Template:TEXT BOX LEFT: Difference between revisions

From CSDMS
mNo edit summary
mNo edit summary
Line 1: Line 1:
[[image:TopoFlow_example.png|200px|left|link=]]            
[[image:TopoFlow_example.png|200px|left|link=]]  
TopoFlow 3.0 is a 2D spatially-distributed hydrologic model to simulate different physical processes in a watershed with the goal of predicting how various hydrological variables evolve in time in response to climatic forcings. Time evolutions for single pixels (like hydrographs), collections of user-selected pixels, or entire grids (as animations) are all supported as output options. TopoFlow became in 2010 available as a set of 20+ components that can be used with the CSDMS Modeling Tool (CMT).<br>[[Model highlight|More...]]<br>[mailto:csdmsweb@colorado.edu Nominate a model]
TopoFlow 3.0, mainly developed by Scott Peckham, is a 2D spatially-distributed hydrologic model that simulates different physical processes in a watershed with the goal of predicting how various hydrological variables, like snowmelt, precipitation, evapotranspiration, infiltration, channel/overland flow, shallow subsurface flow and flow diversions evolve in time in response to climatic forcings. Time evolutions for single pixels (like hydrographs), collections of user-selected pixels, or entire grids (as animations) are all supported as output options.
TopoFlow became available in 2010 as a set of over 20 components that can be used with the CSDMS Modeling Tool (CMT). The components have successfully be linked to other models like a valley glacier model, GC2D.<br>[[Model highlight|More...]]<br>[mailto:csdmsweb@colorado.edu Nominate a model]

Revision as of 15:56, 23 November 2010

TopoFlow example.png

TopoFlow 3.0, mainly developed by Scott Peckham, is a 2D spatially-distributed hydrologic model that simulates different physical processes in a watershed with the goal of predicting how various hydrological variables, like snowmelt, precipitation, evapotranspiration, infiltration, channel/overland flow, shallow subsurface flow and flow diversions evolve in time in response to climatic forcings. Time evolutions for single pixels (like hydrographs), collections of user-selected pixels, or entire grids (as animations) are all supported as output options. TopoFlow became available in 2010 as a set of over 20 components that can be used with the CSDMS Modeling Tool (CMT). The components have successfully be linked to other models like a valley glacier model, GC2D.
More...
Nominate a model