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-List Of Titles -The representation of snow in land-surface schemes : results from PILPS 2(d)

Please use this identifier to cite or link to this item: http://hdl.handle.net/1959.14/17237

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Title
The representation of snow in land-surface schemes : results from PILPS 2(d)
Related
Journal of hydrometeorology, Vol. 2, Issue 1, p.7-25
DOI
10.1175/1525-7541(2001)002<0007:TROSIL>2.0.CO;2
Publisher
American Meteorological Society
Date
2001
Author/Creator
Slater, A. G
Author/Creator
Schlosser, C. A
Author/Creator
Chen, F
Author/Creator
Cox, P. M
Author/Creator
de Rosnay, P
Author/Creator
Dickinson, R. E
Author/Creator
Dai, Y. -J
Author/Creator
Duan, Q
Author/Creator
Entin, J
Author/Creator
Etchevers, P
Author/Creator
Gedney, N
Author/Creator
Gusev, Ye. M
Author/Creator
Desborough, C. E
Author/Creator
Habets, F
Author/Creator
Kim, J
Author/Creator
Koren, V
Author/Creator
Kowalczyk, E. A
Author/Creator
Nasonova, O. N
Author/Creator
Noilhan, J
Author/Creator
Schaake, S
Author/Creator
Shmakin, A. B
Author/Creator
Smirnova, T. G
Author/Creator
Verseghy, D
Author/Creator
Pitman, A. J
Author/Creator
Wetzel, P
Author/Creator
Xue, Y
Author/Creator
Yang, Z. -L
Author/Creator
Zeng, Q
Author/Creator
Henderson-Sellers, A
Author/Creator
Robock, A
Author/Creator
Vinnikov, K. Ya
Author/Creator
Mitchell, K
Author/Creator
Boone, A
Author/Creator
Braden, H
Description
Twenty-one land surface schemes (LSSs) performed simulations forced by 18 yr of observed meteorological data from a grassland catchment at Valdai, Russia, as part of the Project for the Intercomparison of Land-Surface Parameterization Schemes (PILPS) Phase 2(d). In this paper the authors examine the simulation of snow. In comparison with observations, the models are able to capture the broad features of the snow regime on both an intra- and interannual basis. However, weaknesses in the simulations exist, and early season ablation events are a significant source of model scatter. Over the 18-yr simulation, systematic differences between the models’ snow simulations are evident and reveal specific aspects of snow model parameterization and design as being responsible. Vapor exchange at the snow surface varies widely among the models, ranging from a large net loss to a small net source for the snow season. Snow albedo, fractional snow cover, and their interplay have a large effect on energy available for ablation, with differences among models most evident at low snow depths. The incorporation of the snowpack within an LSS structure affects the method by which snow accesses, as well as utilizes, available energy for ablation. The sensitivity of some models to longwave radiation, the dominant winter radiative flux, is partly due to a stability-induced feedback and the differing abilities of models to exchange turbulent energy with the atmosphere. Results presented in this paper suggest where weaknesses in macroscale snow modeling lie and where both theoretical and observational work should be focused to address these weaknesses.
Description
19 page(s)
Resource Type
journal article
Organisation
Macquarie University. Dept. of Physical Geography

Identifier
http://hdl.handle.net/1959.14/17237
Identifier
ISSN:1525-7541
Identifier
mq-rm-2001012132
Language
eng
Reviewed
Reviewed
Save/E-mail Citation
Citation Format
E-mail Address
Subject
"Journal of hydrometeorology"
 
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