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Streamflow in the upper Mississippi river basin as simulated by SWAT driven by 20th Century contemporary results of global climate models and NARCCAP regional climate models

机译:由SWAT模拟的密西西比河上游流域,由20世纪全球气候模型和NARCCAP区域气候模型的当代结果驱动

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摘要

We use Soil and Water Assessment Tool (SWAT) when driven by observations and results of climate models to evaluate hydrological quantities, including streamflow, in the Upper Mississippi River Basin (UMRB) for 1981–2003 in comparison to observed streamflow. Daily meteorological conditions used as input to SWAT are taken from (1) observations at weather stations in the basin, (2) daily meteorological conditions simulated by a collection of regional climate models (RCMs) driven by reanalysis boundary conditions, and (3) daily meteorological conditions simulated by a collection of global climate models (GCMs). Regional models used are those whose data are archived by the North American Regional Climate Change Assessment Program (NARCCAP). Results show that regional models correctly simulate the seasonal cycle of precipitation, temperature, and streamflow within the basin. Regional models also capture interannual extremes represented by the flood of 1993 and the dry conditions of 2000. The ensemble means of both the GCM-driven and RCMdriven simulations by SWAT capture both the timing and amplitude of the seasonal cycle of streamflow with neither demonstrating significant superiority at the basin level.
机译:在观测和气候模型结果驱动下,我们使用土壤和水评估工具(SWAT)来评估1981-2003年密西西比河上游流域(UMRB)的水文量,包括水流,与观察到的水流相比。用作SWAT输入的每日气象条件来自(1)流域气象站的观测结果;(2)由再分析边界条件驱动的区域气候模型(RCM)集合模拟的每日气象条件;以及(3)每日一系列全球气候模型(GCM)模拟的气象条件。使用的区域模型是那些其数据由北美区域气候变化评估计划(NARCCAP)存档的模型。结果表明,区域模型可以正确模拟流域内降水,温度和水流的季节性周期。区域模型还捕获了1993年洪水和2000年干旱情况所代表的年际极端情况。SWAT的GCM驱动和RCM驱动模拟的整体方法既捕获了河流流量的季节性周期的时间和振幅,也没有显示出明显的优势。在流域层面。

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