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Evaluation of soil moisture in CMIP5 simulations over the contiguous United States using in situ and satellite observations

机译:使用原位和卫星观测,在连续的美国模拟中的土壤水分评价

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This study provides a comprehensive evaluation of soil moisture simulations in the Coupled Model Intercomparison Project Phase 5 (CMIP5) extended historical experiment (2003 to 2012). Soil moisture from in situ and satellite sources is used to evaluate CMIP5 simulations in the contiguous United States (CONUS). Both near-surface (0-10 cm) and soil column (0-100 cm) simulations from more than 14 CMIP5 models are evaluated during the warm season (April-September). Multimodel ensemble means and the performance of individual models are assessed at a monthly timescale. Our results indicate that CMIP5 models can reproduce the seasonal variability in soil moisture over CONUS. However, the models tend to overestimate the amount of both near-surface and soil column soil moisture in the western US and underestimate it in the eastern US. There are large variations across models, especially for the near-surface soil moisture. There are significant regional variations in performance as well. Results of a regional analysis show that in the deeper soil layers, the CMIP5 soil moisture simulations tend to be most skillful in the southern US. Based on both the satellite-derived and in situ soil moisture, CESM1, CCSM4 and GFDL-ESM2M perform best in the 0-10 cm soil layer and CESM1, CCSM4, GFDL-ESM2M and HadGEM2-ES perform best in the 0-100 cm soil layer.
机译:本研究规定了耦合模型互联项目第5(CMIP5)延长历史实验(2003年至2012)的土壤水分模拟综合评估。原位和卫星源的土壤水分用于评估连续的美国(康明斯)中的CMIP5模拟。在温暖的季节(4月至9月)期间,评估了来自14多种CMIP5型号的近表面(0-10cm)和土壤柱(0-100cm)模拟。 MultiModel集合手段和各个模型的性能按月计时评估。我们的结果表明,CMIP5型号可以在康复膜中重现土壤水分的季节变异性。然而,该模型往往估计美国西部近地和土壤柱土壤水分的量,并低估了美国东部。模型有很大的变化,特别是对于近表面土壤水分。表现也有重大的区域变化。区域分析结果表明,在较深的土层中,CMIP5土壤水分模拟往往是南方南方最熟练的。基于卫星衍生的和原位土壤水分,CESM1,CCSM4和GFDL-ESM2M在0-10cm土层和CESM1,CCSM4,GFDL-ESM2M和HADGEM2-ES中表现最佳,在0-100厘米中表现最佳土壤层。

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