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An integrated modelling framework of catchment-scale ecohydrological processes: 1. Model description and tests over an energy-limited watershed

Guo-Yue Niu, Claudio Paniconi, Peter Troch, Russell L. Scott, Matej Durcik, Xubin Zeng, Travis Huxman, David C. Goodrich
Ecohydrology 2014 v.7 no.2 pp. 427-439
accuracy, area, calibration, carbon, climate change, dynamics, energy, exhibitions, floods, height, hydrologic cycle, hydrologic models, lakes, land, paper, porous media, prediction, research, rivers, runoff, snow, snowmelt, stream channels, subsurface flow, surface water, testing, topographic slope, watershed hydrology, watersheds, Vermont
The interactions between atmospheric, hydrological, and ecological processes at various spatial and temporal scales are not fully represented inmost ecohydrological models. This first of a two-part paper documents a fully integrated catchment-scale ecohydrological model consisting of a three-dimensional physically based hydrological model and a land surface model. This first part also presents a first application to test the model over an energy-limited catchment (8.4km2) of the Sleepers River watershed in Vermont. The physically based hydrological model (CATchment HYdrology, CATHY) describes three-dimensional subsurface flow in variably saturated porous media and surface routing on hillslopes and in stream channels, whereas the land surface model (LSM), an augmented version of Noah LSM with multiple parameterization schemes (NoahMP), accounts for energy, water, and carbon flux exchanges between various land surface elements and the atmosphere. CATHY and NoahMP are coupled through exchanges of water fluxes and states. In the energy-limited catchment of the Sleepers River watershed, where snowmelt runoff generation is the dominant hydrologic flux, the coupled CATHY/NoahMP model at both 90 and 30-msurface grid resolutions, with minimal calibration, performs well in simulating the observed snow accumulation, and melt and subsequent snowmelt discharge. The Nash–Sutcliffe model efficiency of daily discharge is above 0.82 for both resolutions. The simulation at 90-mresolution shows a marginal improvement over that at 30-m resolution because of more elaborate calibration of model parameters. The coupled CATHY/NoahMP also shows a capability of simulating surface-inundated area and distributed surface water height, although the accuracy of these simulations needs further evaluation. The CATHY/NoahMP model is thus also a potentially useful research tool for predicting flash flood and lake dynamics under climatic change.