Snow disappearance timing is dominated by forest effects on snow accumulation in warm winter climates of the Pacific Northwest, United States-Reference-Cited by-同舟云学术

Snow disappearance timing is dominated by forest effects on snow accumulation in warm winter climates of the Pacific Northwest, United States

Published:2017-04-11 Issue:10 Volume:31 Page:1846-1862
ISSN:0885-6087
Container-title:Hydrological Processes
language:en
Short-container-title:Hydrol. Process.

Author:

Dickerson-Lange Susan E.¹²^ORCID,Gersonde Rolf F.³,Hubbart Jason A.⁴,Link Timothy E.⁵,Nolin Anne W.⁶,Perry Gwyneth H.¹,Roth Travis R.⁶,Wayand Nicholas E.¹^ORCID,Lundquist Jessica D.¹

Affiliation:

1. Civil and Environmental Engineering; University of Washington; Seattle WA USA

2. Natural Systems Design; Seattle WA USA

3. Seattle Public Utilities; Seattle WA USA

4. West Virginia University; Morgantown WV USA

5. College of Natural Resources; University of Idaho; Moscow ID USA

6. College of Earth, Ocean, and Atmospheric Sciences; Oregon State University; Corvallis OR USA

Funder

Department of the Interior Northwest Climate Science Center

USDA CSREES NRI

National Science Foundation

U.S. Forest Service

Publisher

Wiley

Subject

Water Science and Technology

Reference97 articles.

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2. Modeling snow accumulation and ablation processes in forested environments;Andreadis;Water Resources Research,2009

3. Quantifying the effects of vegetation structure on snow accumulation and ablation in mixed-conifer forests;Broxton;Ecohydrology,2015

4. Contrasting microclimates among clearcut, edge, and interior of old-growth Douglas-fir forest;Chen;Agricultural and Forest Meteorology,1993

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