地球科学进展 ›› 2011, Vol. 26 ›› Issue (3): 300 -310. doi: 10.11867/j.issn.1001-8166.2011.03.0300

研究论文 上一篇    下一篇

陆面过程模型对下垫面参数动态变化的敏感性分析
蔡福 1,2,3,周广胜 1,李荣平 3,明惠青 4   
  1. 1.中国气象科学研究院,北京100081;
    2.南京信息工程大学,江苏南京 210044;
    3.中国气象局沈阳大气环境研究所,辽宁沈阳110016;
    4.辽宁省气象科技服务中心,辽宁沈阳110016
  • 收稿日期:2010-05-25 修回日期:2010-09-13 出版日期:2011-03-10
  • 通讯作者: 周广胜(1965-),男,江苏高淳人,研究员,主要从事全球变化与陆地生态系统观测与模拟研究.  E-mail:gszhou@cams.cma.gov.cn
  • 基金资助:

    国家杰出青年科学基金项目“大气边界层物理和大气湍流”(编号:40625015);国家重点基础研究发展计划项目“中国陆地生态系统对未来气候变化的脆弱性与适应性评估”(编号:2010CB951303)资助.

Sensitivity of Land Surfaces Model to Dynamic Land Surface Parameters

Cai Fu 1,2,3, Zhou Guangsheng 1, Li Rongping 3, Ming Huiqing 4   

  1. 1.Chinese Academy of Meteorological Sciences, Beijing100081,China; 
    2. Nanjing University of Information Science and Technology, Nanjing210044, China;3.Institute of Atmospheric Environment, China Meteorological Administration,Shenyang110016,China;
    4.Liaoning Province Meteorological Science and Technology Service Center, Shenyang110016,China
  • Received:2010-05-25 Revised:2010-09-13 Online:2011-03-10 Published:2011-03-10

利用2006年锦州玉米农田生态系统野外观测站动态连续的通量、气象及生物因子观测数据,分析了BATS1e陆面模型对动态的粗糙度(Z0)、叶面积指数(LAI)、植被覆盖度(FVEG)及反照率(α)变化的敏感性。结果表明:Z0的动态变化对表层土壤温度(SST)和感热(SH)的模拟有一定影响,主要发生在玉米农田从裸土向有植被覆盖转变这一阶段。LAI的动态赋值可以改善SST、净入射短波辐射(frs)、SHSWC的模拟效果,对潜热(LE)的模拟也有一定影响。动态FVEG对上述各变量的模拟影响最为明显,当FVEG较小时敏感性最大。α的动态赋值可影响SSTSHLE的模拟,其中SH反应最为敏感。各动态参数越接近模型设定值,模拟结果受影响越小;各参数间关系密切,单一参数的改进可提高某些变量的模拟精度,但不一定改善所有变量的模拟效果。

Using continuous flux data, meteorological data and biological data in 2006(from June 1 to August 9) from Jinzhou agricultural ecosystem research station, based on BATS1e model, the sensitivity of land surface model to dynamic assignment of roughness(Z0), leaf area index(LAI) and fractional vegetation coverage (FVEG) and albedo(α) were investigated. The results show that dynamic assignment of  Z0 has effect on simulating surface soil temperature(SST) and sensible heat flux (SH) especially on the time when maize field surface  covered  changes  from bare soil to vegetation. Dynamic LAI  plays important role in improving the  simulation of  SST, net absorbed solar energy flux(Frs), SH and surface soil water content(SWC), at the same time affects simulation of latent heat flux (LE). Dynamic FVEG affects obviously simulations of all abovementioned variables and shows greater sensitivity  when they are  smaller. Also, dynamical change of α can affect simulations of SST, LE and SH, especially for the latter. Furthermore, the interactions among different dynamic parameters are ignored by the model. The improvement of single land surface parameter might be helpful for simulating one or multivariate but not for all variables. In short, it is necessary to set up a parameterization scheme with the interactions of different land surface parameters.

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