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西南地区主要水循环过程的数值模拟分析

王丽琼 于坤 左瑞亭 罗霞 彭道睿

王丽琼, 于坤, 左瑞亭, 罗霞, 彭道睿. 西南地区主要水循环过程的数值模拟分析[J]. 气候与环境研究, 2014, 19(5): 614-626. doi: 10.3878/j.issn.1006-9585.2013.13086
引用本文: 王丽琼, 于坤, 左瑞亭, 罗霞, 彭道睿. 西南地区主要水循环过程的数值模拟分析[J]. 气候与环境研究, 2014, 19(5): 614-626. doi: 10.3878/j.issn.1006-9585.2013.13086
WANG Liqiong, YU Kun, ZUO Ruiting, LUO Xia, PENG Daorui. Numerical Simulation Analysis on the Primary Water Cycle Process in Southwest China[J]. Climatic and Environmental Research, 2014, 19(5): 614-626. doi: 10.3878/j.issn.1006-9585.2013.13086
Citation: WANG Liqiong, YU Kun, ZUO Ruiting, LUO Xia, PENG Daorui. Numerical Simulation Analysis on the Primary Water Cycle Process in Southwest China[J]. Climatic and Environmental Research, 2014, 19(5): 614-626. doi: 10.3878/j.issn.1006-9585.2013.13086

西南地区主要水循环过程的数值模拟分析

doi: 10.3878/j.issn.1006-9585.2013.13086
基金项目: 国家重点基础研究发展计划项目2013CB956203

Numerical Simulation Analysis on the Primary Water Cycle Process in Southwest China

  • 摘要: 利用NCAR的公用陆面模式CLM4.0(Community Land Model 4.0),以1961~2010年普林斯顿大学的大气驱动场资料作为大气强迫场,对西南地区陆面过程变化进行了非耦合模拟试验。分析结果表明:西南地区降水呈现明显的干湿季节特征,季风期降水量分布为东北—西南走向,以印度缅甸一带向东北方向递减;非季风期近似呈东西梯度,以两湖地区为中心向西递减。全年而言,西南地区约有16.7%的降水首先被冠层截留,到达地面后约有60.5%以渗透的形式进入土壤,另有约17.1%形成地表径流,还有少部分降水以直接蒸发的形式加湿低层大气。各水循环因子分布与降水分布密切相关,其中冠层截留、地表径流、冠层蒸发的季风期与非季风期特征差异不大,而地下排水和地表蒸发在非季风期均明显高于非季风期,渗透过程则相反。非季风期西南地区水循环的蒸发高、渗透小、地下排水量显著,这三个过程的共同作用,造成西南地区冬春季陆面水份显著流失,是引发西南春旱的可能原因之一。
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  • 收稿日期:  2013-05-15
  • 修回日期:  2013-11-11

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