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Section 1: Model Information
Name (e.g., CRHM)
CRHM
Full Name (e.g., Cold Regions Hydrological Model)
Cold Regions Hydrological Model
Description
CRHM is a (modular) framework which integrates researcher-selected numerical algorithms to model hydrological processes in small- to medium-sized catchments to enable the investigation of hydrological conditions for a wide variety of landscape/climate combinations.
Processes modelled may include:
- blowing snow redistribution
- snow and rain interception by forest canopies
- sublimation
- snowmelt in open and forested environments
- infiltration into frozen and unfrozen soils
- soil moisture storage and movement
- water movement along hillslopes (with and without permafrost)
- actual evaporation and evapotranspiration
- radiation exchange on complex surfaces and through vegetation
- wetland dynamics
- variable contributing area
- groundwater flow
- streamflow hydraulics
- gravitational snow transport
- glacier melt
CRHM incorporates information about distinct landscape elements called Hydrological Response Units (HRUs). HRUs can be linked in process-specific sequences such as blowing snow, overland flow, organic layer subsurface flow, mineral interflow, groundwater flow, and streamflow.
More information about the system is included in C.R. Ellis, J.W. Pomeroy, T. Brown, and J. MacDonald 2010: Simulation of snow accumulation and melt in needleleaf forest environments Hydrology and Earth System Sciences 14: pp. 925–940.
https://research-groups.usask.ca/hydrology/documents/downloads/Ellis_etal_2010_HESS.pdfTechnical Details:
https://research-groups.usask.ca/hydrology/modelling/crhm.php#TechnicalDetailsOther links:
https://www.doi.org/10.1002/hyp.6787https://research-groups.usask.ca/hydrology/modelling/crhm_manual_march_15_2013.pdf (CRHM Manual PDF)
Institution
University of Saskatchewan
Purpose
Models an investigator-selected variety of hydrological processes (see list in Description) in small- to medium-sized catchments.
Contact Persons
John Pomeroy | Main Investigator | john.pomeroy@usask.ca |
Logan (Xing) Fang | Model Development | xing.fang@usask.ca |
Section 2: Inputs
Minimum Input Data
Temperature | | |
Relative Humidity | | |
Shortwave Radiation In | | When unavailable, model can estimate it |
Wind Speed | | |
Precipitation | | |
Optimal Input Data (additional to above minimal input data)
Calibration Data
No formal calibration
Validation Data
SWE, snow depth, albedo, glacier ablation stakes, soil moisture, and streamflow
Section 3: Outputs
Model Outputs
Mass and energy fluxes for snowpack and glacier, water balance | |
Processes Modelled
blowing snow redistribution | |
snow and rain interception by forest canopies | |
sublimation | |
snowmelt in open and forested environments | |
infiltration into frozen and unfrozen soils | |
soil moisture storage and movement | |
water movement along hillslopes (with and without permafrost) | |
actual evaporation and evapotranspiration | |
radiation exchange on complex surfaces and through vegetation | |
wetland dynamics | |
variable contributing area | |
groundwater flow | |
streamflow hydraulics | |
gravitational snow transport | |
glacier melt | |
Spatial Resolution
HRU scale
Temporal Resolution
Sub-daily (ideally hourly)
Strengths and Limitations
-Station data are not readily available for all catchments
-Data may contain long gaps
External and Internal Tools
-R package (CRHMr) for filling data through interpolation
-R package (Reanalysis) for creating CRHM .obs files from gridded data
Source Code Availability
Module code and tools are publicly available (with examples)
Data Sources
Station (ECCC, provincial, research site) and Reanalysis data
File Formats
Timeseries stored in flat ASCII (.obs)