Future land cover and climate may drive decreases in snow wind‐scour and transpiration, increasing streamflow at a Colorado, USA headwater catchment-Reference-Cited by-同舟云学术

Future land cover and climate may drive decreases in snow wind‐scour and transpiration, increasing streamflow at a Colorado, USA headwater catchment

Published:2021-11 Issue:11 Volume:35 Page:
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrological Processes

Author:

Barnhart Theodore B.¹²^ORCID,Vukomanovic Jelena³^ORCID,Bourgeron Patrick⁴^ORCID,Molotch Noah P.¹^ORCID

Affiliation:

1. Institute of Arctic and Alpine Research, Center for Water, Energy, Sustainability, and Technology, Department of Geography University of Colorado Boulder Colorado USA

2. Now at U.S. Geological Survey Helena Montana USA

3. Center for Geospatial Analytics, Department of Parks, Recreation and Tourism Management North Carolina State University Raleigh North Carolina USA

4. Institute of Arctic and Alpine Research, Center for the American West University of Colorado Boulder Colorado USA

Funder

National Science Foundation

U.S. Department of Agriculture

Publisher

Wiley

Subject

Water Science and Technology

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/hyp.14416

Reference79 articles.

1. Anderson S. P. Qinghua G. &Parish E. G.(2012).Snow‐on and snow‐off Lidar point cloud data and digital elevation models for study of topography snow ecosystems and environmental change at Boulder Creek Critical Zone Observatory Colorado. Boulder Creek CZO INSTAAR University of Colorado at Boulder.https://doi.org/10.5069/G93R0QR0

2. Mountain hydrology of the western United States

3. The Counteracting Effects of Snowmelt Rate and Timing on Runoff

4. Snowmelt rate dictates streamflow

5. Effect of Tree-to-Shrub Type Conversion in Lower Montane Forests of the Sierra Nevada (USA) on Streamflow

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