Checking for non-preferred file/folder path names (may take a long time depending on the number of files/folders) ...

Supporting Information: Karst Hydrologic Memory Supplements Streamflow during Dry Periods in Snow-Dominated, Mountainous Watersheds


Authors:
Owners: This resource does not have an owner who is an active HydroShare user. Contact CUAHSI (help@cuahsi.org) to determine if accessing this resource is possible.
Type: Resource
Storage: The size of this resource is 510.6 MB
Created: May 24, 2024 at 5:34 p.m.
Last updated: May 24, 2024 at 5:54 p.m.
Citation: See how to cite this resource
Sharing Status: Discoverable
Views: 280
Downloads: 0
+1 Votes: Be the first one to 
 this.
Comments: No comments (yet)

Abstract

This document provides an overview of the accompanying data files used in the production of the manuscript entitled "Karst Hydrologic Memory Supplements Streamflow during Dry Periods in Snow-Dominated, Mountainous Watersheds".

Subject Keywords

Coverage

Spatial

Coordinate System/Geographic Projection:
WGS 84 EPSG:4326
Coordinate Units:
Decimal degrees
Place/Area Name:
Utah, Idaho
North Latitude
42.5026°
East Longitude
-109.6930°
South Latitude
40.2692°
West Longitude
-112.3956°

Content

  You do not have permission to see these content files. Please contact an Owner if you wish to obtain access.

Credits

Funding Agencies

This resource was created using funding from the following sources:
Agency Name Award Title Award Number
National Science Foundation 2043363
National Science Foundation 2044051
National Science Foundation 2043150

How to Cite

Tennant, H., B. Neilson, D. S. Hill, D. L. Newell, J. P. Evans, T. Xu, S. Choi, J. P. McNamara, N. Ashmead (2024). Supporting Information: Karst Hydrologic Memory Supplements Streamflow during Dry Periods in Snow-Dominated, Mountainous Watersheds, HydroShare, http://www.hydroshare.org/resource/52aaba03276c4de4943c396fee2363f2

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

http://creativecommons.org/licenses/by/4.0/
CC-BY

Comments

There are currently no comments

New Comment

required