Presentation is loading. Please wait.

Presentation is loading. Please wait.

Modeling a Spatially Distributed Water Balance Using TOPMODEL

Similar presentations


Presentation on theme: "Modeling a Spatially Distributed Water Balance Using TOPMODEL"— Presentation transcript:

1 Modeling a Spatially Distributed Water Balance Using TOPMODEL
Nduhiu

2 Introduction Spatial Hydrology: Spatial Hydrology is:
“the study of the motion of the earth’s waters and the transport of their constituents using the spatial data structures and functions of a geographic information system” (Maidment, R,D; 1997)

3 Topics of Discussion I will be applying a modified version of TOPMODEL – TOPNET over the Mt. Sterling River Basin, OH. This version, (adapted by David Tarboton), applies the classical lumped TOPMODEL over each sub-watershed in a river network.

4 Topic One TOPMODEL assumptions:
Decreasing hydraulic conductivity with depth, Saturated lateral flow driven by topographic gradient and controlled by depth to water table, Steady state, saturated lateral flow related to equilibrium recharge rate.

5 Project Overview Objectives:
Collect and prepare data to run TOPMODEL over the Mt. Sterling River basin. Calibrate model using multi-objective criteria Compare model output to existing stream flow and soil moisture data (model validation).

6 Model Structure Schematic of model structure

7 Model Inputs Data Requirements: Elevation data (NED) – USGS
Stream flow data (NHD) – USGS Vegetation data (LULC) – USGS Soils data (STATSGO) – Precipitation data (NEXRAD stage III) - Energy forcing data – DMIP (UW)

8 Data Preparation Stream network and elevation data
Prepare DEM (DEM reconditioning); Fill sinks in DEM; Run TauDEM for Stream network and Watershed delineation Verify results.

9 Data Preparation cont. Vegetation Soils In Arc Toolbox convert to grid
In Arc Map, use spatial analyst raster calculator Soils From STATSGO soils data, export coverage to shape file in Arc Toolbox. In Arc map, add this to active data frame. Program fitf (Ross Woods, 2001) is then used to compile soils information for input to TOPMODEL.

10 Data Preparation Precipitation Energy forcing data
NEXRAD Stage III precipitation data OHRFC. Process 12 months of stage III radar data to create a year long file. Run make_raindat.exe to process raw radar data Energy forcing data Two data files created for use with TOPMODEL; i) temper.dat – temperature(ºC), Dew Point temperature, date & time. ii) clipar.dat – Latlong of Basin center, temp. gage elevation, monthly diurnal temp. range.

11 TopSetup Run from within TauDEM and compiles spatial data to be used in TOPMODEL. Model parameters distributed over the basin by subwatershed.


Download ppt "Modeling a Spatially Distributed Water Balance Using TOPMODEL"

Similar presentations


Ads by Google