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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灰心丧气

Tim Marsh,Ashima Thomas,Eng Tat Khoocoefficients (C . ) for each lake and for groups of lakes. Transfer coefficients determined from multiple years of data for the two smallest lakes were similar (1.26 x 10 . and 1.30 x 10 . ) while that for the largest lake was slightly smaller (1.10 x 10 . ). The coefficient for the medium-size lake

Picks-Disease

Myfanwy King,Tim Marsh,Zeynep Akcay of time scales on the magnitude and control of the process. Based on measurements using the eddy covariance method, both the latent and sensible heat fluxes were consistently small following ice break up, but increased dramatically as ice formation commenced. Half of the total evaporative water los

泥瓦匠

美丽的写

Myfanwy King,Tim Marsh,Zeynep Akcaynection 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

Generic-Drug

https://doi.org/10.1007/978-3-030-88272-3e. The northwestern portion of the Shield has a relatively dry, subarctic climate and a heterogeneous landscape comprising exposed bedrock uplands, soil mantled slopes, wetlands and lakes. The water budget of bedrock uplands is influenced by rock fractures, slope aspect, precipitation or melt intens

深陷

Overstate

沉思的鱼

Menna Elshahawy,Said Mostafa,Nada Sharafed damages. However, our ability to forecast such events remains quite limited. An example of this is the Athabasca River at Fort McMurray, Alberta, where severe ice jam events have been documented for over 100 years, and where breakup has been monitored intensively for the past 25 years. Despite th

GRILL

Sundus Fatima,Jannicke Baalsrud Haugethe 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