|Titre||Monitoring the freeze-up and ice cover progression of the Slave River|
|Auteur||Das, A; Sagin, J; Van der Sanden, J; Evans, E; McKay, H; Lindenschmidt, K -E|
|Source||Canadian Journal of Civil Engineering vol. 42, no. 9, 2015 p. 609-621, https://doi.org/10.1139/cjce-2014-0286|
|Séries alt.||Ressources naturelles Canada, Contribution externe 20181793|
|Éditeur||Éditions Sciences Canada|
|Document||publication en série|
|Media||papier; en ligne; numérique|
|Programme||Centre canadien de télédétection Directives cartographiques des inondations|
|Résumé||(disponible en anglais seulement)|
River ice is an important component to maintain traditional and cultural lifestyles for the peoples along the Slave River in the Northwest Territories. During
the winter a stable ice cover provides a vital transportation link to hunting, trapping, and fishing areas along the river. However, little was known about the Slave River ice cover characteristics and behaviour during the freeze-up and ice cover
progression period. RADARSAT-2 satellite and time-lapse camera imagery were used in this study to document the different types of ice and understand the mechanisms of ice cover formation progression along the river during the course of winter.
Time-lapse images were analyzed to observe the frazil ice generation and patterns of stable ice cover formation of the Slave River near Fort Smith during freeze-up. RADARSAT-2 images acquired from the Slave River Delta areas captured ice cover
flooding due to higher river flows in mid-winter. Field surveys along the river provided insights about the ice cover growth in various sections along the river. Air pockets and layers under the ice cover were also detected during the ice surveys.
The variation of water flows during the winter has a great impact on the Slave River ice regime. Increases in discharge cause the ice cover to crack or dislodge from the river banks leading to water seeping onto the ice and flooding it, which has
implications for muskrat and beaver populations.