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全球植被分布对气候影响的数值试验 被引量:17
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作者 曾红玲 季劲钧 吴国雄 《大气科学》 CSCD 北大核心 2010年第1期1-11,共11页
利用一个新的陆气双向耦合模式R42_AVIM,通过有无植被覆盖的对比试验分析,探讨了全球植被分布对气候和大气环流产生的潜在影响。得出:陆面植被覆盖使得地表特征参数发生行星尺度的明显改变,在叶面积指数大的热带和中高纬度森林带尤其显... 利用一个新的陆气双向耦合模式R42_AVIM,通过有无植被覆盖的对比试验分析,探讨了全球植被分布对气候和大气环流产生的潜在影响。得出:陆面植被覆盖使得地表特征参数发生行星尺度的明显改变,在叶面积指数大的热带和中高纬度森林带尤其显著。在现实植被分布下,陆地表面反照率减小,地表净辐射收支和地表潜热通量增加,而地表感热通量减小。植被叶面积指数比较大的区域地表温度降低,并且这种温度的改变一直延伸到对流层中上层,在热带表现为斜压结构,而在中高纬表现为相当正压结构。植被的存在使热带和中高纬度森林带的蒸发和相应的高层凝结潜热加热增强,从而增强了经圈环流的上升支,使得冬季在热带和南半球中纬度降水增多,夏季在热带和北半球中高纬地区降水明显增多;而经圈环流下沉支的增强致使副热带降水减少且更干旱。同时,植被的存在使大陆潜热释放增强,气温下降,减小了海陆温度对比,亚洲夏季风也有所减弱。 展开更多
关键词 陆气双向耦合模式r42_avim 植被分布 气候 大气环流
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An Updated Coupled Model for Land-Atmosphere Interaction.Part II:Simulations of Biological Processes 被引量:4
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作者 曾红玲 季劲钧 吴国雄 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2008年第4期632-640,共9页
In Part I, the authors succeeded in coupling the spectral atmospheric model (SAMIL_R42L9) developed at the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institut... In Part I, the authors succeeded in coupling the spectral atmospheric model (SAMIL_R42L9) developed at the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences (LASG/IAP/CAS) with the land surface model, Atmosphere-Vegetation-Interaction-Model (AVIM) and analyzed the climate basic state and land surface physical fluxes simulated by R42_AVIM. In this Part Ⅱ, we further evaluate the simulated results of the biological processes, including leaf area index (LAI), biomass and net primary productivity (NPP) etc. Results indicate that R42_AVIM can simulate the global distribution of LAI and has good consistency with the monthly mean LAI provided by Max Planck Institute for Meteorology. The simulated biomass corresponds reasonably to the vegetation classifications. In addition, the simulated annual mean NPP has a consistent distribution with the data provided by IGBP and MODIS, and compares well with the work in literature. This land-atmosphere coupled model will offer a new experiment tool for the research on the two-way interaction between climate and biosphere, and the global terrestrial ecosystem carbon cycle. 展开更多
关键词 SAMIL-R42L9 r42_avim vegetation-atmosphere interaction
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An Updated Coupled Model for Land-Atmosphere Interaction.Part I:Simulations of Physical Processes 被引量:2
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作者 曾红玲 王在志 +1 位作者 季劲钧 吴国雄 《Advances in Atmospheric Sciences》 SCIE CAS CSCD 2008年第4期619-631,共13页
A new two-way land-atmosphere interaction model (R42_AVIM) is fulfilled by coupling the spectral atmospheric model (SAMIL_R42L9) developed at the State Key Laboratory of Numerical Modeling for Atmospheric Sciences... A new two-way land-atmosphere interaction model (R42_AVIM) is fulfilled by coupling the spectral atmospheric model (SAMIL_R42L9) developed at the State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences (LASG/IAP/CAS) with the land surface model, Atmosphere-Vegetation-Interaction-Model (AVIM). In this coupled model, physical and biological components of AVIM are both included. Climate base state and land surface physical fluxes simulated by R42_AVIM are analyzed and compared with the results of R42_SSIB [which is coupled by SAMIL_R42L9 and Simplified Simple Biosphere (SSIB) models]. The results show the performance of the new model is closer to the observations. It can basically guarantee that the land surface energy budget is balanced, and can simulate June-July-August (JJA) and December-January- February (DJF) land surface air temperature, sensible heat flux, latent heat flux, precipitation, sea level pressure and other variables reasonably well. Compared with R42_SSIB, there are obvious improvements in the JJA simulations of surface air temperature and surface fluxes. Thus, this land-atmosphere coupled model will offer a good experiment platform for land-atmosphere interaction research. 展开更多
关键词 SAMIL-R42L9 r42_avim R42_SSIB land-atmosphere coupling
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