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The energy exchange at the land surface during winter: existing theories and their limitations
KTH, Superseded Departments, Land and Water Resources Engineering.
(English)Manuscript (preprint) (Other academic)
National Category
Engineering and Technology
URN: urn:nbn:se:kth:diva-13340OAI: diva2:323988
QC 20100614Available from: 2010-06-14 Created: 2010-06-14 Last updated: 2010-06-14Bibliographically approved
In thesis
1. Land surface heat exchange over snow and frozen soil
Open this publication in new window or tab >>Land surface heat exchange over snow and frozen soil
2001 (English)Licentiate thesis, comprehensive summary (Other scientific)
Abstract [en]

The energy exchange in the soil-snow-vegetation-atmospheresystem was studied to improve the quantitative knowledge of thegoverning processes. The lack of such knowledge contributes tothe uncertainty in the applicability of many existing modelsindependent of the temporal or spatial scale. The theoreticalbackground and available methods for measurements and numericalsimulations were reviewed. Numerical simulation models andavailable data sets representing open land and boreal forestwere evaluated in both diurnal and seasonal time-scales.Surface heat fluxes, snow depth, soil temperatures andmeteorological conditions were measured at an agriculturalfield in central Sweden over two winters, 1997-1999. Twoone-dimensional simulation models of different complexity wereused to simulate the heat and water transfer in thesoil-snow-atmosphere system and compared with the measurements.Comparison of simulated and observed heat fluxes showed thatparameter values governing the upper boundary condition weremore important than the formulation of the internal mass andheat balance of the snow cover. The models were useful toevaluate the lack of energy balance closure in the observedsurface heat fluxes, which underlined the importance ofimproved accuracy in eddy correlation measurements of latentflow during winter conditions.

The representation of boreal forest in the land surfacescheme used within a weather forecast model was tested with athree-year data set from the NOPEX forest site in centralSweden. The formulation with separate energy balances forvegetation and the soil/snow beneath tree cover improvedsimulation of the seasonal and diurnal variations of latent andsensible heat flux compared with an older model version.Further improvements of simulated surface heat fluxes could beexpected if the variation of vegetation properties within andbetween years and a new formulation of the boundary conditionsfor heat flux into the soil is included.

Keywords: Surface energy balance, Snow, Boreal forest,SVAT models, Eddy-correlation Measurements, Latent heat flux,Sensible heat flux, Net radiation, Soil temperature,Aerodynamic roughness, Surface resistance

Place, publisher, year, edition, pages
Stockholm: KTH, 2001. iv, 14 p.
Trita-AMI. LIC, 2068
Surface energy balance, Snow, Boreal forest, SVAT models, Eddy-correlation Measurements, Latent heat flux, Sensible heat flux, Net radiation, Soil temperature, Aerodynamic roughness, Surface resistance
National Category
Civil Engineering
urn:nbn:se:kth:diva-1231 (URN)91-7283-061-1 (ISBN)
QC 20100614Available from: 2001-06-18 Created: 2001-06-18 Last updated: 2010-06-14Bibliographically approved

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