- The four land surface models:
GRIBTAB files needed to read the data:
Land Surface Models
National Centers for Environmental Prediction/Oregon State University/Air Force/Hydrologic Research Lab Model (NOAH)
The community
NOAH LSM was developed beginning in 1993 through a collaboration of
investigators from public and private institutions, spearheaded by the National
Centers for Environmental Prediction (Chen et al. 1996; Koren et al. 1999). NOAH is a stand-alone, 1-D
column model which can be executed in either coupled or uncoupled mode. The
model applies finite-difference spatial discretization methods and a
Crank-Nicholson time-integration scheme to numerically integrate the governing
equations of the physical processes of the soil-vegetation-snowpack medium. NOAH has been used operationally
in NCEP models since 1996, and it continues to benefit from a steady
progression of improvements (Betts et al. 1997; Ek et al. 2003). For more
information, go to:
http://www.emc.ncep.noaa.gov/mmb/gcp/noahlsm/Noah_LSM_USERGUIDE_2.7.1.htm
MOSAIC (Koster
and Suarez 1996) is a well established and theoretically sound LSM, as demonstrated by its
performance in PILPS and GSWP experiments. MOSAIC's physics and surface flux
calculations are similar to the SiB LSM (Sellers et al., 1986). It is a
stand-alone, 1-D column model that can be run both uncoupled and coupled to the
atmospheric column. MOSAIC was the first to treat subgrid scale variability by
dividing each model grid cell into a MOSAIC of tiles (after Avissar and Pielke
1989) based on the distribution of vegetation types within the cell. This
capability is now available in the LIS interface for all the models
it drives.
Common Land Model (CLM)
CLM was
conceived at the 1998 National Center for Atmospheric Research (NCAR) Climate System Model
(CSM) meeting, and it was subsequently developed by a grass-roots collaboration
of scientists. CLM includes superior components from each of three contributing
models: the NCAR Land Surface Model (Bonan 1998), the Biosphere-Atmosphere Transfer Scheme
(Dickinson et al. 1993), and the LSM of the Institute of Atmospheric Physics of
the Chinese Academy of Sciences (Dai and Zeng 1997). The model applies
finite-difference spatial discretization methods and a fully implicit time
integration scheme to numerically integrate the governing equations. CLM can be
run as a stand-alone, 1-D column model. It is also the land model for NCAR's
coupled Community Climate System Model
(CCSM). CLM continues to evolve, but only proven and well-tested physical
parameterizations and numerical schemes are installed in the official version
of the code. LIS currently uses CLM version 2.0. For more information, see:
http://www.cgd.ucar.edu/tss/clm/
Variable Infiltration Capacity (VIC) Model
VIC (Liang et al. 1994; Liang et al. 1996) was
originally developed in early 90’s and is maintained and upgraded at the University of Washington. The model focuses on runoff processes that are represented by
the variable infiltration curve, a parameterization of sub-grid variability in
soil moisture holding capacity, and nonlinear baseflow. VIC is a stand-alone,
1-D column model that is run uncoupled. Various simulation modes are available
including, water balance, energy balance, frozen soil, and other special
cases. This macro-scale hydrology model is used extensively in research over
the watersheds in the U.S. as well as globally (e.g. Liang et al. 1998; Hamlet
et al. 1999; Nijssen et al. 2001). For more information, see:
http://www.hydro.washington.edu/Lettenmaier/Models/VIC/VIChome.html
References
Avissar, R. and R.A. Pielke, A
parameterization of heterogeneous land-surface for atmospheric numerical models
and its impact on regional meteorology. Mon. Wea. Rev., 117:2113-2136,
1989.
Betts, A., F. Chen, K. Mitchell,
and Z. Janjic, Assessment of the land surface and boundary layer models in two
operational versions of the NCEP Eta model using FIFE data. Mon.Wea. Rev.,
125, 2896-2916, 1997.
Bonan, G.B., The land surface
climatology of the NCAR Land Surface Model coupled to the NCAR Community
Climate Model. J. Climate, 11, 1307-1326, 1998.
Chen, F., K. Mitchell, J.
Schaake, Y. Xue, H. Pan, V. Koren, Y. Duan, M. Ek, and A. Betts, Modeling of land-surface
evaporation by four schemes and comparison with FIFE observations. J.
Geophys. Res.,101 (D3), 7251-7268, 1996.
Dai, Y., and Q. Zeng, 1997: A
land surface model (IAP94) for climate studies, Part I: Formulation and
validation in off-line experiments. Advances in Atmos. Sci., 14, 443-460.
Dickinson, R. E., A.
Henderson-Sellers, and P. J. Kennedy, Biosphere–Atmosphere Transfer Scheme (BATS) version
1e as coupled to the NCAR Community Climate Model. NCAR Tech. Note
NCAR/TN-387+STR, 72 pp., 1993.
Ek, M. B., K. E. Mitchell, Y.
Lin, E. Rogers, P. Grunmann, V. Koren, G. Gayno, and J. D. Tarpley,
Implementation of Noah land surface model advances in the National Centers for
Environmental Prediction operational mesoscale Eta model, J. Geophys. Res., 108(D22), 8851,
doi:10.1029/2002JD003296, 2003.
Hamlet, A.F. and D.P. Lettenmaier, Effects of Climate Change
on Hydrology and Water Resources in the Columbia River Basin, Am. Water Res.
Assoc., 35(6), 1597-1623, 1999.
Koren, V., J. Schaake, K.
Mitchell, Q. Y. Duan, F. Chen, and J. M. Baker, A parameterization of snowpack
and frozen ground intended for NCEP weather and climate models. J. Geophys.
Res.,104, 19569-19585, 1999.
Koster, R. D., and M. J. Suarez,
Energy and Water Balance Calculations in the MOSAIC LSM. NASA Technical
Memorandum 104606, 9, 76 pp., 1996.
Liang, X., D. P. Lettenmaier, E. F. Wood, and S. J. Burges,
A Simple hydrologically Based Model of Land Surface Water and Energy Fluxes for
GSMs, J. Geophys. Res., 99(D7), 14,415-14,428, 1994.
Liang, X., D. P. Lettenmaier, E. F. Wood, One-dimensional
Statistical Dynamic Representation of Subgrid Spatial Variability of
Precipitation in the Two-Layer Variable Infiltration Capacity Model, J. Geophys.
Res., 101(D16) 21,403-21,422, 1996.
Liang, X., E. F. Wood, D. Lohmann, D.P. Lettenmaier, and
others, The Project for Intercomparison of Land-surface Parameterization
Schemes (PILPS) Phase-2c Red-Arkansas River Basin Experiment: 2. Spatial and
Temporal Analysis of Energy Fluxes, J. Global and Planetary Change, 19,
137-159, 1998.
Nijssen, B.N., R. Schnur and D.P. Lettenmaier, Global
retrospective estimation of soil moisture using the VIC land surface model,
1980-1993, J. Clim. 14, 1790-1808. , 2001.
Sellers, P. J., Y. Mintz, and A.
Dalcher, 1986: A simple biosphere model (SiB) for use within general
circulation models. J. Atmos. Sci., 43: 505-531.