water Source Area for the Middle Route Project of South-to-North Water Transfer Before 2050

      • Received:2009-12-29 Revised:2010-03-04 Online:2010-11-30 Published:2010-12-10

      摘要: 以南水北調(diào)中線工程水源區(qū)為研究流域,采用線性回歸法、Mann-Kendall非參數(shù)檢驗(yàn)等方法,分析了1961—2000年的水文氣象要素變化特征;基于數(shù)字高程模型、土地利用和土壤類型等資料,研究了SWAT模型在研究流域的適用性;根據(jù)IPCC第四次評(píng)估報(bào)告多模式結(jié)果,分析了IPCC SRES A2和A1B情景下2011—2050年的降水、氣溫、徑流的響應(yīng)過程。結(jié)果表明:1961—2000年南水北調(diào)中線工程水源區(qū)降水量無(wú)顯著變化趨勢(shì),氣溫呈緩慢上升趨勢(shì),徑流量呈緩慢減少趨勢(shì)。與基準(zhǔn)期(1961—1990年)相比,未來(lái)40年A2和A1B兩種氣候情景下水源區(qū)降水量、氣溫和徑流量都呈現(xiàn)出增加趨勢(shì),A2情景下增加趨勢(shì)明顯,但徑流量增幅小于降水量的增幅,這可能與蒸發(fā)量的增加有關(guān)。未來(lái)氣候變化對(duì)南水北調(diào)中線工程水源區(qū)徑流變化影響不大,總體有利于南水北調(diào)中線工程的調(diào)水。

      關(guān)鍵詞: 氣候變化, SWAT模型, 地表徑流, 南水北調(diào)中線工程, 水源區(qū), Climate change, SWAT model, surface runoff, Middle Route Project of South-to-North Water Transfer, water source area

      Abstract: Linear regression and Mann-Kendall non-parametric test were first used to analyze the change characteristics of the hydrological and meteorological elements in the water source area (catchment) of the Middle Route Project of South-to-North Water Transfer; then a distributed hydrological SWAT model was developed based on a digital elevation model and the land use and soil type information, and its applicability in the catchment was also verified. Finally, the precipitation, temperature and runoff response processes were analyzed based on the IPCC Fourth Assessment Report multi-mode ensembles under different greenhouse gas emission scenarios (SRES A2 and A1B) in 2011-2050. The analysis results show that precipitation in the catchment had no trend, temperature rose slowly, and surface runoff decreased slowly during 1961-2000. Compared with the baseline period, precipitation, temperature and runoff in the catchment in future 40 years will all increase under the A2 and A1B scenarios, especially under the A2 scenario, but the increment amplitude of runoff will be less than that of precipitation, this may be associated with the increase in evaporation. Future climate change will have a little influence on the runoff of the water source area, and thus will generally be favorable to the South to North Water Transfer Project.

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