GIS Hydro '98

Atmosphere and Soil Water Module

Center for Research in Water Resources, University of Texas at Austin


View an animated map of moisture flow over North America (June, 1991 - July, 1993)

Introduction

This page describes research and educational material related to water balance calculations in the atmosphere and in the soil. Much of the material in this module was also present on the GISHydro97 CD-ROM produced for the 1997 ESRI User's Conference and is just organized in a different way. The highlights of last year's "Atmosphere" and "Soilwater" modules were instructional exercises showing how simple water balance calculations can be made within ArcView GIS. Project reports added this year describe more complex hydrology models run using external codes. ArcView and Arc/Info are used to prepare input data sets for these models.

New materials include (1) a master's thesis written by Kris Martinez to investigate the effects of climate change on the Edward's Aquifer in Central Texas by linking a simple soil water balance model to a recharge and groundwater model, and (2) a term project by Karen Mohr which describes data assimilation for a physically based model that couples the energy, momentum, and water fluxes at the land surface. In these projects, ArcView and/or Arc/Info were used for pre-processing rather than making the actual hydrologic computations because useful FORTRAN and/or C codes already existed and because GIS macro languages are slow when compared with compiled languages like FORTRAN and C.

Atmospheric Water Balance

Definition:
Define a control volume in the atmosphere bounded vertically by the earth's surface and the top of the atmosphere (defined at a specified atmospheric pressure) and horizontally by an arbitrary polygon (i.e. a state or country boundary) extended from the earth's surface to the top of the atmosphere. Use radiosonde data or the output data from a General Circulation Model to compute the inflow and outlfow of atmospheric moisture. If data are also available to compute the change in atmospheric water storage or if the change in atmospheric water storage is assumed negligible, regional runoff can be estimated using this approach. If precipitation data are also used, estimates of regional evaporation can be made.

Soil Water Balance

Definition:
Using a soil layer as the control volume, estimate the amount of water entering and leaving the soil, and keep track of the amount of water stored in the soil. Use parameterization schemes to estimate runoff and evaporation given precipitation and other meteorological data.

Coupled Atmospheric and Soil Water Process Models

Primary Contact


These materials may be used for study, research, and education, but please credit the authors and the Center for Research in Water Resources, The University of Texas at Austin. All commercial rights reserved. Copyright 1998 Center for Research in Water Resources.