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Water 2017, 9(5), 306;

Using Remote Sensing Data to Parameterize Ice Jam Modeling for a Northern Inland Delta

Global Institute for Water Security, Saskatoon, SK S7N 3H5, Canada
Author to whom correspondence should be addressed.
Academic Editor: Hongjie Xie
Received: 27 January 2017 / Revised: 22 April 2017 / Accepted: 23 April 2017 / Published: 27 April 2017
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The Slave River is a northern river in Canada, with ice being an important component of its flow regime for at least half of the year. During the spring breakup period, ice jams and ice-jam flooding can occur in the Slave River Delta, which is of benefit for the replenishment of moisture and sediment required to maintain the ecological integrity of the delta. To better understand the ice jam processes that lead to flooding, as well as the replenishment of the delta, the one-dimensional hydraulic river ice model RIVICE was implemented to simulate and explore ice jam formation in the Slave River Delta. Incoming ice volume, a crucial input parameter for RIVICE, was determined by the novel approach of using MODIS space-born remote sensing imagery. Space-borne and air-borne remote sensing data were used to parameterize the upstream ice volume available for ice jamming. Gauged data was used to complement modeling calibration and validation. HEC-RAS, another one-dimensional hydrodynamic model, was used to determine ice volumes required for equilibrium jams and the upper limit of ice volume that a jam can sustain, as well as being used as a threshold for the volumes estimated by the dynamic ice jam simulations using RIVICE. Parameter sensitivity analysis shows that morphological and hydraulic properties have great impacts on the ice jam length and water depth in the Slave River Delta. View Full-Text
Keywords: river ice; modeling; RIVICE; MODIS; the Slave River Delta river ice; modeling; RIVICE; MODIS; the Slave River Delta

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Zhang, F.; Mosaffa, M.; Chu, T.; Lindenschmidt, K.-E. Using Remote Sensing Data to Parameterize Ice Jam Modeling for a Northern Inland Delta. Water 2017, 9, 306.

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