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土壤质地对中国区域陆面过程模拟的影响

吴龙刚 王爱慧 盛炎平

吴龙刚, 王爱慧, 盛炎平. 土壤质地对中国区域陆面过程模拟的影响[J]. 气候与环境研究, 2014, 19(5): 559-571. doi: 10.3878/j.issn.1006-9585.2013.13055
引用本文: 吴龙刚, 王爱慧, 盛炎平. 土壤质地对中国区域陆面过程模拟的影响[J]. 气候与环境研究, 2014, 19(5): 559-571. doi: 10.3878/j.issn.1006-9585.2013.13055
WU Longgang, WANG Aihui, SHENG Yanping. Impact of Soil Texture on the Simulation of Land Surface Processes in China[J]. Climatic and Environmental Research, 2014, 19(5): 559-571. doi: 10.3878/j.issn.1006-9585.2013.13055
Citation: WU Longgang, WANG Aihui, SHENG Yanping. Impact of Soil Texture on the Simulation of Land Surface Processes in China[J]. Climatic and Environmental Research, 2014, 19(5): 559-571. doi: 10.3878/j.issn.1006-9585.2013.13055

土壤质地对中国区域陆面过程模拟的影响

doi: 10.3878/j.issn.1006-9585.2013.13055
基金项目: 国家重点基础研究发展计划项目2010CB428403,国家自然科学基金项目41275110,北京市自然科学基金1122015,教育教学-人才培养模式创新试验-应用型人才培养模式试点改革pxm2013_014224_000076

Impact of Soil Texture on the Simulation of Land Surface Processes in China

  • 摘要: 利用陆面过程模式(CLM3.5)和中国区域两种土壤质地数据(分别来自第二次中国土壤调查SNSS和联合国粮食农业组织FAO),研究了土壤质地变化对于模式模拟的陆表水热变量的影响。结果显示,土壤质地对土壤水文学变量的影响远大于对土壤热力学变量的影响,尤其是对于饱和土壤含水量和饱和水力传导率的影响。对于模式的输出,土壤质地影响比较明显的有土壤湿度、总径流和土壤渗透等水文学变量以及地表潜热、地表感热和土壤热通量等热力学变量,而影响相对较小的有地面吸收的太阳辐射和地表反照率。同时,发现基于SNSS模拟的土壤湿度与站点观测值更加接近。因此,本研究认为基于SNSS土壤质地数据可以有效地改进模式模拟结果,建议以后在陆面模式试验中尽可能使用以观测为基础的SNSS土壤质地数据。
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  • 收稿日期:  2013-03-29
  • 修回日期:  2013-06-25

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