Surface ablation model evaluation on a drifting ice island in the Canadian Arctic
A 4-week micro-meteorological dataset was collected by an automatic weather station on a small ice island (0.13 km 2 ) adrift off Bylot Island (Lancaster Sound, Nunavut, Canada) during the 2011 melt season. This dataset provided an opportunity to identify the environmental variables and energy fluxe...
Published in: | Cold Regions Science and Technology |
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Language: | English |
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2015
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Online Access: | https://research-portal.st-andrews.ac.uk/en/researchoutput/surface-ablation-model-evaluation-on-a-drifting-ice-island-in-the-canadian-arctic(0ba58470-eacf-4694-82b8-a4d33c64f61b).html https://doi.org/10.1016/j.coldregions.2014.11.011 |
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ftunstandrewcris:oai:research-portal.st-andrews.ac.uk:publications/0ba58470-eacf-4694-82b8-a4d33c64f61b 2024-06-23T07:48:22+00:00 Surface ablation model evaluation on a drifting ice island in the Canadian Arctic Crawford, Anna J. Mueller, Derek Humphreys, Ellen Carrieres, Tom Tran, Hai 2015-02 https://research-portal.st-andrews.ac.uk/en/researchoutput/surface-ablation-model-evaluation-on-a-drifting-ice-island-in-the-canadian-arctic(0ba58470-eacf-4694-82b8-a4d33c64f61b).html https://doi.org/10.1016/j.coldregions.2014.11.011 eng eng https://research-portal.st-andrews.ac.uk/en/researchoutput/surface-ablation-model-evaluation-on-a-drifting-ice-island-in-the-canadian-arctic(0ba58470-eacf-4694-82b8-a4d33c64f61b).html info:eu-repo/semantics/restrictedAccess Crawford , A J , Mueller , D , Humphreys , E , Carrieres , T & Tran , H 2015 , ' Surface ablation model evaluation on a drifting ice island in the Canadian Arctic ' , Cold Regions Science and Technology , vol. 110 , pp. 170-182 . https://doi.org/10.1016/j.coldregions.2014.11.011 Ice hazards Ice islands Surface ablation Melting modeling Deterioration modeling Energy-balance article 2015 ftunstandrewcris https://doi.org/10.1016/j.coldregions.2014.11.011 2024-06-13T01:05:10Z A 4-week micro-meteorological dataset was collected by an automatic weather station on a small ice island (0.13 km 2 ) adrift off Bylot Island (Lancaster Sound, Nunavut, Canada) during the 2011 melt season. This dataset provided an opportunity to identify the environmental variables and energy fluxes that contribute most to surface ablation during the melt season, as well as test previously developed surface melt (ablation) models. Surface ablation was estimated using energy fluxes calculated using the bulk aerodynamic approach (EB AWS ) and three existing surface ablation models. These models included a simple solar radiation model developed for iceberg use (CIS-IB), a more sophisticated energy-balance model developed for ice island use (CIS-II), and a temperature index melt (TIM) model based on an assumed relationship between air temperature, time, and surface ablation. The models were driven by our measured micro-meteorological data (optimal forcing) or regional environmental forecast data from the Global Environmental Multiscale (GEM) Model, which is used for operational iceberg modeling. The sensible heat flux contributed most to the ice surface's available melt energy (47%), followed by net radiation (38%) and the latent heat flux (30%), while the subsurface heat flux removed 15% of available energy. When cumulative surface ablation was predicted with these calculated energy fluxes (EB AWS ), observed surface ablation was under-predicted by 38%. Results illustrate the decreased performance of the melt models when run with GEM data versus in-situ micro-meteorological data, which is optimal for model input but not available for operational modeling. The CIS-II model under-predicted cumulative surface ablation by 5.7% (RMSE = 1.2 cm) with observed micro-meteorological data and over-predicted cumulative surface ablation by 35% when run with GEM model data. This is likely a result of the GEM model wind speed being 57% greater than that recorded on the ice island. Since surface ablation plays a greater relative ... Article in Journal/Newspaper Arctic Arctic Bylot Island Iceberg* Lancaster Sound Nunavut University of St Andrews: Research Portal Arctic Bylot Island Canada Lancaster Sound ENVELOPE(-83.999,-83.999,74.218,74.218) Nunavut Cold Regions Science and Technology 110 170 182 |
institution |
Open Polar |
collection |
University of St Andrews: Research Portal |
op_collection_id |
ftunstandrewcris |
language |
English |
topic |
Ice hazards Ice islands Surface ablation Melting modeling Deterioration modeling Energy-balance |
spellingShingle |
Ice hazards Ice islands Surface ablation Melting modeling Deterioration modeling Energy-balance Crawford, Anna J. Mueller, Derek Humphreys, Ellen Carrieres, Tom Tran, Hai Surface ablation model evaluation on a drifting ice island in the Canadian Arctic |
topic_facet |
Ice hazards Ice islands Surface ablation Melting modeling Deterioration modeling Energy-balance |
description |
A 4-week micro-meteorological dataset was collected by an automatic weather station on a small ice island (0.13 km 2 ) adrift off Bylot Island (Lancaster Sound, Nunavut, Canada) during the 2011 melt season. This dataset provided an opportunity to identify the environmental variables and energy fluxes that contribute most to surface ablation during the melt season, as well as test previously developed surface melt (ablation) models. Surface ablation was estimated using energy fluxes calculated using the bulk aerodynamic approach (EB AWS ) and three existing surface ablation models. These models included a simple solar radiation model developed for iceberg use (CIS-IB), a more sophisticated energy-balance model developed for ice island use (CIS-II), and a temperature index melt (TIM) model based on an assumed relationship between air temperature, time, and surface ablation. The models were driven by our measured micro-meteorological data (optimal forcing) or regional environmental forecast data from the Global Environmental Multiscale (GEM) Model, which is used for operational iceberg modeling. The sensible heat flux contributed most to the ice surface's available melt energy (47%), followed by net radiation (38%) and the latent heat flux (30%), while the subsurface heat flux removed 15% of available energy. When cumulative surface ablation was predicted with these calculated energy fluxes (EB AWS ), observed surface ablation was under-predicted by 38%. Results illustrate the decreased performance of the melt models when run with GEM data versus in-situ micro-meteorological data, which is optimal for model input but not available for operational modeling. The CIS-II model under-predicted cumulative surface ablation by 5.7% (RMSE = 1.2 cm) with observed micro-meteorological data and over-predicted cumulative surface ablation by 35% when run with GEM model data. This is likely a result of the GEM model wind speed being 57% greater than that recorded on the ice island. Since surface ablation plays a greater relative ... |
format |
Article in Journal/Newspaper |
author |
Crawford, Anna J. Mueller, Derek Humphreys, Ellen Carrieres, Tom Tran, Hai |
author_facet |
Crawford, Anna J. Mueller, Derek Humphreys, Ellen Carrieres, Tom Tran, Hai |
author_sort |
Crawford, Anna J. |
title |
Surface ablation model evaluation on a drifting ice island in the Canadian Arctic |
title_short |
Surface ablation model evaluation on a drifting ice island in the Canadian Arctic |
title_full |
Surface ablation model evaluation on a drifting ice island in the Canadian Arctic |
title_fullStr |
Surface ablation model evaluation on a drifting ice island in the Canadian Arctic |
title_full_unstemmed |
Surface ablation model evaluation on a drifting ice island in the Canadian Arctic |
title_sort |
surface ablation model evaluation on a drifting ice island in the canadian arctic |
publishDate |
2015 |
url |
https://research-portal.st-andrews.ac.uk/en/researchoutput/surface-ablation-model-evaluation-on-a-drifting-ice-island-in-the-canadian-arctic(0ba58470-eacf-4694-82b8-a4d33c64f61b).html https://doi.org/10.1016/j.coldregions.2014.11.011 |
long_lat |
ENVELOPE(-83.999,-83.999,74.218,74.218) |
geographic |
Arctic Bylot Island Canada Lancaster Sound Nunavut |
geographic_facet |
Arctic Bylot Island Canada Lancaster Sound Nunavut |
genre |
Arctic Arctic Bylot Island Iceberg* Lancaster Sound Nunavut |
genre_facet |
Arctic Arctic Bylot Island Iceberg* Lancaster Sound Nunavut |
op_source |
Crawford , A J , Mueller , D , Humphreys , E , Carrieres , T & Tran , H 2015 , ' Surface ablation model evaluation on a drifting ice island in the Canadian Arctic ' , Cold Regions Science and Technology , vol. 110 , pp. 170-182 . https://doi.org/10.1016/j.coldregions.2014.11.011 |
op_relation |
https://research-portal.st-andrews.ac.uk/en/researchoutput/surface-ablation-model-evaluation-on-a-drifting-ice-island-in-the-canadian-arctic(0ba58470-eacf-4694-82b8-a4d33c64f61b).html |
op_rights |
info:eu-repo/semantics/restrictedAccess |
op_doi |
https://doi.org/10.1016/j.coldregions.2014.11.011 |
container_title |
Cold Regions Science and Technology |
container_volume |
110 |
container_start_page |
170 |
op_container_end_page |
182 |
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1802638787779493888 |