2025 CSDMS meeting-052

From CSDMS
Revision as of 21:40, 22 February 2025 by LouisQuigley (talk | contribs) (Created page with "{{CSDMS meeting personal information template-2025 |CSDMS meeting first name=Louis |CSDMS meeting last name=Quigley |CSDMS Pronouns=He/Him |CSDMS meeting institute=University of Illinois Chicago |CSDMS meeting city=Elmwood Park |CSDMS meeting country=United States |CSDMS meeting state=Illinois |CSDMS meeting email address=lquigl3@uic.edu |CSDMS meeting phone=3128601003 }} {{CSDMS meeting select clinics1 2025 |CSDMS_meeting_select_clinics1_2025=3) An Introduction to GRASS...")
(diff) ← Older revision | Latest revision (diff) | Newer revision → (diff)



(if you haven't already)




Log in (or create account for non-CSDMS members)
Forgot username? Search or email:CSDMSweb@colorado.edu


Browse  abstracts


The Depression Connection: Mapping the Interplay between Topographical Depressions and Hydrologic Connectivity


Louis Quigley, (He/Him),University of Illinois Chicago Chicago Illinois, United States. lquigl3@uic.edu



Hydrologic connectivity is dictated by depression structure in a landscape and changes in response to variations in runoff at storm, seasonal, or longer timescales. In this work, we analyzed watershed characteristics across the Illinois, Platte, Arkansas and Susquehanna river watersheds. Utilizing the Fill-Spill-Merge model, our research moves beyond traditional approaches that arbitrarily fill topographic depressions. Instead, it employs Fill-Spill-Merge to simulate depression filling based on selected runoff values using a depression hierarchy data structure for rapid water routing into depressions. This innovative approach offers a nuanced model of water movement and accumulation.

We explored correlations between depression characteristics and watershed landscape features, such as shape, slope, and area. This exploration attempts to demonstrate the impact of topographical attributes on runoff and storage. Our findings indicate consistent relationships between depression fill and other landscape characteristics.

This research provides support to new hydrological models by providing more precise predictions of the impact of depressions on surface hydrologic connectivity. By moving away from conventional depression filling techniques to a more dynamic simulation, this study highlights the importance of technological advancements in improving our understanding of natural phenomena like watershed dynamics with implications for improving water management practices.