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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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Myfanwy King,Tim Marsh,Zeynep Akcaynd 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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https://doi.org/10.1007/978-3-030-88272-3rated 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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Menna Elshahawy,Said Mostafa,Nada Sharafvers 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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Lecture Notes in Computer Sciencetrating an enhanced capability to model melt related runoff. Future research is required to accurately model both snow-covered area and runoff at a variety of scales and to incorporate topographic and vegetation effects correctly in the models.
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