๐”– Bobbio Scriptorium
โœฆ   LIBER   โœฆ

One-dimensional snow water and energy balance model for vegetated surfaces

โœ Scribed by Jiming Jin; Xiaogang Gao; Soroosh Sorooshian; Zong-Liang Yang; Roger Bales; Robert E. Dickinson; Shu-Fen Sun; Guo-Xiong Wu


Publisher
John Wiley and Sons
Year
1999
Tongue
English
Weight
367 KB
Volume
13
Category
Article
ISSN
0885-6087

No coin nor oath required. For personal study only.

โœฆ Synopsis


We developed and evaluated a three-layer snow model for application in general circulation models. This onedimensional snow model has many features of the detailed physically based model SNTHERM, yet is computationally much simpler. We have also extended the point model to vegetated areas using the parameterization concepts of the Biosphere-Atmosphere Transfer Scheme (BATS). Results of model applications for two types of vegetated ยฎelds ร a short grassland in the French Alps and an old aspen forest in the southern study area of BOREAS ร were presented. The results, on one hand, indicate the suitability of the model structure and parameter setting; on the other hand, the results explore the limitation of using `point' ยฎeld observations to evaluate an area model.


๐Ÿ“œ SIMILAR VOLUMES


Modification and testing of a one-dimens
โœ Andrew M. Fox; Ian C. Willis; Neil S. Arnold ๐Ÿ“‚ Article ๐Ÿ“… 2008 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 328 KB

## Abstract A oneโ€dimensional energy and mass balance snow model (SNTHERM) has been modified for use with supraglacial snowpacks and applied to a point on Haut Glacier d'Arolla, Switzerland. It has been adapted to incorporate the underlying glacier ice and a siteโ€specific, empirically derived albed

Sub-grid parameterization of snow distri
โœ Charles H. Luce; David G. Tarboton; Keith R. Cooley ๐Ÿ“‚ Article ๐Ÿ“… 1999 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 346 KB ๐Ÿ‘ 1 views

Representation of sub-element scale variability in snow accumulation and ablation is increasingly recognized as important in distributed hydrologic modelling. Representing sub-grid scale variability may be accomplished through numerical integration of a nested grid or through a lumped modelling appr

Methods for developing time-series clima
โœ David Susong; Danny Marks; David Garen ๐Ÿ“‚ Article ๐Ÿ“… 1999 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 811 KB

Topographically distributed energy-and water-balance models can accurately simulate both the development and melting of a seasonal snowcover in the mountain basins. To do this they require time-series climate surfaces of air temperature, humidity, wind speed, precipitation, and solar and thermal rad

An investigation into the effect of spat
โœ T. J. Jolley; H. S. Wheater ๐Ÿ“‚ Article ๐Ÿ“… 1997 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 294 KB ๐Ÿ‘ 2 views

Land surface parameterizations used in atmospheric general circulation models (AGCMs) are one dimensional representations of the transfer of energy and water vapour at the earth's surface over grid squares that are typically of the order of 10 4 km 2 . It is known, however, that climate variables an

Seasonal, spatially distributed modellin
โœ Harald Kling; Josef Fรผrst; Hans Peter Nachtnebel ๐Ÿ“‚ Article ๐Ÿ“… 2006 ๐Ÿ› John Wiley and Sons ๐ŸŒ English โš– 631 KB

## Abstract In mountainous regions of mid latitudes, the accumulation and melting of snow plays an important role for the seasonal water balance. These processes not only exhibit a strong seasonality, but also a high spatial variability, which has to be accounted for when establishing distributed w