Dam-induced and natural channel changes in the Saskatchewan River below the E.B. Campbell Dam, Canada-Reference-Cited by-同舟云学术

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Dam-induced and natural channel changes in the Saskatchewan River below the E.B. Campbell Dam, Canada

Published:2016-09 Issue: Volume:269 Page:186-202
ISSN:0169-555X
Container-title:Geomorphology
language:en
Short-container-title:Geomorphology

Author:

Smith Norman D.,Morozova Galina S.,Pérez-Arlucea Marta,Gibling Martin R.

Funder

Natural Sciences and Engineering Research Council of Canada

National Science Foundation

Publisher

Elsevier BV

Subject

Earth-Surface Processes

Reference65 articles.

1. Channel changes in largest Russian rivers: natural and anthropogenic effects;Alexeevsky;Int. J. River Basin Manag.,2013

2. Spatial and temporal patterns of suspended-sediment yield in the Saskatchewan River basin;Ashmore;Can. J. Earth Sci.,1988

3. The Laitaure Delta;Axelsson;Geogr. Ann.,1967

4. Classification of geomorphological effects downstream of dams;Brandt;Catena,2000

5. Changes in river regime after the construction of upstream reservoirs;Chien;Earth Surf. Process. Landf.,1985

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