MODELING WATER-BALANCE WITH THE ERHYM MODEL ON SOUTH TEXAS RANGELANDS

Citation
Ma. Weltz et Wh. Blackburn, MODELING WATER-BALANCE WITH THE ERHYM MODEL ON SOUTH TEXAS RANGELANDS, Water resources bulletin, 29(3), 1993, pp. 461-474
Citations number
44
Categorie Soggetti
Geosciences, Interdisciplinary","Water Resources","Engineering, Civil
Journal title
ISSN journal
00431370
Volume
29
Issue
3
Year of publication
1993
Pages
461 - 474
Database
ISI
SICI code
0043-1370(1993)29:3<461:MWWTEM>2.0.ZU;2-S
Abstract
Understanding the hydrologic processes of rangeland, plant communities is essential to determine if water augmentation through shrub managem ent is feasible. Vegetation manipulation studies are costly, difficult to accurately replicate, and often require more than 10 years to dete rmine treatment effect on the water budget. If properly applied, hydro logic simulation models are an attractive alternative for assessing ve getation manipulation practices. The ERHYM-II model was evaluated to d etermine if it was capable of simulating the water balance for honey m esquite shrub clusters, grass interspaces, and bare soil in south Texa s. The simulated water budget was within 2 percent of the measured eva potranspiration for the shrub clusters and grass interspaces. The mode l underestimated the number of runoff events and overestimated runoff volume for the grass interspace and shrub clusters. Simulated runoff w as overestimated by approximately twofold for the grass interspace and threefold for the shrub clusters. Although simulated runoff was subst antially overestimated, observed and simulated runoff only accounted f or 3 to 6 percent of annual rainfall for the grass and shrub dominated areas, respectively. Simulated evapotranspiration was underestimated by 18 percent and soil water content was overestimated by 82 percent f or the bare soil. The model underestimated evapotranspiration for the bare soil as a result of restricting evaporative losses to the first s oil layer. Based on our analysis, the ERHYM-II model has the potential for simulating the annual water balance for semiarid rangeland plant communities where runoff and deep drainage are limited components of t he water balance.