Validation and comparison of two soil-vegetation-atmosphere transfer models for tropical Africa

被引:21
|
作者
Akkermans, T. [1 ]
Lauwaet, D. [1 ]
Demuzere, M. [1 ]
Vogel, G. [6 ]
Nouvellon, Y. [3 ,7 ,8 ]
Ardo, J. [2 ]
Caquet, B. [3 ,7 ]
De Grandcourt, A. [3 ,7 ]
Merbold, L. [5 ]
Kutsch, W. [4 ]
Van Lipzig, N. [1 ]
机构
[1] Katholieke Univ Leuven, Dept Earth & Environm Sci, B-3001 Heverlee, Belgium
[2] Lund Univ, Dept Phys Geog & Ecosyst Sci, SE-22362 Lund, Sweden
[3] Ctr Cooperat Int Rech Agron Dev CIRAD, UMR Eco & Sols, F-34060 Montpellier, France
[4] Johann Heinrich von Thunen Inst, Inst Agrarrelevante Klimaforsch, D-38116 Braunschweig, Germany
[5] ETH, Inst Agr Sci, Grassland Sci Grp, CH-8092 Zurich, Switzerland
[6] Deutsch Wetterdienst, Meteorol Observ Lindenberg, D-15848 Tauche, Germany
[7] Ctr Rech Durabilite & Prod Plantat Ind CRDPI, Pointe Noire, DEM REP CONGO
[8] Univ Sao Paulo, Escola Super Agr Luiz de Queiroz, Dept Ciencias Atmosfer, Sao Paulo, Brazil
关键词
ROOTING DEPTH; HEAT-FLUX; CLIMATE; WATER; CARBON; ENERGY; RADIATION; EVAPORATION; EXCHANGES; EQUATIONS;
D O I
10.1029/2011JG001802
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This study aims to compare and validate two soil-vegetation-atmosphere-transfer (SVAT) schemes: TERRA-ML and the Community Land Model (CLM). Both SVAT schemes are run in standalone mode (decoupled from an atmospheric model) and forced with meteorological in-situ measurements obtained at several tropical African sites. Model performance is quantified by comparing simulated sensible and latent heat fluxes with eddy-covariance measurements. Our analysis indicates that the Community Land Model corresponds more closely to the micrometeorological observations, reflecting the advantages of the higher model complexity and physical realism. Deficiencies in TERRA-ML are addressed and its performance is improved: (1) adjusting input data (root depth) to region-specific values (tropical evergreen forest) resolves dry-season underestimation of evapotranspiration; (2) adjusting the leaf area index and albedo (depending on hard-coded model constants) resolves overestimations of both latent and sensible heat fluxes; and (3) an unrealistic flux partitioning caused by overestimated superficial water contents is reduced by adjusting the hydraulic conductivity parameterization. CLM is by default more versatile in its global application on different vegetation types and climates. On the other hand, with its lower degree of complexity, TERRA-ML is much less computationally demanding, which leads to faster calculation times in a coupled climate simulation.
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页数:15
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