Titlebook: Cold Region Atmospheric and Hydrologic Studies. The Mackenzie GEWEX Experience; Volume 2: Hydrologic Ming-ko Woo Book 2008 Springer-Verlag

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蹣跚

Excise

Analysis and Application of 1-km Resolution Visible and Infrared Satellite Data over the Mackenzie collected at 1-km resolution over the Mackenzie Basin specifically for the Mackenzie GEWEX Study (MAGS) water year and the Canadian GEWEX Enhanced Study period. Through the use of satellite data, clear sky products (land surface temperature, evapotranspiration, water temperature time series over la

construct

On the Use of Satellite Passive Microwave Data for Estimating Surface Soil Wetness in the Mackenziesin using SSM/I remotely sensed brightness temperature measurements. The approach accounts for the seasonal evolution of the vegetation state and the basin surface heterogeneity. Results demonstrate that the approach can filter out the vegetation effect and produce reasonable estimates of . at the b

crescendo

Studies on Snow Redistribution by Wind and Forest, Snow-covered Area Depletion, and Frozen Soil Infwing snow, interception and sublimation of snow in forest canopies, snow spatial distributions in complex environments, snowmelt in open environments and under forest canopies, advection of energy from bare ground to snow, snowcover depletion during melt, and heat and mass transfer during infiltrati

violate

violate

Modeling Maximum Active Layer Thaw in Boreal and Tundra Environments using Limited Data,uatic ecosystems, and the integrity of northern infrastructure, including oil and gas pipelines. For most planning and management purposes, the long-term probability distribution of active layer thickness is of primary interest. This study presents a robust method for calculating maximum active laye

hegemony

Climate-Lake Interactions,enience they are classified into small, medium and large in terms of surface area. MRB lakes are subjected to a wide range in air temperature from south to north, and to substantial differences in precipitation. The ice-covered period is a function of lake size and location. Small lakes have a longe

essential-fats

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