Application of an improved surface energy balance model to two large valley glaciers in the St. Elias Mountains, Yukon
Glacier surficial melt rates are commonly modelled using surface energy balance (SEB) models, with outputs applied to extend point-based mass-balance measurements to regional scales, assess water resource availability, examine supraglacial hydrology and to investigate the relationship between surfac...
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Cambridge University Press
2021
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Online Access: | https://doi.org/10.1017/jog.2020.106 https://doaj.org/article/ca1c11a0bcfe4a6ba015069a68b4e0e1 |
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ftdoajarticles:oai:doaj.org/article:ca1c11a0bcfe4a6ba015069a68b4e0e1 2023-05-15T16:22:28+02:00 Application of an improved surface energy balance model to two large valley glaciers in the St. Elias Mountains, Yukon Tim Hill Christine F. Dow Eleanor A. Bash Luke Copland 2021-04-01T00:00:00Z https://doi.org/10.1017/jog.2020.106 https://doaj.org/article/ca1c11a0bcfe4a6ba015069a68b4e0e1 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143020001069/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2020.106 0022-1430 1727-5652 https://doaj.org/article/ca1c11a0bcfe4a6ba015069a68b4e0e1 Journal of Glaciology, Vol 67, Pp 297-312 (2021) Energy balance melt surface surface mass budget Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.1017/jog.2020.106 2023-03-12T01:30:57Z Glacier surficial melt rates are commonly modelled using surface energy balance (SEB) models, with outputs applied to extend point-based mass-balance measurements to regional scales, assess water resource availability, examine supraglacial hydrology and to investigate the relationship between surface melt and ice dynamics. We present an improved SEB model that addresses the primary limitations of existing models by: (1) deriving high-resolution (30 m) surface albedo from Landsat 8 imagery, (2) calculating shadows cast onto the glacier surface by high-relief topography to model incident shortwave radiation, (3) developing an algorithm to map debris sufficiently thick to insulate the glacier surface and (4) presenting a formulation of the SEB model coupled to a subsurface heat conduction model. We drive the model with 6 years of in situ meteorological data from Kaskawulsh Glacier and Nàłùdäy (Lowell) Glacier in the St. Elias Mountains, Yukon, Canada, and validate outputs against in situ measurements. Modelled seasonal melt agrees with observations within 9% across a range of elevations on both glaciers in years with high-quality in situ observations. We recommend applying the model to investigate the impacts of surface melt for individual glaciers when sufficient input data are available. Article in Journal/Newspaper glacier* Journal of Glaciology Yukon Directory of Open Access Journals: DOAJ Articles Yukon Canada Kaskawulsh Glacier ENVELOPE(-139.104,-139.104,60.749,60.749) Lowell Glacier ENVELOPE(-138.254,-138.254,60.299,60.299) Journal of Glaciology 67 262 297 312 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Energy balance melt surface surface mass budget Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Energy balance melt surface surface mass budget Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Tim Hill Christine F. Dow Eleanor A. Bash Luke Copland Application of an improved surface energy balance model to two large valley glaciers in the St. Elias Mountains, Yukon |
topic_facet |
Energy balance melt surface surface mass budget Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Glacier surficial melt rates are commonly modelled using surface energy balance (SEB) models, with outputs applied to extend point-based mass-balance measurements to regional scales, assess water resource availability, examine supraglacial hydrology and to investigate the relationship between surface melt and ice dynamics. We present an improved SEB model that addresses the primary limitations of existing models by: (1) deriving high-resolution (30 m) surface albedo from Landsat 8 imagery, (2) calculating shadows cast onto the glacier surface by high-relief topography to model incident shortwave radiation, (3) developing an algorithm to map debris sufficiently thick to insulate the glacier surface and (4) presenting a formulation of the SEB model coupled to a subsurface heat conduction model. We drive the model with 6 years of in situ meteorological data from Kaskawulsh Glacier and Nàłùdäy (Lowell) Glacier in the St. Elias Mountains, Yukon, Canada, and validate outputs against in situ measurements. Modelled seasonal melt agrees with observations within 9% across a range of elevations on both glaciers in years with high-quality in situ observations. We recommend applying the model to investigate the impacts of surface melt for individual glaciers when sufficient input data are available. |
format |
Article in Journal/Newspaper |
author |
Tim Hill Christine F. Dow Eleanor A. Bash Luke Copland |
author_facet |
Tim Hill Christine F. Dow Eleanor A. Bash Luke Copland |
author_sort |
Tim Hill |
title |
Application of an improved surface energy balance model to two large valley glaciers in the St. Elias Mountains, Yukon |
title_short |
Application of an improved surface energy balance model to two large valley glaciers in the St. Elias Mountains, Yukon |
title_full |
Application of an improved surface energy balance model to two large valley glaciers in the St. Elias Mountains, Yukon |
title_fullStr |
Application of an improved surface energy balance model to two large valley glaciers in the St. Elias Mountains, Yukon |
title_full_unstemmed |
Application of an improved surface energy balance model to two large valley glaciers in the St. Elias Mountains, Yukon |
title_sort |
application of an improved surface energy balance model to two large valley glaciers in the st. elias mountains, yukon |
publisher |
Cambridge University Press |
publishDate |
2021 |
url |
https://doi.org/10.1017/jog.2020.106 https://doaj.org/article/ca1c11a0bcfe4a6ba015069a68b4e0e1 |
long_lat |
ENVELOPE(-139.104,-139.104,60.749,60.749) ENVELOPE(-138.254,-138.254,60.299,60.299) |
geographic |
Yukon Canada Kaskawulsh Glacier Lowell Glacier |
geographic_facet |
Yukon Canada Kaskawulsh Glacier Lowell Glacier |
genre |
glacier* Journal of Glaciology Yukon |
genre_facet |
glacier* Journal of Glaciology Yukon |
op_source |
Journal of Glaciology, Vol 67, Pp 297-312 (2021) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143020001069/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2020.106 0022-1430 1727-5652 https://doaj.org/article/ca1c11a0bcfe4a6ba015069a68b4e0e1 |
op_doi |
https://doi.org/10.1017/jog.2020.106 |
container_title |
Journal of Glaciology |
container_volume |
67 |
container_issue |
262 |
container_start_page |
297 |
op_container_end_page |
312 |
_version_ |
1766010440479932416 |