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Analysis of growing season carbon and water fluxes of a subalpine wetland in the Canadian Rocky Mountains: implications of shade on ecosystem water use efficiency
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  • Dylan Hrach,
  • Richard Petrone,
  • Adam Green,
  • Myroslava Khomik
Dylan Hrach
University of Waterloo

Corresponding Author:dmhrach@uwaterloo.ca

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Richard Petrone
University of Waterloo
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Adam Green
University of Waterloo Faculty of Environment
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Myroslava Khomik
University of Waterloo
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Mountain regions are an important regulator in the global water cycle through their disproportionate water contribution. Often referred to as the “Water Towers of the World”, mountains contribute 40 to 60% of the world’s annual surface flow. Shade is a common feature in mountains, where complex terrain cycles land surfaces in and out of shadows over daily and seasonal scales. This study investigated turbulent water and carbon dioxide fluxes over the snow-free period in a subalpine wetland in the Canadian Rocky Mountains, from June 7th to September 10th, 2018. Shading had a significant and substantial effect on water and carbon fluxes at our site. Each hourly increase of shade per day reduced evapotranspiration (ET) and gross primary production (GPP) by 0.42 mm and 0.77 gCm-2, equivalent to 17% and 15% per day, respectively, over the entire study period. However, during only peak growing season, when leaves were fully out and mature, shade caused by the local complex terrain, reduced ET and increased GPP, likely due to enhanced diffuse radiation. The overall result was increased water use efficiency at the site during periods of increased shading during the peak growing season. In addition to incoming solar radiation (Rg), temporal variability in ET was found to relate to temporal variability in soil temperature, moisture and vapour pressure deficit. Shade impacted the curvature and intercept of the nonlinear ET-Rg relationship at our site. In contrast, temporal variability in GPP at our site was dependent largely on Rg only. Our findings suggest that shaded subalpine wetlands can store large volumes of water for late season runoff and are productive through short growing seasons.
29 Mar 2021Submitted to Hydrological Processes
30 Mar 2021Submission Checks Completed
30 Mar 2021Assigned to Editor
30 Mar 2021Reviewer(s) Assigned
30 Mar 2021Review(s) Completed, Editorial Evaluation Pending
26 Jun 2021Editorial Decision: Revise Major
27 Sep 20211st Revision Received
28 Sep 2021Submission Checks Completed
28 Sep 2021Assigned to Editor
28 Sep 2021Reviewer(s) Assigned
24 Oct 2021Review(s) Completed, Editorial Evaluation Pending
24 Oct 2021Editorial Decision: Accept
Jan 2022Published in Hydrological Processes volume 36 issue 1. 10.1002/hyp.14425