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This study compares NARR model's groundwater recharge simulation with UNAT-H model, finding discrepancies in recharge estimates. Utilizing various data conversion methods and soil hydrology analyses, the research aims to propose modifications for better vadose-zone moisture transport modeling.
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How well does the NARR data simulate recharge to groundwater? Lindsey Gulden Surface Water Hydrology April 26, 2005
Point of comparison for NARR recharge: Keese et al., 2005 • Results: average annual recharge 1961-1990 • 1-D recharge simulations • Unsaturated-zone model (UNSAT-H) Keese et al., 2005
Methods… Evaporation 144 GRIB Files containing NARR monthly data (baseflow, precip., surface runoff, and evaporation) Myriaddata conversion steps Baseflow FORTRAN! VBA! Precipitation NCL! Blood, sweat tears ArcGIS grids, polygons
NARR-Noah average percent of precipitation that becomes recharge
Preliminary conclusion • “Recharge” calculated by NARR is approximately half that calculated by UNSAT-H • Baseflow is moderately correlated between NARR and UNSAT-H
Many (~100), variably spaced layers Precise Ψ, K calculations based on soil texture Implicit surface runoff 3-dimensional variation in soil texture 4 soil layers Coarse calculations of Ψ, K Explicit surface runoff scheme Homogeneous soil across each 32-km grid cell Soil hydrology of Noah LSM Keese et al.’s UNSAT-H
Next steps . . . • Recalculate Keese et al.’s recharge for the overlapping time period (’79-’90) • Continue to analyze reasons for discrepancy • Propose modifications to Noah LSM that will improve vadose-zone moisture transport