Hyperpycnal flows control the persistence and flushing of hypoxic high conductivity bottom water in a High Arctic lake

In the deepest portions of many lakes, zones of high conductivity bottom water (HCBW) depleted in dissolved oxygen (DO) are present. HCBW and DO are important for determining benthic diversity and abundance, nutrients and contaminant cycling, and understanding the long-term evolution of lakes. We in...

Full description

Bibliographic Details
Main Authors: Lewis, Ted, Lamoureux, Scott F., Normandeau, Alexandre, Dugan, Hilary A
Format: Article in Journal/Newspaper
Language:unknown
Published: NRC Research Press (a division of Canadian Science Publishing) 2017
Subjects:
Online Access:http://hdl.handle.net/1807/81139
http://www.nrcresearchpress.com/doi/abs/10.1139/AS-2017-0022