Habitat Suitability of Chinook Salmon with morphodynamic modelling
Authors: | |
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Owners: | Manisha Panthi |
Type: | Resource |
Storage: | The size of this resource is 251.1 MB |
Created: | Apr 14, 2022 at 6:27 p.m. |
Last updated: | May 20, 2022 at 8:11 p.m. |
Citation: | See how to cite this resource |
Sharing Status: | Discoverable |
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Abstract
The acute and long-term effect on Chinook salmon during flushing events and natural flood events is estimated using the severity index and habitat suitability index at different locations after the events. Suspended sediment concentration at different locations after flushing events are used for determining the acute effects using severity index whereas, changes in bed composition, depth of water column, and velocity are used to estimate the suitability of the habitat of chinook salmon. Both flushing and natural flood scenarios are recreated using Delft 3D models in the Sandy River downstream of Marmot Dam (removed in 2007).
Subject Keywords
Coverage
Spatial
Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Location of Marmot Dam
Longitude
-122.1323°
Latitude
45.3998°














Leaflet Map data © OpenStreetMap contributors
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The content of this resource is derived from | Major, J. J. et al. Geomorphic response of the sandy river, oregon, to removal of marmot dam. 64 https://pubs.usgs.gov/pp/1792/ (2012) |
This resource is described by | Panthi, M., 2020. Generation and fate of fine sediment from dam flushing. IHE Delft Institute for water Education, https://doi.org/10.25831/ys1q-n736 |
This resource is described by | Lee, A. Modelling salmon spawning habitat response to dam removal. (MSc Thesis, IHE Delft, the Netherlands, 2017). https://doi.org/10.25831/0fc1-gq67 |
How to Cite
Panthi, M., A. A. Lee, S. Dahal (2022). Habitat Suitability of Chinook Salmon with morphodynamic modelling, HydroShare, http://www.hydroshare.org/resource/7674e96fa50b436fba80ba59d566a767
This resource is shared under the Creative Commons Attribution CC BY.
http://creativecommons.org/licenses/by/4.0/
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