The Impact of Variable Horizon Shade on the Growing Season Energy Budget of a Subalpine Headwater Wetland
Surface energy budgets are important to the ecohydrology of complex terrain, where land surfaces cycle in and out of shadows creating distinct microclimates. Shading in such environments can help regulate downstream flow over the course of a growing season, but our knowledge on how shadows impact th...
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2021
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oai:doaj.org-article:343fe3e1f9dd4bda8d5992b0ff54d61a2021-11-25T16:45:13ZThe Impact of Variable Horizon Shade on the Growing Season Energy Budget of a Subalpine Headwater Wetland10.3390/atmos121114732073-4433https://doaj.org/article/343fe3e1f9dd4bda8d5992b0ff54d61a2021-11-01T00:00:00Zhttps://www.mdpi.com/2073-4433/12/11/1473https://doaj.org/toc/2073-4433Surface energy budgets are important to the ecohydrology of complex terrain, where land surfaces cycle in and out of shadows creating distinct microclimates. Shading in such environments can help regulate downstream flow over the course of a growing season, but our knowledge on how shadows impact the energy budget and consequently ecohydrology in montane ecosystems is very limited. We investigated the influence of horizon shade on the surface energy fluxes of a subalpine headwater wetland in the Canadian Rocky Mountains during the growing season. During the study, surface insolation decreased by 60% (32% due to evolving horizon shade and 28% from seasonality). The influence of shade on the energy budget varied between two distinct periods: (1) Stable Shade, when horizon shade was constant and reduced sunlight by 2 h per day; and (2) Dynamic Shade, when shade increased and reduced sunlight by 0.18 h more each day, equivalent to a 13% reduction in incoming shortwave radiation and 16% in net radiation. Latent heat flux, the dominant energy flux at our site, varied temporally because of changes in incoming radiation, atmospheric demand, soil moisture and shade. Horizon shade controlled soil moisture at our site by prolonging snowmelt and reducing evapotranspiration in the late growing season, resulting in increased water storage capacity compared to other mountain wetlands. With the mounting risk of climate-change-driven severe spring flooding and late season droughts downstream of mountain headwaters, shaded subalpine wetlands provide important ecohydrological and mitigation services that are worthy of further study and mapping. This will help us better understand and protect mountain and prairie water resources.Dylan M. HrachRichard M. PetroneBrandon Van HuizenAdam GreenMyroslava KhomikMDPI AGarticlehorizon shadesolar radiationenergy budgetCanadian Rocky Mountainssubalpine wetlandlatent heat fluxMeteorology. ClimatologyQC851-999ENAtmosphere, Vol 12, Iss 1473, p 1473 (2021) |
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horizon shade solar radiation energy budget Canadian Rocky Mountains subalpine wetland latent heat flux Meteorology. Climatology QC851-999 |
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horizon shade solar radiation energy budget Canadian Rocky Mountains subalpine wetland latent heat flux Meteorology. Climatology QC851-999 Dylan M. Hrach Richard M. Petrone Brandon Van Huizen Adam Green Myroslava Khomik The Impact of Variable Horizon Shade on the Growing Season Energy Budget of a Subalpine Headwater Wetland |
description |
Surface energy budgets are important to the ecohydrology of complex terrain, where land surfaces cycle in and out of shadows creating distinct microclimates. Shading in such environments can help regulate downstream flow over the course of a growing season, but our knowledge on how shadows impact the energy budget and consequently ecohydrology in montane ecosystems is very limited. We investigated the influence of horizon shade on the surface energy fluxes of a subalpine headwater wetland in the Canadian Rocky Mountains during the growing season. During the study, surface insolation decreased by 60% (32% due to evolving horizon shade and 28% from seasonality). The influence of shade on the energy budget varied between two distinct periods: (1) Stable Shade, when horizon shade was constant and reduced sunlight by 2 h per day; and (2) Dynamic Shade, when shade increased and reduced sunlight by 0.18 h more each day, equivalent to a 13% reduction in incoming shortwave radiation and 16% in net radiation. Latent heat flux, the dominant energy flux at our site, varied temporally because of changes in incoming radiation, atmospheric demand, soil moisture and shade. Horizon shade controlled soil moisture at our site by prolonging snowmelt and reducing evapotranspiration in the late growing season, resulting in increased water storage capacity compared to other mountain wetlands. With the mounting risk of climate-change-driven severe spring flooding and late season droughts downstream of mountain headwaters, shaded subalpine wetlands provide important ecohydrological and mitigation services that are worthy of further study and mapping. This will help us better understand and protect mountain and prairie water resources. |
format |
article |
author |
Dylan M. Hrach Richard M. Petrone Brandon Van Huizen Adam Green Myroslava Khomik |
author_facet |
Dylan M. Hrach Richard M. Petrone Brandon Van Huizen Adam Green Myroslava Khomik |
author_sort |
Dylan M. Hrach |
title |
The Impact of Variable Horizon Shade on the Growing Season Energy Budget of a Subalpine Headwater Wetland |
title_short |
The Impact of Variable Horizon Shade on the Growing Season Energy Budget of a Subalpine Headwater Wetland |
title_full |
The Impact of Variable Horizon Shade on the Growing Season Energy Budget of a Subalpine Headwater Wetland |
title_fullStr |
The Impact of Variable Horizon Shade on the Growing Season Energy Budget of a Subalpine Headwater Wetland |
title_full_unstemmed |
The Impact of Variable Horizon Shade on the Growing Season Energy Budget of a Subalpine Headwater Wetland |
title_sort |
impact of variable horizon shade on the growing season energy budget of a subalpine headwater wetland |
publisher |
MDPI AG |
publishDate |
2021 |
url |
https://doaj.org/article/343fe3e1f9dd4bda8d5992b0ff54d61a |
work_keys_str_mv |
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