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Permanent link (DOI): https://doi.org/10.7939/R3222RH36

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Elevation dependent landscape processes in rapidly warming sub-Arctic mountains: influences of snow, temperature and vegetation Open Access

Descriptions

Other title
Subject/Keyword
Snow albedo feedback
Climate
Land Surface Temperature (LST)
Type of item
Thesis
Degree grantor
University of Alberta
Author or creator
Williamson, Scott N
Supervisor and department
Gamon, John (Earth and Atmospheric Sciences & Biological Sciences)
Hik, David (Biological Sciences)
Examining committee member and department
Grant, Robert (Renewable Resources)
Marsh, Philip (Geography and Environmental Studies)
Kavanaugh, Jeffrey (Earth and Atmospheric Sciences)
Department
Department of Biological Sciences
Specialization
Ecology
Date accepted
2015-09-24T14:46:19Z
Graduation date
2015-11
Degree
Doctor of Philosophy
Degree level
Doctoral
Abstract
The loss of spring snow in the Northern Hemisphere has been dramatic. From 1967 to 2008 snow cover decreased by 14% in May and 46% in June, with a simultaneous reduction in snow cover duration of 6 – 8 days per decade in both summer and fall. These effects have been particularly pronounced in the Kluane region of the southwest Yukon, making the area well suited for a detailed study of the effects of the reciprocal interactions of snow cover decline with ecological, geographical and climatological features. The mountainous Kluane region, like most of the Arctic, is difficult to access and has few long-term ground-based observations, which necessitates the use of remote sensing and mathematical modelling to determine surface characteristics. This thesis integrates data from diverse sources including meteorological stations, field albedo measurements, downscaled surface temperature, infrared Land Surface Temperature (LST), snow cover, land cover, and cloud cover to quantify the snow albedo feedback in the southwest Yukon. The first four chapters of this thesis addresses the validation and integration of different sources of data. My main findings are that (i) cloud contamination of MODIS-derived day-time LST within the study area is ~15%, which cools affected grid cells by no more than 2 K; (ii) combining night-time with day-time LST leads to a cold bias when compared to temporally averaged (8-day or monthly) air temperature; and (iii) the cold bias gets larger as within grid cell snow fraction increases. The last three chapters of my thesis attempts to account for various feedback processes using a combination of field measurements and modeling studies. Following spring snow melt, albedo increases for woody tundra vegetation as the growing season progresses, but the increase is small in magnitude compared to the albedo difference between snow covered and snow-free land. The albedo increase caused by the progressive canopy closure of woody vegetation is differentiated by stature and species, a result that will influence tundra energy balance on a successional timescale in a wetter, warmer Arctic. Finally, I demonstrate that the 35 – 50% decrease in snow cover in tundra in May between 2000 and 2008 produces a small radiative feedback to climate, but the strength is insufficient to influence the monthly average temperature change. This suggests that snow cover and temperature change is largely the result of external forcing consistent with meridional heat transport. Furthermore, the similarity in temperature trends among three land cover types (Icefields, Conifer forests with no snow, and Tundra characterized by a large decrease in snow cover) indicates that the snow cover albedo feedback contributes < 6% (or the equivalent of <0.091 W m-2 per decade over the 2000 to 2008 study period) to the changes observed in air temperature. Consequently, if the atmospheric local heating related to the large albedo decrease caused by snow cover decline is small, the much smaller albedo changes caused by successional changes in vegetation will be negligible over the short-term.
Language
English
DOI
doi:10.7939/R3222RH36
Rights
Permission is hereby granted to the University of Alberta Libraries to reproduce single copies of this thesis and to lend or sell such copies for private, scholarly or scientific research purposes only. The author reserves all other publication and other rights in association with the copyright in the thesis and, except as herein before provided, neither the thesis nor any substantial portion thereof may be printed or otherwise reproduced in any material form whatsoever without the author's prior written permission.
Citation for previous publication
Williamson, S. N., Hik, D. S., Gamon, J. A., Kavanaugh, J. L., & Koh, S. (2013). Evaluating cloud contamination in clear-sky MODIS Terra daytime land surface temperatures using ground-based meteorology station observations. Journal of Climate, 26(5), 1551-1560.Williamson, S. N., Hik, D. S., Gamon, J. A., Kavanaugh, J. L., & Flowers, G. E. (2014). Estimating temperature fields from MODIS land surface temperature and air temperature observations in a sub-Arctic Alpine environment. Remote Sensing, 6(2), 946-963.

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