Gao Zhiqiu, Bian Lingen, Cheng Yanjie, et al. Modeling of energy budget using simple biosphere model version 2(SiB2) over Tibetan Naqu prairie. J Appl Meteor Sci, 2002, 13(2): 129-141.
Citation: Gao Zhiqiu, Bian Lingen, Cheng Yanjie, et al. Modeling of energy budget using simple biosphere model version 2(SiB2) over Tibetan Naqu prairie. J Appl Meteor Sci, 2002, 13(2): 129-141.

MODELINGOF ENERGY BUDGET USING SIMPLE BIOSPHERE MODEL VERSION 2(SiB2) OVER TIBETAN NAQU PRAIRIE

  • Received Date: 2000-03-03
  • Rev Recd Date: 2000-08-20
  • Publish Date: 2002-04-30
  • SiB2 (Simple Biosphere model version 2) is adopted to simulate surface energy budget in offline mode with certain atmospheric forcing values measured in the near surface observations taken over in the Tibetan short grass prairie as a part of the GAME/Tibet (DEWEX Asian Monsoon Experiment/Tibet) experiment. On the condition that all parameters are reasonably fixed, the simulated net radiation, latent heat flux and soil heat flux are shown to be basically in agreement with observations with their relative errors being 8% (underestimated), 6% (underestimated), and 3% (underestimated), respectively; in meantime, SiB2 overestimates sensible heat flux by 40%. The detail analysis about energy components is conducted.
  • [1]
    Krishnamurti T N, Ramanathan Y.Sensitivity of the monsoon onset to different heating.Mon.Wea.Rev., 1982, 39:1090-1306.
    [2]
    Murakami T, Chen L X, Xie A.Relationship among seasonal cycles, low frequency oscillations and transient disturbances as revealed from OLR data.Mon.Wea.Rev., 1986, 114:1456-1465. doi:  10.1175/1520-0493(1986)114<1456:RASCLF>2.0.CO;2
    [3]
    Chen L X, Reiter E, Feng Z Q.The atmospheric heat sources over the Tibetan plateau:May-Agugst 1979.Mon.Wea.Rev., 1985, 113:1771-1790. doi:  10.1175/1520-0493(1985)113<1771:TAHSOT>2.0.CO;2
    [4]
    Sellers P J, Randall D A, Collatz G J, et al.A revised land surface parameterization (SiB2) for atmospheric GCMs.Part I:Model formulation.Journal of Climate, 1996a, 9:676-705. doi:  10.1175/1520-0442(1996)009<0676:ARLSPF>2.0.CO;2
    [5]
    Sellers P J, Los S O, Tucker C J, et al.A revised land surface parameterization (SiB2) for atmospheric GCMs.Part II:The generation of global fields of terrestrial biophysical parameters from satellite data.Journal of Climate, 1996b, 9:706-737. doi:  10.1175/1520-0442(1996)009<0706:ARLSPF>2.0.CO;2
    [6]
    Kim J, Choi T, Lee H, et al.Energy partitioning and its imbalance over a prairie site in central Tibetan plateau during GAME-IOP 1998.Journal of Meteorological Society of Japan, 2001, (accepted).
    [7]
    Garratt J R.Extreme maximum land surface temperatures.Journal of Applied Meteorology, 1992, 31:1097.
    [8]
    Stull R B.Introduction to Boundary Layer Meteorology.London:Kluwer Academic Publishes, 1988.287.
    [9]
    Dickinson R E.Land surface processes and climate-surface albedos and energy balance.Advances in Geophysics, 1983, 48.
    [10]
    Randall D A, Dazlich D A, Zhang C.A revised land surface parameterization (SiB2) for atmospheric GCMs.Part III:The greening of the Colorado State University general circulation model.Journal of Climate, 1996, 9:738-763. doi:  10.1175/1520-0442(1996)009<0738:ARLSPF>2.0.CO;2
    [11]
    Gao Z, Wang J, Ma Y, et al.Study of roughness lengths and drag coefficients over Nansha Sea Region, Gobi, Desert, Oasis and Tibetan Plateau.Phys.Chem.Earth (B), 2000, 25 (2):141-145. doi:  10.1016/S1464-1909(99)00126-4
    [12]
    Monteith J L.Principles of Environmental Physics.New York:American Elsvier Publishing Company, Inc, 1973.39-52.
  • 加载中
  • -->

Catalog

    Figures(7)

    Article views (4381) PDF downloads(1936) Cited by()
    • Received : 2000-03-03
    • Accepted : 2000-08-20
    • Published : 2002-04-30

    /

    DownLoad:  Full-Size Img  PowerPoint