Cherie Westbrook, John Pomeroy, Xing Fang, Kevin Shook ......Snow redistribution to channels Spring...
Transcript of Cherie Westbrook, John Pomeroy, Xing Fang, Kevin Shook ......Snow redistribution to channels Spring...
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Cherie Westbrook, John Pomeroy, Xing Fang, Kevin Shook, Tom Brown, Xulin Guo, Adam Minke, Nicole Seitz, Nathalie Brunet
Centre for Hydrology (www.usask.ca/hydrology)[email protected]
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• First – what is distinctive about our hydrology?
• Second – examine available approaches and technical options
• Third – recognize we have a unique hydrography and hydrology. Then, do it right.
• Fourth – recognize prairie hydrology rapidly changes and adapt
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Interflow
Runoff
SnowfallSublimation
Blowing SnowEvaporation
Evapo-transpirationRainfall
Snowmelt
Infiltration Frozen Ground
Saturated Porous Media Flow
Bergeron Process
Ice
Wetland storage
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Snow redistribution to channels
Spring melt and runoff
Water storage in wetlands
Dry non-contributing areas to runoff
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Wetland 1
Wetland 2
sill
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Lack of groundwater connections in this landscape – heavy tills
The ‘fill and spill’ hypothesis
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Smith Creek Watershed, Spring 2011(courtesy of DUC)
Lack of inventory of wetland extent and loss in the Canadian Prairies
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1958 2009
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Smith Creek, SaskatchewanDrainage area ~ 450 km2
No baseflow from groundwater (?)
Hydrological drought can be viewed as the absence of prairie runoff……
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• The Hydrological Cycle is manifested with strong regional variations around the world.
• Hydrologists have created a vast number of models (assumptions) to describe some aspects of this cycle.
• It is generally not necessary or likely that one hydrological model approach is applicable to all environments, scales or predictive interest
• Physically-based models attempt to describe reality faithfully (but do not completely succeed)
• Hydrological models predict most successfully in catchments near where they were derived
• Logical selection and design of model strategy, structure and their inherent assumptions are governed by local problems and local hydrology – this is not just parameter selection.
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• Frustration with adding process algorithms to existing hydrological models that do not have cold regions features
• Frustration with trying to fit inappropriate structure of existing models to basins – all water does not drain to the stream!
• Frustration with inability to fit gridded or other conceptual spatial representations to reality – water flows in drainage basins, not grid cells.
• Frustration with models that only focus on streamflow response to precipitation – soil moisture or wetland storage level are equally interesting to some.
• Frustration with attempts to teach modelling to young hydrologists using older computer languages, no user interface, limited documentation of models - Fortran belongs in a museum.
• Frustration with the lack of a graphical system to evaluate model inputs and outputs
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• Need a physical basis to calculate the effects of changing climate, land use, wetland drainage
• Need to incorporate key prairie hydrology processes: snow redistribution, frozen soils, spring runoff, wetland fill and spill, non-contributing areas
• Frustration that hydrological models developed elsewhere do not have these features and fail in this environment
• Streamflow calibration does not provide information on basin non-contributing areas and is not suitable for change analysis
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• Modular – purpose built from C++ modules
• Modules based upon +45 years of prairie hydrology research at Univ. of Saskatchewan
• No provision for calibration or optimization, parameters set by knowledge
• Hydrological Response Unit (HRU)
• HRUs assumed to represent one response type, basis for coupled energy and mass balance
• HRUs connected aerodynamically for blowing snow and via dynamic drainage networks for streamflow
• Incorporate wetlands directly using fill and spill algorithm
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• Data from multiple sites• Interpolation to the HRUs
• Infiltration into soils (frozen and unfrozen)• Snowmelt (open & forest)• Radiation – level, slopes• Wind speed variation – complex topo• Evapotranspiration• Blowing snow transport• Interception (snow & rain)• Sublimation (dynamic & static)• Soil moisture balance• Pond/depression storage• Surface runoff• Sub-surface runoff• Routing (hillslope & channel)
DATA ASSIMILATION
SPATIAL PARAMETERS
PROCESSES
• Basin and HRU parameters are set (area, latitude, elevation, ground slope, aspect)
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• A HRU is a spatial unit in the basin that has 3 groups of attributes
• biophysical structure - soils, vegetation, drainage, slope, elevation, area (determine from GIS, maps)
• hydrological state – snow water equivalent, snow internal energy, intercepted snow load, soil moisture, depressionalstorage, lake storage, water table (track using model)
• hydrological flux - snow transport, sublimation, evaporation, melt discharge, infiltration, drainage, runoff. Fluxes are determined using fluxes from adjacent HRU and so depend on location in a flow sequence.
• HRUs need not be spatially continuous but must have some approx. geographical location or location in a hydrological flow sequence
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Sequential HRU –landscape connectivity
Grouped HRU or Tile –must drain to stream
HRU 1
HRU 2
HRU 3
OUTFLOW
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Ifpond
Snowmelt Rainfall
Snowmelt Infiltration
Rainfall Infiltration
Recharge Zone
Soil Column
Evapotranspiration
SubsurfaceDischarge
Groundwater GroundwaterDischarge
Ifsoil column
is full
Yes
No
No Yes
Saturated OverlandFlow = 0
SaturatedOverland
Flow
Ifdepression
NoRunoff
YesRunoff to
Depression
Depression
Evaporation
GroundwaterGroundwaterDischarge
SubsurfaceDischarge
Ifdepression
is full
NoNo fill-and-spill
Yesfill-and-spill
Snowmelt Rainfall
Snowmelt Infiltration
Rainfall Infiltration
Wetland Pond
Evaporation
Groundwater
Ifpond is full
No fill-and-spill
No
Yesfill-and-spill
SubsurfaceDischarge
GroundwaterDischarge
Surface Runoff
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• Calculated depression storage using simplified pond volume-depth-area method (see Minke et al. 2010, Wetlands)
Original 10-m LiDAR DEM Filled depressionless10-m LiDAR DEM
‘Cut-fill’ output
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Note, blowing snow aerodynamic routing from smooth to rough land covers
Amongst HRU in a Representative Basin
Amongst Representative Basins
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(for details see Fang et al. 2010, HESS)
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Rapidly changing climate, adaptive human management, etc.
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May 10, 2011
May 11, 2011after 35 mm of rain
Stream in central part of Smith Creek Research
Watershed
Groundwater contributions to streamflow after series of
very wet years?
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Spring 2011Spring 2005courtesy of Don Werle
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Smith Creek Watershed(Spring 2011)
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• Newly established beaver bounties in SK (2011) and MB (2012)
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Lot of process field work has been done at various sites• Stream water quality• Water quality of wetland drainage (see Brunet and Westbrook 2012, AEE)• Water quality along fill and spill sequences
• How to best incorporate water quality into CHRM?
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• Appropriate models must be selected for Canadian Prairie hydrological conditions
• This has meant a +40 year research programme at the University of Saskatchewan
• The resulting CHRM model platform has key components of prairie hydrology → some more are needed
• Applications in wetland dominated basins are leading to information to guide management practices
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• Prairie Habitat Joint Venture Committee• Saskatchewan Watershed Authority• Manitoba Water Stewardship• Ducks Unlimited Canada• Agriculture and Agri‐food Canada, PFRA• Saskatchewan Ministry of Agriculture• Environment Canada (WSC, PPWB)• Smith Creek Watershed Association and landowners• NSERC• DRI, IP3, CRC, Univ. of Saskatchewan