期刊文献+

陆面网格尺度变换时植被类型处理方法的探讨 被引量:1

Impacts from the Processing of Vegetation Types Within a Model Grid Cell
下载PDF
导出
摘要 针对陆面模式与大气模式耦合,对比分析了模式网格点上多种植被并存和单一植被两种情况下的计算结果,同时给出了网格元上地表有效温度、地表有效感热和潜热通量等的计算方案。试验使用SSiB陆面模式并以HAPEX-MOBILHY资料作为气象强迫场。试验结果表明:如果将网格元上多种植被类型归类成同一种植被类型,模式对有效地表温度、感热和潜热通量等的计算结果与考虑多种植被类型的结果有很大差异。根据实际情况,HAPEX-MOBILHY试验区40%为森林,60%为混合农业区,如果根据一般的植被类型归类法,将该试验区全部看作草地,其积分结果与将该试验区看作40%为落叶针叶林和60%为草地的积分结果也存在一定的差别;虽然有些植被类型在网格元上所占的覆盖面积较小,但它却对网格元上地表通量的计算有较大的贡献。该研究对今后陆面模式耦合工作有一定的指导意义。 Traditionally, when coupling a land surface model into a GCM, the vegetation types within a model grid cell are grouped as one type, by which some discrepancy of model results to the reality are certainly led to. To better understand the impact, the simulated study through offline experiments of two cases in the same grid cell are conducted. Underlying surface in the cell is considered in one case as the coexistence of multi-vegetation types and the other as one single typical vegetation type. A practical scheme is suggested for this kind of coupling, i.e. , a model grid cell is divided into several subgrid cells with each one being called "Tile" according to the number of vegetation types within the grid cell in the form of high resolution data. Meanwhile the land surface model is designed to be able to run simultaneously at different subgrid cells, rather than further to group the vegetation types from the high resolution data. By doing so, the same forcing is shared by all the subgrid cells within one grid cell as in the conventional way, but the ground fluxes need to be integrated from the subgrid cells by percentage of vegetation area coverage. As a matter of fact, the approach can be easily realized. In the meantime, the way to estimate effective ground temperature, effective sensible and latent heats and so on is proposed. In the offline experiments, the land surface model of SSiB and the field observation data of HAPEX-MOBILHY, which are generously provided by Xue who is also the SSiB author, are used to carry out the study. As for real condition, the field of HAPEX-MOBILHY which consists of forest with the percentage of 40 % and mixed agricultural crops with the percentage of 60 % should be categorized to grass land according to the classification in SSiB. Outputs of simulations show that there are big differences in the effective ground temperature, effective sensible and latent heats predicted respectively by three cases of the land surface including forest, grass and the coexistence of forest and grass. Also, the outputs show that the vegetation type with less percentage cover in a grid cell may make more contribution to the latent or sensible heat in the cell than the vegetation type with more percentage cover in the same grid cell. The validity of the method which considers the vegetation with more percentage in a cell as one representative vegetation type in the cell for some previous land surface model should be reevaluated.
出处 《应用气象学报》 CSCD 北大核心 2008年第2期129-136,共8页 Journal of Applied Meteorological Science
基金 国家自然科学基金项目(40575043,40233034) 中国科学院重点项目(KZCX3-SW-229) “十一五”国家科技支撑计划项目(2006BAC02B00)共同资助
关键词 陆面模式 尺度变换 植被类型 land surface scale conversation vegetation type
  • 相关文献

参考文献16

  • 1孙菽芬,金继明.陆面过程模式研究中的几个问题[J].应用气象学报,1997,8(A00):50-57. 被引量:34
  • 2张正秋,周秀骥,李维亮,孙菽芬.一些陆面要素非均匀分布对模式计算结果影响的理论分析[J].应用气象学报,2005,16(5):561-568. 被引量:2
  • 3Shao Y, Sogalla M, Kerschgens M, et al. Effects of land-surface heterogeneity upon surface fluxes and turbulent conditions. Meteorology and Atmospheric Physics, 2001,78:157-181.
  • 4Avissar R, Pielke R A, A pararneterization of heterogeneous land surfaces for atmospheric numerical models and its impact on regional meteorology. Mon Wea Rev ,1989,117(10) :2113-2136.
  • 5Hu Zhenglin, Islam Shafiqul, Jiang Le. Approaches for aggregating heterogeneous surface parameters and fluxes for mesoscale and climate models. Boundary-Layer Meteorology, 1999, 93 (2) :313-336.
  • 6Koster R D. A comparative analysis of two land surface heterogeneity representations. J Climate, 1992,5(12) :1379-1390.
  • 7Seth A F, Giorgi F, Dickinson R E. Simulating flux from heterogeneous land surface: Explicit sub-grid method employing the Biosphere-Atmosphere Transfer Scheme (BATS). J Geophys Rev, 1994, 99(D9): 18651-18667.
  • 8Leung R L, Ghan S J. A subgrid parameterization of orographic precipitation. Theor Appl Climatol, 1995, 52: 95-118.
  • 9钟中,苏炳凯,赵鸣.大气数值模式中有效粗糙度计算的一种新方法[J].自然科学进展,2002,12(5):519-523. 被引量:3
  • 10Pitman A J, Yang Z L, Cogley J G, et al. Description of Bare Essential of Surface Transfer for the Bureau of Meteorology Research Centre. AGCM. BMRC Research Report, No. 32, 1992.

二级参考文献5

共引文献36

同被引文献19

引证文献1

二级引证文献35

相关作者

内容加载中请稍等...

相关机构

内容加载中请稍等...

相关主题

内容加载中请稍等...

浏览历史

内容加载中请稍等...
;
使用帮助 返回顶部