HR: 0800h
AN: C31A-0285    [Abstracts]
TI: The Effects of Vegetation Canopy Processes on Snow Surface Energy and Mass Balances
AU: * Niu, G
EM: niu@geo.utexas.edu
AF: The Department of Geological Sciences, The Univ. of Texas at Austin, Austin, TX 78712 United States
AU: Yang, Z
EM: liang@mail.utexas.edu
AF: The Department of Geological Sciences, The Univ. of Texas at Austin, Austin, TX 78712 United States
AB: This paper addresses the effects of canopy physical processes on snow mass and energy balances in boreal ecosystems. We incorporate new parameterizations of radiation transfer through the vegetation canopy, interception of snow by the vegetation canopy, and under-canopy sensible heat transfer processes into the Versatile Integrator of Surface and Atmosphere (VISA) and test the model results against the Boreal Ecosystem-Atmosphere Study (BOREAS) data observed at South Study Area, Old Jack Pine (SSA-OJP). A modified two-stream radiation transfer scheme that accounts for the three-dimensional (3-D) geometry of vegetation accurately simulates the transferring of solar radiation through the vegetation canopy when the leaf and stem area index (LSAI) is reduced to match the observed, but the simulated wintertime surface albedos are higher than the observed. This overestimation can be removed by lowering the fractional snow cover on the canopy through the introduction of a snow interception model that explicitly describes the loading and unloading of snow and the melting and refreezing of snow. VISA overestimates the downward sensible heat fluxes from the canopy to the snow surface, which leads to earlier snow ablation and a shallower snowpack than the observed. Explicitly including a canopy heat storage term in the canopy energy balance equation decreases the spuriously large amplitude of the diurnal canopy temperature variation and reduces the excessive daytime sensible heat flux from the canopy downward to the snow surface. Sensitivity tests reveal that the turbulent sensible heat flux below the vegetation canopy strongly depends on the canopy absorption coefficient of momentum. During spring, the daytime temperature difference between the snow surface and the vegetation canopy forms a strongly stable atmospheric condition, which results in a larger absorption coefficient of momentum and a weak turbulent sensible heat flux. The modeled excessive downward sensible heat flux from the vegetation canopy to the snow surface is considerably reduced through the stability correction to the canopy absorption coefficient of momentum.
UR: http://www.geo.utexas.edu/climate/Research/publications.htm
DE: 1655 Water cycles (1836)
DE: 1863 Snow and ice (1827)
DE: 1620 Climate dynamics (3309)
SC: Cryosphere [C]
MN: 2004 AGU Fall Meeting