2023 CSDMS meeting-022: Difference between revisions
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{{CSDMS meeting abstract title temp2023 | {{CSDMS meeting abstract title temp2023 | ||
|CSDMS meeting abstract title= | |CSDMS meeting abstract title=Topographic depressions and hydrologic connectivity in the United States | ||
|Working_group_member_WG_FRG=Terrestrial Working Group, Hydrology Focus Research Group | |Working_group_member_WG_FRG=Terrestrial Working Group, Hydrology Focus Research Group | ||
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{{CSDMS meeting abstract template 2023 | {{CSDMS meeting abstract template 2023 | ||
|CSDMS meeting abstract= | |CSDMS meeting abstract=Hydrologic connectivity can change as climate changes, seasonally, or even after a single rain event. Here, I assess the depression structure of the topography of the United States and determine its capacity to hold surface water in lakes. I provide results from a simulation indicating the pre-industrial water level in these depressions and the resulting degree of hydrologic connectivity. I then share results from a series of experimental simulations to modify water levels and the resulting hydrologic connectivity across the country. | ||
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Latest revision as of 15:55, 3 April 2023
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Topographic depressions and hydrologic connectivity in the United States
Kerry Callaghan,
University of Illinois Chicago Chicago Illinois, United States. kerryc@uic.edu
Hydrologic connectivity can change as climate changes, seasonally, or even after a single rain event. Here, I assess the depression structure of the topography of the United States and determine its capacity to hold surface water in lakes. I provide results from a simulation indicating the pre-industrial water level in these depressions and the resulting degree of hydrologic connectivity. I then share results from a series of experimental simulations to modify water levels and the resulting hydrologic connectivity across the country.
