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Status of Incorporating Ice Into NWS Hydraulic Models. Janice Sylvestre NOAA NWS Office of Hydrologic Development In Collaboration with Dr. Steven F. Daly ERDC/CRRL. 2004 Cold Regions Workshop November 15-18, 2004 NWS Training Center Kansas City, MO. Objective.
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Status of Incorporating Ice Into NWS Hydraulic Models Janice Sylvestre NOAA NWS Office of Hydrologic Development In Collaboration with Dr. Steven F. Daly ERDC/CRRL 2004 Cold Regions Workshop November 15-18, 2004 NWS Training Center Kansas City, MO
Objective • Add river ice modeling capability to NWS FLDWAV model based on ERDC/CRREL methodology developed by Dr. Steven Daly. After Daly, 2004
Hydraulic Component: Modifications to account for the presence of ice • Geometric terms in continuity and momentum equations: • Area, Hydraulic Radius, roughness, conveyance • Dynamic modification of geometric “look-up” tables • Representation of the dynamic ice cover extent • Time varying ice roughness After Daly, 2004
FLDWAV Modeling Assumptions • River ice is stationary • Ice information from observations
FLDWAV Input Parameters • For each ice block along the river: • Upstream & downstream location of ice block • Time period of ice block existence • Ice block formation period • Ice thickness • Specific weight of ice • Roughness coefficient for ice • A sensitivity analysis will be done on the parameters to determine how critical they are – which ones can be given default values?
FLDWAV Test Area • River ice effects were observed when calibrating the Susquehanna River system • FLDWAV ice effect enhancement is being tested using this data
March 20, 1999 – August 11, 2000 Affected by ice Verification Flood Period
Ice jam confirmed in Wyoming County on Jan 25th. No other info available.
Jan 5, 2000 Feb 16, 2000
Continued Research • Test FLDWAV capability thoroughly in areas with observed data • Add ice movement option • Determine feasibility of modeling ice cover formation operationally