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Published on: October 16, 2018
Topographic hydro-conditioning to resolve surface depression storage and ponding in a fully distributed hydrologic
Ai-Ling Jiang1, Kuolin Hsu1, Brett F Sanders2,3
1Center for Hydrometeorology and Remote Sensing, Department of Civil and Environmental Engineering, University of California, Irvine, Irvine, CA, USA.
The new Depression-Preserved DEM Processing (D2P) algorithm effectively captures land surface depressions, crucial for accurate hydrologic modeling. This method improves surface water dynamics and streamflow predictions by preserving natural landscape features in digital elevation models (DEMs).
Area of Science:
- Hydrology and Geomorphology
- Remote Sensing and GIS
- Environmental Modeling
Background:
- Land surface depressions are critical for understanding rainfall-water interactions like ponding, infiltration, and runoff.
- Existing digital elevation models (DEMs) often fail to represent depressions at relevant scales for hydrologic modeling.
- Current DEM processing methods, including those using LiDAR, tend to smooth out depressions, impacting hydrological accuracy.
Purpose of the Study:
- To introduce a novel topographic conditioning workflow, the Depression-Preserved DEM Processing (D2P) algorithm.
- To develop a method that preserves physically meaningful surface depressions for improved hydrologic modeling.
- To enhance the integration of depression dynamics into efficient hydrologic simulations.
Main Methods:
- The D2P algorithm features adaptive screening for depression delineation.
- It incorporates filtering for anthropogenic features like bridges.
- D2P blends river smoothing with depression-resolving functionalities for comprehensive topographic conditioning.
Main Results:
- In a case study, D2P successfully identified 86% of ponds at a 10m DEM resolution.
- Compared to conventional methods, D2P reduced modified DEM cells by 51%, minimizing topographic alteration.
- Hydrologic simulations using D2P-processed DEMs showed improved surface water storage and attenuated, delayed peak streamflow.
Conclusions:
- The D2P algorithm offers a significant advancement in creating DEMs that accurately represent land surface depressions.
- Preserving depressions in DEMs leads to more robust and accurate hydrologic simulations of surface water dynamics.
- D2P facilitates better understanding and modeling of hydrological processes influenced by surface depressions.
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