Impact of permafrost dynamics on Arctic groundwater flow systems with application to the evolution of spring and lake taliks
Groundwater flow in permafrost is restricted to unfrozen zones, known as taliks. There is an interaction between groundwater flow and heat flow, because the permafrost distribution determines the occurrence of groundwater, but groundwater also contributes to advective heat transport influencing the...
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University of East Anglia
2013
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| Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.614494 |