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中国沙漠 ›› 2002, Vol. 22 ›› Issue (6): 545-552.

• 研究论文 • 上一篇    下一篇

考虑生物结皮影响的陆气湍流模式研究

杜岳1, 姚德良1,2, 李新荣2, 谢正桐1, 张景光2   

  1. 1. 中国科学院 力学研究所, 北京 100080;
    2. 中国科学院 寒区旱区环境与工程研究所沙坡头沙漠试验研究站, 甘肃 兰州 730000
  • 收稿日期:2002-06-20 修回日期:2002-09-08 出版日期:2002-12-20 发布日期:2002-12-20
  • 作者简介:杜岳(1977-),男(汉族),北京市人,硕士生,主要从事环境流体力学研究。
  • 基金资助:
    中国科学院沙坡头沙漠试验研究站基金(200007);国家自然科学基金项目(19832060;40071007)资助

A Turbulent Model of the Land-Atmosphere Interaction with the Crust Layer Influence

DU Yue1, YAO De-liang1,2, LI Xin-rong2, XIE Zheng-tong1, ZHANG Jing-guang2   

  1. 1. Institute of Mechanics, Chinese Academy of Sciences, Beijing 100080, China;
    2. Shapotou Desert Research and Experiment Station, Cold and Arid Regions Environmental and Engineering Research Institute, Chinese Academy of Sciences, Lanzhou 730000, China
  • Received:2002-06-20 Revised:2002-09-08 Online:2002-12-20 Published:2002-12-20

摘要: 在以前工作基础上,针对腾格里沙漠人工植被区陆气水热传输过程,提出了一个多层陆气耦合模式。特别给出了导水率的计算模型和修正后的根系吸水模式,考虑了结皮层对土壤水分入渗的影响以及植被演化的过程。陆面过程耦合模式分别对大气、植被、土壤作多层划分,以助于细致了解沿高度分布的各物理量。同时,利用本模式对中国科学院沙坡头沙漠站人工植被区陆气水热交换过程进行了数值模拟,模拟结果与实测值吻合较好,可为当地合理利用水热资源和沙漠治理提供科学依据。

关键词: 陆气湍流模型, 结皮层, 湍流输运, 数值模拟

Abstract: In the paper, we have elucidated the importance of investigation on land surface-atmosphere interaction for mankind's living environment protection and local economics development as well as its present state. Based on the previous work, a coupling micro meteorological model for SPAC system over wheat field in the Tengger Desert is presented. Especially, the leaf stoma non-saturation condition is considered to calculate the evapotranspiration, and the root absorption model is revised as well. The presence of micro biotic crust changes the soil hydraulic conductivity, alters the temporal and spatial distribution of limited precipitation in sand layer and leads to the degradation of deep-rooted shrubs. The canopy is divided into several layers, aiming at revealing the vertical profiles of mean quantities within it and providing scientific basis for parameterization of terrestrial processes. The model is shown capable of well simulating the micro environment of wheat canopy in good agreement with measured mean temperature, specific humidity and latent heat fluxes et al. And the sensitivity test is carried out as well to analyze canopy's influence.

Key words: land-atmosphere turbulent model, crust layer, turbulent transfer, numerical simulation

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