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East Fork White River near Seymour, IN, 2017 high-water marks

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Type:	Resource
Storage:	The size of this resource is 7.8 KB
Created:	Nov 11, 2020 at 9:31 p.m.
Last updated:	Jan 29, 2021 at 9:39 p.m.
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Sharing Status:	Public
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Abstract

These RTK GPS survey points were collected on 3 March 2017.

The "Code" attribute refers to the following:

"DEBRIS" -- the location of some sort of debris line (corn stalks, leaves, wood) that indicated high water in the past that we believe was tied to a flooding event earlier that January.
"WSEL" -- water-surface elevation at the time of the survey. This marks the extent/location of water on the floodplain at the time of survey.
"ICE" -- the location of ice, the water-surface was higher the previous day and had been receding over night, at some point the water froze to ice, and this marks the location of the water surface when some of the water froze to ice. Not all ice had melted by the morning of the survey.
"MUD" -- locations where the ground was wet and likely had been inundated recently, perhaps marking a high point of flooding from the most recent storm(?)

For the January 2017 high water-marks used by
Czuba, J.A., S.R. David, D.A. Edmonds, and A.S. Ward (2019), Dynamics of surface-water connectivity in a low-gradient meandering river floodplain, Water Resources Research, 55(3), 1849-1870, https://doi.org/10.1029/2018WR023527
only the "DEBRIS" points were used.

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Coverage

Spatial

Coordinate System/Geographic Projection:

WGS 84 EPSG:4326

Coordinate Units:

Decimal degrees

North Latitude

39.1445°

East Longitude

-85.7981°

South Latitude

38.8821°

West Longitude

-86.0852°

Content

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Related Resources

This resource is referenced by	Czuba, J.A., S.R. David, D.A. Edmonds, and A.S. Ward (2019), Dynamics of surface-water connectivity in a low-gradient meandering river floodplain, Water Resources Research, 55(3), 1849-1870, https://doi.org/10.1029/2018WR023527
This resource is referenced by	David, S.R., J.A. Czuba, D.A. Edmonds, and A.S. Ward (in review), The influence of floodplain channel connectivity on flood hydrodynamics.
This resource is referenced by	Sumaiya, S., J.A. Czuba, J.T. Schubert, S.R. David, G.H. Johnston, and D.A. Edmonds (in review), Sediment transport potential in a hydraulically connected river and floodplain-channel system

This resource belongs to the following collections:

Title	Owners	Sharing Status	My Permission
East Fork White River near Seymour, IN	Jonathan Czuba	Public & Shareable	Open Access

How to Cite

Czuba, J. (2021). East Fork White River near Seymour, IN, 2017 high-water marks, HydroShare, http://www.hydroshare.org/resource/ab4bae58148d4b45b43d675ccea72778

This resource is shared under the Creative Commons Attribution CC BY.

http://creativecommons.org/licenses/by/4.0/

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