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Skip to Search Results- 11Myers, Paul G.
- 5Smith, Daniel W.
- 3Haines, Keith
- 2Chowdhury, T
- 2El-Din, Mohamed Gamal
- 2Hall, Eric R.
- 25Graduate and Postdoctoral Studies (GPS), Faculty of
- 25Graduate and Postdoctoral Studies (GPS), Faculty of/Theses and Dissertations
- 14Oil Sands Research and Information Network (OSRIN)
- 12Earth and Atmospheric Sciences, Department of
- 12Earth and Atmospheric Sciences, Department of/Journal Articles (Earth and Atmospheric Sciences)
- 10Sustainable Forest Management Network
- 25Thesis
- 24Report
- 23Article (Published)
- 1Article (Draft / Submitted)
- 1Conference/Workshop Poster
- 1Conference/Workshop Presentation
- 5Department of Chemical and Materials Engineering
- 4Department of Earth and Atmospheric Sciences
- 4Department of Mechanical Engineering
- 3Department of Renewable Resources
- 2Department of Civil and Environmental Engineering
- 2Department of Resource Economics and Environmental Sociology
- 2Myers, Paul G. (Earth and Atmospheric Sciences)
- 1Adamowicz, Vic (Resource Economics and Environmental Sociology)
- 1Adamowicz, Vic (Rural Economy)
- 1Amirfazli, Alidad (Mechanical Engineering, University of Alberta and York University)
- 1Ashbolt, Nicholas (Public Health)
- 1Bolton, James R. (Civil and Environmental Engineering)
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1979-01-01
This report contains all the available suspended sediment discharge information for 1976 that was collected by Water Survey of Canada and by Alberta Oil Sands Environmental Research Program (AOSERP) personnel within the AOSERP study boundaries. Information on suspended sediment concentrations at...
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1977-01-01
Loeppky, K. D., Spitzer, M. O.
This report contains hydrometric data for the Alberta Oil Sands Environmental Research Program (AOSERP) study area to December, 1976. All available daily discharge data are contained within Appendices of this report. The report also contains annual hydrographs of discharge data, water level...
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2007
Kulan, Nilgun, Ribergaard, Mads H., Myers, Paul G.
We examine the historical variability of Irminger Water (IW) along 3 sections across the West Greenland Current over 1950–2005. Significant variability in the salinity, size and position of the IW core are seen over time. Some of the saltiest and warmest IW ever recorded have been seen since 1995...
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2006
Shabber, A., Logan, K., Flannigan, M.D., Skinner, W.R.
Relationships between variations in peak Canadian forest fire season (JJA) severity and previous winter (DJF) global sea surface temperature (SST) variations are examined for the period 1953 to 1999. Coupled modes of variability between the seasonal severity rating (SSR) index and the previous...
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Mathematical modeling of nitrous oxide emissions from an agricultural field during spring thaw
Download1999
Confidence in regional estimates of N2O emissions used in national greenhouse gas inventories could be improved by using mathematical models of the biological and physical processes by which these emissions are known to be controlled. However these models must first be rigorously tested against...
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Mechanisms of Aggregation and Separation of Water and Solids from Bitumen Froth using Cluster Size Distribution
DownloadFall 2016
The large-scale corrosion and equipment damage caused by water and solids respectively in bitumen froth necessitate their removal using various methods. This study is aimed at understanding how water and solids aggregate (water-water, water-solid and solid-solid) in bitumen froth and what the...
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Modeling the paleocirculation of the Mediterranean: The Last Glacial Maximum and the Holocene with emphasis on the formation of sapropel S1
Download1998
Myers, Paul G., Rohling, Eelco J., Haines, Keith
An ocean general circulation model is used to simulate the thermohaline circulation in the Mediterranean sea during the last glacial maximum and the Holocene, when the sapropel S1 was deposited. The model is forced by prescribed surface temperatures and salinities, where present-day values lead...
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Numerical modelling of the Arctic and North Atlantic exchanges with NEMO: Focus on freshwater and dynamics
DownloadFall 2018
The Arctic is currently undergoing significant changes due to increasing anthropogenic greenhouse gases causing atmospheric warming. The impact of this warming is clearly visible in the Arctic: reduced sea-ice cover, enhanced land-ice melting, increased frequency of extreme weather, etc....