New Allometric Equations for Arctic Shrubs and Their Application for Calculating the Albedo of Surfaces with Snow and Protruding Branches

Author:

Belke-Brea M.123,Domine F.124,Boudreau S.25,Picard G.6,Barrere M.1237,Arnaud L.6,Paradis M.5

Affiliation:

1. a Takuvik Joint International Laboratory, Université Laval, Quebec City, Quebec, Canada

2. b Centre d’Études Nordiques, Université Laval, Quebec City, Quebec, Canada

3. c Department of Geography, Université Laval, Quebec City, Quebec, Canada

4. d Department of Chemistry, Université Laval, Quebec City, Quebec, Canada

5. e Department of Biology, Université Laval, Quebec City, Quebec, Canada

6. f Université Grenoble Alpes, CNRS, IRD, Grenoble INP, IGE, Grenoble, France

7. g Météo-France–CNRS, CNRM UMR 3589, CEN, Grenoble, France

Abstract

AbstractArctic shrubs reduce surface albedo in winter when branches protrude above the snow. To calculate the albedo of those mixed surfaces, the branch area index (BAI) of Arctic shrubs needs to be known. Moreover, an exposed-vegetation function is required to determine the BAI for protruding branches only. This study used a structural analysis of 30Betula glandulosashrubs, sampled near Umiujaq, northern Quebec, to (i) establish an allometric relationship between shrub height and BAI and (ii) determine a specific exposed-vegetation function for Arctic shrubs. The spectral albedo (400–1080 nm) of mixed surfaces was then simulated with the equations derived from this study and validated with in situ measured spectra. Shrubs were sampled from two sites, one along the coast and the other in a nearby valley. The shrub height–BAI relationship varied between both sites. BAI values of shrubs growing in the wind-sheltered valley were 30%–50% lower. The exposed-vegetation function obtained here differed from the linear functions found in the literature. The linear functions strongly overestimated the BAI of exposed branches. Albedo was well simulated with an accuracy of 3% when using an allometric relationship adapted to the environmental conditions of our study site. However, simulated albedo values were consistently higher than field measurements, probably because radiation absorbed by impurities and buried branches was neglected in the model. We conclude that specific exposed-vegetation and allometric equations need to be implemented in models to accurately simulate the albedo of mixed snow–shrub surfaces.

Funder

Fondation BNP Paribas

Canadian Network for Research and Innovation in Machining Technology, Natural Sciences and Engineering Research Council of Canada

Institut Polaire Français Paul Emile Victor

Publisher

American Meteorological Society

Subject

Atmospheric Science

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