Variable Infiltration Capacity (VIC) model
Criterion |
Explanation |
General Description |
VIC is a macroscale hydrologic model that balances both surface energy and water over a grid mesh, typically at resolutions ranging from a fraction of a degree to several degrees latitude by longitude. |
Model Domain |
VIC is a land surface model (LSM); the model domain is near-surface atmosphere and land surface hydrological processes. |
Developer |
Currently maintained by University of Washington (UW) Computational Hydrology Group; development over the course of two decades by UW, Princeton University, and collaborators around the globe. |
Hardware computing requirements |
No special hardware requirements; runs on a variety of platforms. |
Code language |
C |
Original application |
Representing land surface processes for general circulation models (GCMs). |
Public/proprietary and cost |
Publicly available source code. |
Physically or empirically based |
Physically based. |
Mathematical methods used |
VIC solves a water or water and energy balance calculation at each grid cell at each user-defined time step. Following this computation, flows are routed over a landscape using the Saint Venant equations. |
Input data requirements |
Meteorological forcing (temperature, precipitation, wind etc.), parameterization of soils, vegetation parameters (landcover, rooting depths, etc.). |
Outputs |
Default outputs are moisture and energy flux (including runoff), snowpack information, and information about frozen soil or lake domains, if applicable. |
Pre-processing and post-processing tools |
Model website has a basic collection of scripts and tools for preparing inputs, plotting results, and converting output to standard netCDF format. |
Representation of uncertainty |
No explicit representation of uncertainty. |
Prevalence |
Widespread use among climate and hydrological applications, with hundreds of published applications in the peer-reviewed literature. There are applications of it across the Western U.S., and the model has been used for runoff modeling as part of the CalAdapt tool for California climate change analyses ( https://cal-adapt.org/tools/streamflow/). |
Ease of use for public entities |
Model setup and use requires specialized training, but VIC has been used for major studies published by the U.S. Bureau of Reclamation (Elsner at al., 2014) and CalAdapt. |
Ease of obtaining information and availability of technical support |
There is an active user group (VIC listserve) |
Source code availability |
Source code is publicly available on Github |
Status of model development |
Model is mature, having been in widespread use since the 1990s. Over this time numerous improvements in the VIC model have been made. The current version of VIC available for download is 4.2. Available on the internet at: http://www.hydro.washington.edu/Lettenmaier/Models/VIC/Development/CurrentVersion.shtml |
Challenges in integration |
Because the VIC model source code is in the public domain, inte gration with other models should be possible, and recent modifications to VIC over the past decade reflect the addition of new processes, such as biogeochemistry and reservoirs. |
References:
Elsner, M., S. Gangopadhyay, T. Pruitt, L. Brekke, N. Mizukami, and M. Clark (2014) How does the Choice of Distributed Meteorological Data Affect Hydrologic Model Calibration and Streamflow Simulations? J. Hydrometeorology. doi:10.1175/JHM-D-13-083.1.
Liang, X., D.P. Lettenmaier, E.F. Wood, and S.J. Burges (1994): A simple hydrologically based model of land surface water and energy fluxes for GSMs. J. Geophysical Research 99(D7): 14,415-14,428.