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陇东黄土高原下垫面不均匀性指标的建立及其对大孔径闪烁仪(LAS)观测感热通量的影响
引用本文:郝小翠, 张强, 杨泽粟. 陇东黄土高原下垫面不均匀性指标的建立及其对大孔径闪烁仪(LAS)观测感热通量的影响[J]. 地球物理学报, 2016, 59(3): 816-827, doi: 10.6038/cjg20160305
作者姓名:郝小翠  张强  杨泽粟
作者单位:1. 西北区域气候中心, 兰州 730020; 2. 中国气象局兰州干旱气象研究所, 甘肃省干旱气候变化与减灾重点实验室, 中国气象局干旱气候变化与减灾重点实验室, 兰州 730020; 3. 兰州大学大气科学学院, 兰州 730000
基金项目:干旱气象科学研究基金项目(IAM201413)和国家重点基础研究发展计划(973计划)项目(2013CB430206)联合资助.
摘    要:目前定量研究下垫面不均匀性对大孔径闪烁仪(LAS)、涡动相关仪(ECS)观测感热通量差异的影响还比较少.本文利用黄土高原庆阳观测站2012年6、7月典型晴天两主风向范围E-SE和SW-W的陆面过程数据,在建立了下垫面不均匀性定量化指标的基础上,分析了下垫面不均匀性与地表温度变率的关系及其对LAS、ECS观测感热通量差异的影响.结果表明:庆阳站下垫面不均匀性大小η和地表温度变率г具有很好的相关性,相关系数达到0.566以上,证明了新建立指标的合理性.下垫面不均匀性大小η和LAS、ECS观测的感热通量差异HLAS-HECS具有很好的一致性,相关系数达到0.634.下垫面不均匀性对LAS和ECS的感热通量差异影响显著,下垫面越不均匀LAS和ECS测量的感热通量差异越大.对两主风向分别进行分析,在E-SE风向范围η和HLAS-HECS的相关系数为0.430,HLAS和HEC拟合的线性趋势系数为1.279,在SW-W风向范围η和HLAS-HECS的相关系数为0.680,HLAS和HEC拟合的线性趋势系数为1.297.下垫面不均匀性的影响程度越大,LAS和ECS观测的感热通量差异越大.

关 键 词:大孔径闪烁仪(LAS)   涡动相关仪(ECS)   下垫面不均匀性   地表温度变率   感热通量差异
收稿时间:2015-09-27
修稿时间:2015-12-31

A new index for land surface inhomogeneity and its impact on sensible heat flux measured by Large Aperture Scintillometer(LAS) over eastern Gansu of Loess Plateau
HAO Xiao-Cui, ZHANG Qiang, YANG Ze-Su. A new index for land surface inhomogeneity and its impact on sensible heat flux measured by Large Aperture Scintillometer(LAS) over eastern Gansu of Loess Plateau[J]. Chinese Journal of Geophysics (in Chinese), 2016, 59(3): 816-827, doi: 10.6038/cjg20160305
Authors:HAO Xiao-Cui  ZHANG Qiang  YANG Ze-Su
Affiliation:1. Northwest Regional Climate Center, Lanzhou 730020, China; 2. Institute of Arid Meteorology, CMA; 3. Key Laboratory of Arid Climatic Change and Reducing Disaster of Gansu Province
Abstract:There are few quantitative researches focused on the influence of inhomogeneous land surface condition on sensible heat fluxes measured by Large Aperture Scintillometer(LAS) and Eddy Covariance System(ECS) at present. In this paper, based on the observed land surface process data in two prevailing wind directions(E-SE and SW-W) at Qingyang site in the Loess Plateau during June and July 2012, firstly, a quantitative index representing the degree of land surface inhomogeneity was established, and then an analysis was made of the relationship between surface inhomogeneity and surface temperature variability and its influence on the difference between LAS and ECS measured sensible heat fluxes. Results showed that the land surface inhomogeneity η had a good correlation with surface temperature variability г with a correlation coefficient up to 0.566, indicating that η can well represent land surface inhomogeneity. η also had a good consistency with the difference between LAS and ECS measured sensible heat fluxes(HLAS-HECS), its correlation coefficient being up to 0.634. η significantly influenced the difference between LAS and ECS measured sensible heat fluxes. The more inhomogeneous η was, the greater HLAS-HECS was. For the two prevailing wind directions, η had a correlation coefficient of 0.430 with HLAS-HECS in E-SE wind direction, the fitting coefficient being 1.279; η had a correlation coefficient of 0.680 with HLAS-HECS in SW-W wind direction, the fitting coefficient being 1.297. LAS and ECS measured sensible heat fluxes will have a greater difference when the influence of land surface inhomogeneity is larger.
Keywords:Large Aperture Scintillometer(LAS)  Eddy Covariance System(ECS)  Land surface inhomogeneity  Surface temperature variability  Difference of sensible heat flux
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