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Model Information Inputs Outputs Workflow
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.pdf

Technical Details:
https://research-groups.usask.ca/hydrology/modelling/crhm.php#TechnicalDetails

Other links:
https://www.doi.org/10.1002/hyp.6787
https://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
NameRoleContact Information
John Pomeroy
Main Investigator
john.pomeroy@usask.ca
Logan (Xing) Fang
Model Development
xing.fang@usask.ca
Minimum Input Data
Input DataUnits (if specific or preferred)Additional Information
Temperature
Relative Humidity
Shortwave Radiation In
When unavailable, model can estimate it
Wind Speed
Precipitation
Calibration Data
No formal calibration
Validation Data
SWE, snow depth, albedo, glacier ablation stakes, soil moisture, and streamflow
Model Outputs
OutputsAdditional Information
Mass and energy fluxes for snowpack and glacier, water balance
Processes Modelled
ProcessesAdditional Information
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)
Model Workflow
1. Download station data
2. QA/QC (manual/ using CRHMr package)
3. Filling the gaps in data through interpolation/ imputation using CRHMr
4. Create .obs files of forcing timeseries using CRHMr

See https://research-groups.usask.ca/hydrology/modelling/crhm.php#TechnicalDetails
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