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CE-QUAL-W2 Shasta Modeling
Katherine Clancey Laurel Saito, Ph.D., P.E. Project Update - July ##, 2015 Graduate Program of Hydrologic Sciences University of Nevada, Reno
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Outline Meteorological data for Shasta Lake
Recalibration/verification of CE-QUAL-W2 (W2) Shasta model Reliability of W2 water temperatures Selecting segments to simulate temperature curtains
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Meteorological data Hourly inputs to W2:
air temperature relative humidity wind speed Observed data at Shasta Lake: daily air temperature California Data Exchange Center ( Stations: Shasta Dam-Water Quality (SHD) & Shasta Dam-USBR (SHS) wind direction cloud cover
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Meteorological data Two datasets available for W2 Shasta model:
Redding Municipal Airport data adjusted to Shasta Lake NOAA National Climatic Data Center ( Station: NOAA AWS North American Regional Reanalysis (NARR) data National Centers for Environmental Prediction (NCEP)
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Redding Municipal Airport data adjusted to Shasta Lake
Meteorological data Redding Municipal Airport data adjusted to Shasta Lake Used methods from Saito (1999): Air temperatures: adjustment uses change in elevation between Redding and Shasta Lake (~600 ft difference) Dewpoint: adjustment uses change in elevation Wind speed: adjustment uses regression equation Wind direction: uses Redding data without adjustment Cloud cover: uses Redding data without adjustment
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NARR data Output from numerical weather prediction model
Meteorological data NARR data Output from numerical weather prediction model assimilate data from various sources: upper air soundings hourly and daily meteorology observations satellite Provides all meteorological data needed for W2 Used grid cell data nearest to Shasta Dam Grid resolution is approximately 0.3 degrees (32 km) 3-hour increments
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Air temperature for W2 Shasta model vs SHS station
Meteorological data Air temperature for W2 Shasta model vs SHS station
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Air temperature for W2 Shasta model vs SHD station
Meteorological data Air temperature for W2 Shasta model vs SHD station
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Wind rose Wind is predominantly in the NW direction at Shasta Lake
Meteorological data Wind rose Wind is predominantly in the NW direction at Shasta Lake
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Recalibration of W2 Shasta model
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Verification of W2
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Verification of W2 Water surface elevation (calibration year): January 1995 to December 1995
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Water surface elevation (dry year): January 2001 to September 2002
Verification of W2 Water surface elevation (dry year): January 2001 to September 2002
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Water surface elevation (median year): January 2003 to September 2004
Verification of W2 Water surface elevation (median year): January 2003 to September 2004
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Water surface elevation (wet year): January 2005 to September 2006
Verification of W2 Water surface elevation (wet year): January 2005 to September 2006
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Verification of W2 Water temperature at segment 41 on the McCloud River: January 1995 to December 1995 Elevation (m) Temperature oC
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Verification of W2 Water temperature at segment 53/54 on the Sacramento River: January 1995 to December 1995 Elevation (m) Temperature oC
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Results and conclusion of meteorological data to use for W2
Verification of W2 Results and conclusion of meteorological data to use for W2 Slight differences in performance metrics Pros of using NARR data: Currently being used to predict water temperatures in Sacramento River All meteorological data needed for W2 is in NARR dataset Cons: Meteorological data is for entire grid which covers a large area 3-hour increments – need adjustment
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Results and conclusion of meteorological data to use for W2
Verification of W2 Results and conclusion of meteorological data to use for W2 Pros of using Redding data adjusted to Shasta: Method used for previous W2 model applications. Data available in an hourly timestep Cons: Data adjusted through several different methods Conclusion: Use NARR data for meteorological input to W2
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Reliability of W2 water temperatures
Forebay temperatures Obtained data for 2001 to 2003 from USBR No data available for 2004 to 2006
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2001-2002 Forebay temperatures (dry year)
Reliability of W2 Forebay temperatures (dry year) Elevation (ft) Temperature oC
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2003 Forebay temperatures (median year)
Reliability of W2 2003 Forebay temperatures (median year) Elevation (ft) Temperature oC
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Overall performance metrics
Reliability of W2 Overall performance metrics
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Water temperatures comparisons at the most upstream segments of the W2 model
Reliability of W2 CDEC Station ID: DLT Latitude oN Longitude oW CDEC Station ID: MSS Latitude oN Longitude oW Sacramento River McCloud River CDEC Station ID: PMN Latitude oN Longitude oW Squaw Creek Pit River Shasta Dam Not to scale
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Water temperature (dry year): January 2001 to September 2002
Reliability of W2 Water temperature (dry year): January 2001 to September 2002
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Water temperature (dry year): January 2001 to September 2002
Reliability of W2 Water temperature (dry year): January 2001 to September 2002
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Reliability of W2 Water temperature comparison (median year): January 2003 to September 2004
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Reliability of W2 Water temperature comparison (wet year): January 2005 to September 2006
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Temperature curtains Selecting segments to place temperature curtains (dry year): January 2001 to September 2002 Fall-run Chinook salmon only Fall and spring-run Chinook salmon only All runs No runs Sacramento River McCloud River Squaw Creek Pit River Shasta Dam
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Temperature curtains Selecting segments to place temperature curtains (median year): January 2003 to September 2004 Fall-run Chinook salmon only All runs No runs Sacramento River McCloud River Squaw Creek Pit River Shasta Dam
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Temperature curtains Selecting segments to place temperature curtains (wet year): January 2005 to September 2006 Fall-run Chinook salmon only All runs No runs Sacramento River McCloud River Squaw Creek Pit River Shasta Dam
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References Saito, L. S., 1999, Interdisciplinary modeling at Shasta Lake, Fort Collins: Colorado State University (Ph.D. dissertation) Caldwell, J., 2015, Shasta Modeling Project Coupling CE-QUAL-W2 and RAFT (Draft), MetStat, Inc. QUESTIONS?
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