Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains
In situ observations of summer (June through August, or JJA) albedo are presented for the period 2002–2017 from Haig Glacier in the Canadian Rocky Mountains. The observations provide insight into the seasonal evolution and interannual variability of snow and ice albedo, including the effects of summ...
Published in: | The Cryosphere |
---|---|
Main Authors: | , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Copernicus Publications
2020
|
Subjects: | |
Online Access: | https://doi.org/10.5194/tc-14-3249-2020 https://tc.copernicus.org/articles/14/3249/2020/tc-14-3249-2020.pdf https://doaj.org/article/2dad714e359f4ae78a356148bb615803 |
id |
fttriple:oai:gotriple.eu:oai:doaj.org/article:2dad714e359f4ae78a356148bb615803 |
---|---|
record_format |
openpolar |
spelling |
fttriple:oai:gotriple.eu:oai:doaj.org/article:2dad714e359f4ae78a356148bb615803 2023-05-15T18:32:17+02:00 Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains S. J. Marshall K. Miller 2020-10-01 https://doi.org/10.5194/tc-14-3249-2020 https://tc.copernicus.org/articles/14/3249/2020/tc-14-3249-2020.pdf https://doaj.org/article/2dad714e359f4ae78a356148bb615803 en eng Copernicus Publications doi:10.5194/tc-14-3249-2020 1994-0416 1994-0424 https://tc.copernicus.org/articles/14/3249/2020/tc-14-3249-2020.pdf https://doaj.org/article/2dad714e359f4ae78a356148bb615803 undefined The Cryosphere, Vol 14, Pp 3249-3267 (2020) geo envir Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2020 fttriple https://doi.org/10.5194/tc-14-3249-2020 2023-01-22T18:03:51Z In situ observations of summer (June through August, or JJA) albedo are presented for the period 2002–2017 from Haig Glacier in the Canadian Rocky Mountains. The observations provide insight into the seasonal evolution and interannual variability of snow and ice albedo, including the effects of summer snowfall, the decay of snow albedo through the melt season, and the potential short-term impacts of regional wildfire activity on glacier-albedo reductions. Mean JJA albedo (± 1σ) recorded at an automatic weather station in the upper ablation zone of the glacier was αS=0.55 ± 0.07 over this period, with no evidence of long-term trends in surface albedo. Each summer the surface conditions at the weather station undergo a transition from a dry, reflective spring snowpack (αS∼0.8) to a wet, homogeneous midsummer snowpack (αS∼0.5) to exposed, impurity-rich glacier ice, with a measured albedo of 0.21 ± 0.06 over the study period. The ice albedo drops to ∼ 0.12 during years of intense regional wildfire activity such as 2003 and 2017, but it recovers from this in subsequent years. This seasonal albedo decline is well simulated through a parameterization of snow-albedo decay based on cumulative positive degree days (PDDs), but the parameterization does not capture the impact of summer snowfall events, which cause transient increases in albedo and significantly reduce glacier melt. We introduce this effect through a stochastic parameterization of summer precipitation events within a surface energy balance model. The amount of precipitation and the date of snowfall are randomly selected for each model realization based on a predefined number of summer snow events. This stochastic parameterization provides an improved representation of the mean summer albedo and mass balance at Haig Glacier. We also suggest modifications to conventional degree-day melt factors to better capture the effects of seasonal albedo evolution in temperature-index or positive-degree-day melt models on mountain glaciers. Climate, hydrology, or glacier ... Article in Journal/Newspaper The Cryosphere Unknown The Cryosphere 14 10 3249 3267 |
institution |
Open Polar |
collection |
Unknown |
op_collection_id |
fttriple |
language |
English |
topic |
geo envir |
spellingShingle |
geo envir S. J. Marshall K. Miller Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains |
topic_facet |
geo envir |
description |
In situ observations of summer (June through August, or JJA) albedo are presented for the period 2002–2017 from Haig Glacier in the Canadian Rocky Mountains. The observations provide insight into the seasonal evolution and interannual variability of snow and ice albedo, including the effects of summer snowfall, the decay of snow albedo through the melt season, and the potential short-term impacts of regional wildfire activity on glacier-albedo reductions. Mean JJA albedo (± 1σ) recorded at an automatic weather station in the upper ablation zone of the glacier was αS=0.55 ± 0.07 over this period, with no evidence of long-term trends in surface albedo. Each summer the surface conditions at the weather station undergo a transition from a dry, reflective spring snowpack (αS∼0.8) to a wet, homogeneous midsummer snowpack (αS∼0.5) to exposed, impurity-rich glacier ice, with a measured albedo of 0.21 ± 0.06 over the study period. The ice albedo drops to ∼ 0.12 during years of intense regional wildfire activity such as 2003 and 2017, but it recovers from this in subsequent years. This seasonal albedo decline is well simulated through a parameterization of snow-albedo decay based on cumulative positive degree days (PDDs), but the parameterization does not capture the impact of summer snowfall events, which cause transient increases in albedo and significantly reduce glacier melt. We introduce this effect through a stochastic parameterization of summer precipitation events within a surface energy balance model. The amount of precipitation and the date of snowfall are randomly selected for each model realization based on a predefined number of summer snow events. This stochastic parameterization provides an improved representation of the mean summer albedo and mass balance at Haig Glacier. We also suggest modifications to conventional degree-day melt factors to better capture the effects of seasonal albedo evolution in temperature-index or positive-degree-day melt models on mountain glaciers. Climate, hydrology, or glacier ... |
format |
Article in Journal/Newspaper |
author |
S. J. Marshall K. Miller |
author_facet |
S. J. Marshall K. Miller |
author_sort |
S. J. Marshall |
title |
Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains |
title_short |
Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains |
title_full |
Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains |
title_fullStr |
Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains |
title_full_unstemmed |
Seasonal and interannual variability of melt-season albedo at Haig Glacier, Canadian Rocky Mountains |
title_sort |
seasonal and interannual variability of melt-season albedo at haig glacier, canadian rocky mountains |
publisher |
Copernicus Publications |
publishDate |
2020 |
url |
https://doi.org/10.5194/tc-14-3249-2020 https://tc.copernicus.org/articles/14/3249/2020/tc-14-3249-2020.pdf https://doaj.org/article/2dad714e359f4ae78a356148bb615803 |
genre |
The Cryosphere |
genre_facet |
The Cryosphere |
op_source |
The Cryosphere, Vol 14, Pp 3249-3267 (2020) |
op_relation |
doi:10.5194/tc-14-3249-2020 1994-0416 1994-0424 https://tc.copernicus.org/articles/14/3249/2020/tc-14-3249-2020.pdf https://doaj.org/article/2dad714e359f4ae78a356148bb615803 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/tc-14-3249-2020 |
container_title |
The Cryosphere |
container_volume |
14 |
container_issue |
10 |
container_start_page |
3249 |
op_container_end_page |
3267 |
_version_ |
1766216389161385984 |