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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Flow Connectivity of a Lake-Stream System in a Semi-arid Precambrian Shield Environment,nd spill of lakes should be considered in modeling Shield hydrology under semi-arid conditions, to take account of (1) antecedent storage in individual lakes, (2) their storage change calculated through water balance, and (3) the thresholds to be exceeded for outflows to occur.

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Hydrology of the Northwestern Subarctic Canadian Shield,rated in headwaters can be transferred to basin outlets. The subarctic Shield environment has large spatial and temporal variations in available storage, where the hydrologic connectivity that dictates runoff response is controlled in part by the geometry and spatial distribution of landscape compon

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Climate Impacts on Ice-jam Floods in a Regulated Northern River,vers would be slightly thinner than they are at present. More importantly, a large part of the Peace River basin is expected to experience frequent and sustained mid-winter thaws. These events are expected to cause significant melt and depleted snowpack in the spring, leading to severe reduction in

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Minhua Ma,Bobbie Fletcher,Tim Marshomponent in estimating the ., and to downscale the index at the digital elevation models scale using a topographic index (.) which is continuously adjusted to account for vegetation growth. When applied to the Peace-Athabasca-Delta area, this method improved the correlation between soil wetness and

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Tim Marsh,Ashima Thomas,Eng Tat Khoogest that the multi-year coefficients give acceptable results for small and medium-size lakes only, and that these coefficients cannot be transferred from one lake to another, unless the lakes are similar in size.

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Myfanwy King,Tim Marsh,Zeynep Akcayous sampling intervals. Varying the sampling interval from one to six hours in 1-hr steps had no significant effect on the coefficients used to predict the 24-hr evaporation totals. The dichotomy between lake and land surfaces in terms of temporal changes in heat source and sink, and the longer dura

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Lecture Notes in Computer Scienceure differences. Variation of the 8 ° C isotherm effectively demonstrated interannual variability in the lake heating. Annual heat content ranged from 2.61 × 10. J in 1998 to 2.13 × 10. J in 2002. Five-year mean heat content maximum was 2.24 × 10. J. The bulk heat exchange, ranging between 267 W m.