S
Scott R. Dallimore
Researcher at Geological Survey of Canada
Publications - 109
Citations - 4693
Scott R. Dallimore is an academic researcher from Geological Survey of Canada. The author has contributed to research in topics: Clathrate hydrate & Permafrost. The author has an hindex of 33, co-authored 106 publications receiving 4103 citations. Previous affiliations of Scott R. Dallimore include Natural Resources Canada.
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Journal ArticleDOI
Sensitivity of the carbon cycle in the Arctic to climate change
A. David McGuire,Leif G. Anderson,Torben R. Christensen,Scott R. Dallimore,Laodong Guo,Daniel J. Hayes,Martin Heimann,Thomas D. Lorenson,Robie W. Macdonald,Nigel T. Roulet +9 more
TL;DR: In this article, a comprehensive review of the status of the contemporary carbon cycle of the Arctic and its response to climate change is presented to clarify key uncertainties and vulnerabilities in the response of the carbon cycle in the Arctic to ongoing climatic change.
ReportDOI
Scientific Results from the Mallik 2002 Gas Hydrate Production Research Well Program, Mackenzie Delta, Northwest Territories, Canada
TL;DR: The results of the Mallik 2002 Gas Hydrate Production Research Well Program (MHP-2002) are described in this article, which is a joint effort of 300 scientists from Japan, Canada, Germany, the United States and India.
Journal ArticleDOI
Identification of Younger Dryas outburst flood path from Lake Agassiz to the Arctic Ocean
TL;DR: A large flood into the Arctic Ocean at the start of the Younger Dryas leads us to reject the widespread view that Agassiz overflow at this time was solely eastward into the North Atlantic Ocean.
Journal ArticleDOI
Numerical studies of gas production from several CH4 hydrate zones at the Mallik site, Mackenzie Delta, Canada
George J. Moridis,Timothy S. Collett,Scott R. Dallimore,Tohru Satoh,Steven H. Hancock,Brian Weatherill +5 more
TL;DR: In this article, the analysis of various gas production scenarios from five methane hydrate-bearing zones at the Mallik site is presented, where a gas hydrate research well was drilled at the site in 1998, and numerical simulations using the EOSHYDR2 model indicated that gas production from hydrates at Mallik Site was possible by depressurizing a thin free gas zone at the base of the hydrate stability field.