Hydrologic connectivity at the hillslope scale through intra‐snowpack flow paths during snowmelt-Reference-Cited by-同舟云学术

Hydrologic connectivity at the hillslope scale through intra‐snowpack flow paths during snowmelt

Published:2020-01-06 Issue:7 Volume:34 Page:1616-1629
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Webb Ryan W.¹²³^ORCID,Wigmore Oliver³⁴,Jennings Keith³⁵⁶,Fend Mike⁷,Molotch Noah P.³⁸

Affiliation:

1. Department of Civil, Construction, and Environmental Engineering University of New Mexico Albuquerque New Mexico

2. Center for Water and the Environment University of New Mexico Albuquerque New Mexico

3. Institute of Arctic and Alpine Research University of Colorado Boulder Boulder Colorado

4. Antarctic Research Centre Victoria University of Wellington Wellington New Zealand

5. Department of Geography University of Nevada Reno Nevada

6. Division of Hydrologic Sciences Desert Research Institute Reno Nevada

7. UNAVCO Boulder Colorado

8. Department of Geography University of Colorado Boulder Boulder Colorado

Funder

Division of Earth Sciences

Division of Environmental Biology

National Science Foundation

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.13686

Reference76 articles.

1. Anderson S. &Rager D.(2019).CZO dataset: Gordon Gulch: Lower – air temperature meorology (2012–2019)—North‐facing meteorological tower (GGL_NF_Met).http://criticalzone.org/boulder/data/dataset/2888/.

2. Tracer release in melting snow: Diurnal and seasonal patterns

3. Mountain hydrology of the western United States

4. Snowmelt rate dictates streamflow

5. A physical SNOWPACK model for the Swiss avalanche warning

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