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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Analysis of the land surface heterogeneity and its impact on atmospheric variables and the aerodynamic and thermodynamic roughness lengths
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Analysis of the land surface heterogeneity and its impact on atmospheric variables and the aerodynamic and thermodynamic roughness lengths

机译:地表异质性及其分析对大气变量和影响空气动力学和热力学粗糙度长度

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The land surface heterogeneity has a very significant impact on atmospheric variables (air temperature T a, wind speed u, and humidity q), the aerodynamic roughness length z 0m, thermodynamic roughness length z 0h, and the excess resistance to heat transfer kB ?1. First, in this study the land surface heterogeneity has been documented through the comparison of surface reflectance r 0, surface temperature T 0, net radiation flux R n, and sensible heat flux H partitioning over the different land cover types in the experimental areas of the Global Energy and Water Cycle Experiment (GEWEX) Asian Monsoon Experiment on the Tibetan Plateau (GAME/Tibet), the Coordinated Enhanced Observing Period (CEOP) Asia-Australia Monsoon Project on the Tibetan Plateau (CAMP/Tibet), the Heihe Basin Field Experiment (HEIFE), the Arid Environment Comprehensive Monitoring Plan, 95 (AECMP'95), and the Dun Huang Experiment (DHEX). The results show that the surface heterogeneity was very significant in the areas of the HEIFE, the AECMP'95, and the DHEX and that it was less significant in the areas of CAMP/Tibet and GAME/Tibet. Second, the vertical profiles of T a, u, and q in the near-surface layer and above the blending height z b have been analyzed using the atmospheric boundary layer (ABL) tower data, radiosonde data, and tethered balloon data observed during the HEIFE, the DHEX, and the CAMP/Tibet. The results show that the land surface heterogeneity leads in the near-surface layer to different vertical profiles of u, T a, and q overlying the surfaces of the Gobi and the oasis in the areas of the HEIFE and DHEX. The values of u, T a, and q become well mixed above a height of about 300 m at the HEIFE and 150 m at the DHEX. z 0m, z 0h, and kB ?1 over the different land surfaces have also been determined in this study. The results show that the land surface heterogeneity leads to different aerodynamic and thermodynamic parameters over the areas of the HEIFE, the AECMP'95, and the GAME/Tibet.
机译:地表异质性有非常对大气变量(空气产生巨大的影响温度T, u风速和湿度问),空气动力学粗糙度长度z 0 m,热力学粗糙长度z 0 h,多余的传热阻力kB ? 1。在这项研究中地表异质性通过比较表面记载反射率r 0,表面温度T 0,净辐射通量R n,显热通量H在不同的土地覆盖类型分区在实验领域的全球能源和水循环试验(GEWEX)亚洲季风实验在青藏高原(游戏/西藏),协调增强观察期间(CEOP)在西藏Asia-Australia季风项目西藏高原(营),黑河流域实验(HEIFE),干旱的环境全面的监控计划,95),95 (AECMP”商补实验(DHEX)。表面非均质性非常领域的重要HEIFE,AECMP 95年,和DHEX少/西藏和重要领域的营地游戏/西藏。u,近地表层及以上的问分析了z b使用混合高度大气边界层(ABL)塔数据,无线电探空仪的数据,和系留气球,数据观察HEIFE期间,DHEX,营/西藏。在近地表表面的异质性导致层不同的垂直的u, T,和q戈壁和上覆的表面领域的绿洲HEIFE DHEX。u值,T, q成为混合之上HEIFE高度约300米,150米DHEX。不同的土地表面也被确定在这项研究中。表面的异质性导致不同空气动力学和热力学参数HEIFE, AECMP的95年,看看西藏/游戏的游戏玩家们。

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