Boreal Forest Surface Parameterization in the ECMWF Model—1D Test with NOPEX Long-Term DataSource: Journal of Applied Meteorology:;2003:;volume( 042 ):;issue: 001::page 95Author:Gustafsson, D.
,
Lewan, E.
,
van den Hurk, B. J. J. M.
,
Viterbo, P.
,
Grelle, A.
,
Lindroth, A.
,
Cienciala, E.
,
Mölder, M.
,
Halldin, S.
,
Lundin, L-C.
DOI: 10.1175/1520-0450(2003)042<0095:BFSPIT>2.0.CO;2Publisher: American Meteorological Society
Abstract: The objective of the present study was to assess the performance and recent improvements of the land surface scheme used operationally in the European Centre for Medium-Range Weather Forecasts (ECMWF) in a Scandinavian boreal forest climate/ecosystem. The previous (the 1999 scheme of P. Viterbo and A. K. Betts) and the new (Tiled ECMWF Surface Scheme for Exchange Processes over Land, TESSEL) surface schemes were validated by single-column runs against data from NOPEX (Northern Hemisphere Climate-Processes Land-Surface Experiment). Driving and validation datasets were prepared for a 3-yr period (1994?96). The new surface scheme, with separate surface energy balances for subgrid fractions (tiling), improved predictions of seasonal as well as diurnal variation in surface energy fluxes in comparison with the old scheme. Simulated wintertime evaporation improved significantly as a consequence of the introduced additional aerodynamic resistance for evaporation from snow lying under high vegetation. Simulated springtime evaporation also improved because the limitation of transpiration in frozen soils was now accounted for. However, downward sensible heat flux was still underestimated during winter, especially at nighttime, whereas soil temperatures were underestimated in winter and overestimated in summer. The new scheme also underestimated evaporation during dry periods in summer, whereas soil moisture was overestimated. Sensitivity tests showed that further improvements of simulated surface heat fluxes and soil temperatures could be obtained by calibration of parameters governing the coupling between the surface and the atmosphere and the ground heat flux, and parameters governing the water uptake by the vegetation. Model performance also improved when the seasonal variation in vegetation properties was included.
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contributor author | Gustafsson, D. | |
contributor author | Lewan, E. | |
contributor author | van den Hurk, B. J. J. M. | |
contributor author | Viterbo, P. | |
contributor author | Grelle, A. | |
contributor author | Lindroth, A. | |
contributor author | Cienciala, E. | |
contributor author | Mölder, M. | |
contributor author | Halldin, S. | |
contributor author | Lundin, L-C. | |
date accessioned | 2017-06-09T14:08:38Z | |
date available | 2017-06-09T14:08:38Z | |
date copyright | 2003/01/01 | |
date issued | 2003 | |
identifier issn | 0894-8763 | |
identifier other | ams-13211.pdf | |
identifier uri | http://onlinelibrary.yabesh.ir/handle/yetl/4148637 | |
description abstract | The objective of the present study was to assess the performance and recent improvements of the land surface scheme used operationally in the European Centre for Medium-Range Weather Forecasts (ECMWF) in a Scandinavian boreal forest climate/ecosystem. The previous (the 1999 scheme of P. Viterbo and A. K. Betts) and the new (Tiled ECMWF Surface Scheme for Exchange Processes over Land, TESSEL) surface schemes were validated by single-column runs against data from NOPEX (Northern Hemisphere Climate-Processes Land-Surface Experiment). Driving and validation datasets were prepared for a 3-yr period (1994?96). The new surface scheme, with separate surface energy balances for subgrid fractions (tiling), improved predictions of seasonal as well as diurnal variation in surface energy fluxes in comparison with the old scheme. Simulated wintertime evaporation improved significantly as a consequence of the introduced additional aerodynamic resistance for evaporation from snow lying under high vegetation. Simulated springtime evaporation also improved because the limitation of transpiration in frozen soils was now accounted for. However, downward sensible heat flux was still underestimated during winter, especially at nighttime, whereas soil temperatures were underestimated in winter and overestimated in summer. The new scheme also underestimated evaporation during dry periods in summer, whereas soil moisture was overestimated. Sensitivity tests showed that further improvements of simulated surface heat fluxes and soil temperatures could be obtained by calibration of parameters governing the coupling between the surface and the atmosphere and the ground heat flux, and parameters governing the water uptake by the vegetation. Model performance also improved when the seasonal variation in vegetation properties was included. | |
publisher | American Meteorological Society | |
title | Boreal Forest Surface Parameterization in the ECMWF Model—1D Test with NOPEX Long-Term Data | |
type | Journal Paper | |
journal volume | 42 | |
journal issue | 1 | |
journal title | Journal of Applied Meteorology | |
identifier doi | 10.1175/1520-0450(2003)042<0095:BFSPIT>2.0.CO;2 | |
journal fristpage | 95 | |
journal lastpage | 112 | |
tree | Journal of Applied Meteorology:;2003:;volume( 042 ):;issue: 001 | |
contenttype | Fulltext |