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Snow disappearance timing is dominated by forest effects on snow accumulation in warm winter climates of the Pacific Northwest, United States.
- Published in:
- Hydrological Processes, 2017, v. 31, n. 10, p. 1846, doi. 10.1002/hyp.11144
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- Article
Modeling the effects of climate change projections on streamflow in the Nooksack River basin, Northwest Washington.
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- Hydrological Processes, 2014, v. 28, n. 20, p. 5236, doi. 10.1002/hyp.10012
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- Article
Observations of distributed snow depth and snow duration within diverse forest structures in a maritime mountain watershed.
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- Water Resources Research, 2015, v. 51, n. 11, p. 9353, doi. 10.1002/2015WR017873
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- Article
Evaluating observational methods to quantify snow duration under diverse forest canopies.
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- Water Resources Research, 2015, v. 51, n. 2, p. 1203, doi. 10.1002/2014WR015744
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- Article
Lower forest density enhances snow retention in regions with warmer winters: A global framework developed from plot-scale observations and modeling.
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- Water Resources Research, 2013, v. 49, n. 10, p. 6356, doi. 10.1002/wrcr.20504
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- Article
Development and testing of a snow interceptometer to quantify canopy water storage and interception processes in the rain/snow transition zone of the North Cascades, Washington, USA.
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- Water Resources Research, 2013, v. 49, n. 6, p. 3243, doi. 10.1002/wrcr.20271
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- Article
Ranking Forest Effects on Snow Storage: A Decision Tool for Forest Management.
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- Water Resources Research, 2021, v. 57, n. 10, p. 1, doi. 10.1029/2020WR027926
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- Article