Forest impacts on snow accumulation and melt in a semi-arid mountain environment

Snowmelt is complex under heterogeneous forest cover due to spatially variable snow surface energy and mass balances and snow accumulation. Forest canopies influence the under-canopy snowpack net total radiation energy balance by enhancing longwave radiation, shading the surface from shortwave radia...

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Main Authors: Maggi Kraft, James P. McNamara, Hans-Peter Marshall, Nancy F. Glenn
Format: Article
Language:English
Published: Frontiers Media S.A. 2022-11-01
Series:Frontiers in Water
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/frwa.2022.1004123/full
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author Maggi Kraft
James P. McNamara
Hans-Peter Marshall
Nancy F. Glenn
author_facet Maggi Kraft
James P. McNamara
Hans-Peter Marshall
Nancy F. Glenn
author_sort Maggi Kraft
collection DOAJ
description Snowmelt is complex under heterogeneous forest cover due to spatially variable snow surface energy and mass balances and snow accumulation. Forest canopies influence the under-canopy snowpack net total radiation energy balance by enhancing longwave radiation, shading the surface from shortwave radiation, in addition to intercepting snow, and protecting the snow surface from the wind. Despite the importance of predicting snowmelt timing for water resources, there are limited observations of snowmelt timing in heterogeneous forest cover across the Intermountain West. This research seeks to evaluate the processes that control snowmelt timing and magnitude at two paired forested and open sites in semi-arid southern Idaho, USA. Snow accumulation, snowmelt, and snow energy balance components were measured at a marginal snowpack and seasonal snowpack location in the forest, sparse vegetation, forest edge, and open environments. At both locations, the snow disappeared either later in the forest or relatively uniformly in the open and forest. At the upper elevation location, a later peak in maximum snow depth resulted in more variable snow disappearance timing between the open and forest sites with later snow disappearance in the forest. Snow disappearance timing at the marginal snowpack location was controlled by the magnitude and duration of a late season storm increasing snow depth variability and reducing the shortwave radiation energy input. Here, a shorter duration spring storm resulted in more uniform snowmelt in the forest and open. At both locations, the low-density forests shaded the snow surface into the melt period slowing the melt rate in the forest. However, the forest site had less cold content to overcome before melting started, partially canceling out the forest shading effect. Our results highlight the regional similarities and differences of snow surface energy balance controls on the timing and duration of snowmelt.
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spelling doaj.art-48b8ede066144de4a70a7ac8af8c331b2022-12-22T04:36:25ZengFrontiers Media S.A.Frontiers in Water2624-93752022-11-01410.3389/frwa.2022.10041231004123Forest impacts on snow accumulation and melt in a semi-arid mountain environmentMaggi KraftJames P. McNamaraHans-Peter MarshallNancy F. GlennSnowmelt is complex under heterogeneous forest cover due to spatially variable snow surface energy and mass balances and snow accumulation. Forest canopies influence the under-canopy snowpack net total radiation energy balance by enhancing longwave radiation, shading the surface from shortwave radiation, in addition to intercepting snow, and protecting the snow surface from the wind. Despite the importance of predicting snowmelt timing for water resources, there are limited observations of snowmelt timing in heterogeneous forest cover across the Intermountain West. This research seeks to evaluate the processes that control snowmelt timing and magnitude at two paired forested and open sites in semi-arid southern Idaho, USA. Snow accumulation, snowmelt, and snow energy balance components were measured at a marginal snowpack and seasonal snowpack location in the forest, sparse vegetation, forest edge, and open environments. At both locations, the snow disappeared either later in the forest or relatively uniformly in the open and forest. At the upper elevation location, a later peak in maximum snow depth resulted in more variable snow disappearance timing between the open and forest sites with later snow disappearance in the forest. Snow disappearance timing at the marginal snowpack location was controlled by the magnitude and duration of a late season storm increasing snow depth variability and reducing the shortwave radiation energy input. Here, a shorter duration spring storm resulted in more uniform snowmelt in the forest and open. At both locations, the low-density forests shaded the snow surface into the melt period slowing the melt rate in the forest. However, the forest site had less cold content to overcome before melting started, partially canceling out the forest shading effect. Our results highlight the regional similarities and differences of snow surface energy balance controls on the timing and duration of snowmelt.https://www.frontiersin.org/articles/10.3389/frwa.2022.1004123/fullsnowmeltsnow-vegetation interactionssnow accumulationsemi-aridsnow ablationenergy balance
spellingShingle Maggi Kraft
James P. McNamara
Hans-Peter Marshall
Nancy F. Glenn
Forest impacts on snow accumulation and melt in a semi-arid mountain environment
Frontiers in Water
snowmelt
snow-vegetation interactions
snow accumulation
semi-arid
snow ablation
energy balance
title Forest impacts on snow accumulation and melt in a semi-arid mountain environment
title_full Forest impacts on snow accumulation and melt in a semi-arid mountain environment
title_fullStr Forest impacts on snow accumulation and melt in a semi-arid mountain environment
title_full_unstemmed Forest impacts on snow accumulation and melt in a semi-arid mountain environment
title_short Forest impacts on snow accumulation and melt in a semi-arid mountain environment
title_sort forest impacts on snow accumulation and melt in a semi arid mountain environment
topic snowmelt
snow-vegetation interactions
snow accumulation
semi-arid
snow ablation
energy balance
url https://www.frontiersin.org/articles/10.3389/frwa.2022.1004123/full
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AT jamespmcnamara forestimpactsonsnowaccumulationandmeltinasemiaridmountainenvironment
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AT nancyfglenn forestimpactsonsnowaccumulationandmeltinasemiaridmountainenvironment