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Uncertainty in climate change impacts on streamflow in Be River Catchment, Vietnam

机译:气候变化的不确定性影响越南比河集水区的水流

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摘要

This paper focuses on the uncertainty in climate change impacts on streamflow in Be River Catchment. Uncertainty associated with GCM structure from a subset of CMIP3 (CCCMA CGCM3.1, CSIRO Mk30, IPSL CM4, MPI ECHAM5, NCAR CCSM3.0, UKMO HadGEMI, and UKMO HadCM3), SRES emission scenarios (A1B, A2, B1, and B2), and prescribed increases in global mean temperature (0.5℃ to 6℃) using SWAT model is investigated. For prescribed warming scenarios using HadCM3, linear decreases in mean annual streamflow range from 3.1 to 16.7%. Differences in projected annual streamflow between SRES emission scenarios using HadCM3 are small (-5.6% to -4.6%). Under the A1B scenario and 2℃ increase in global mean temperature using seven GCMs, there is substantial disparity, by -2.9-25.5% and -8.3-19.1 %, respectively. It is generally reasonable to conclude that GCM structure-related uncertainty is greater than that associated with the emission scenarios and climate sensitivity.
机译:本文着眼于气候变化的不确定性对Be河集水区的水流量的影响。来自CMIP3(CCCMA CGCM3.1,CSIRO Mk30,IPSL CM4,MPI ECHAM5,NCAR CCSM3.0,UKMO HadGEMI和UKMO HadCM3)子集的GCM结构的不确定性,SRES排放情景(A1B,A2,B1和B2) ),并使用SWAT模型研究了规定的全球平均温度(0.5℃至6℃)的升高。对于使用HadCM3的指定变暖方案,年平均流量的线性下降范围从3.1到16.7%。使用HadCM3的SRES排放情景之间的预计年流量差异很小(-5.6%至-4.6%)。在A1B情景和使用7个GCM的全球平均温度升高2℃的情况下,存在显着差异,分别为-2.9-25.5%和-8.3-19.1%。通常合理的结论是,与GCM结构有关的不确定性大于与排放情景和气候敏感性相关的不确定性。

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