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

丑恶

Interannual Variability of the Thermal Components and Bulk Heat Exchange of Great Slave Lake,longer-term climatic conditions. The lake is dimictic and exhibits spatial and temporal variability in air temperature and wind speed that impacts water surface temperature and lake heat flux. Storm events with high winds were responsible for short-term highly dynamical responses of the lake, with d

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Flow Connectivity of a Lake-Stream System in a Semi-arid Precambrian Shield Environment,nection in the lake-stream system, a chain of lakes in northern Canada was studied in 2004. Water balance shows that rapid and substantial runoff from the local basin slopes during the snowmelt period led to a rise of lake levels above their outlet elevations to generate outflow. Continued summer ev

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灰心丧气

Impact of Climate Change on the Peace River Thermal Ice Regime,the ice regime of the Peace River in Alberta. The model employs an Eulerian frame of reference for both the flow hydrodynamics and the ice processes (ice cover formation and deterioration) and uses the characteristic-dissipative-Galerkin finite element method to solve the primary equations. Model ca

arthroscopy

Climate Impacts on Ice-jam Floods in a Regulated Northern River,ice-jam flooding in the lower Peace River has resulted in prolonged dry periods and considerable reduction in the area covered by lakes and ponds that provide habitat for aquatic life in the PAD. Using archived hydrometric data and in situ observations, the ice regime of the lower Peace is quantifie

向外才掩饰

Trends in Mackenzie River Basin Streamflows, annual trends were identified using the Mann-Kendall test with an approach that corrects for serial correlation. The global (or field) significance of the results for each watershed was evaluated using a bootstrap resampling technique. The results reveal more trends in some hydrologic variables tha

conference

https://doi.org/10.1007/978-3-540-75136-6Atmospheric; Frost; Hydrologic; Infiltration; Precipitation; Scale; Snow; Storm; climate change; digital elev