Measurement and modeling of ablation of the bottom of supraglacial lakes in western Greenland
We report measurements of ablation rates of the bottom of two supraglacial lakes and of temperatures at different depths collected during the summers of 2010 and 2011 in west Greenland. To our knowledge, this is the first time that such data sets are reported and discussed in the literature. The mea...
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ftdatacite:10.7916/d8np24bq 2023-05-15T16:28:20+02:00 Measurement and modeling of ablation of the bottom of supraglacial lakes in western Greenland Tedesco, Marco Lüthje, M. Steffen, K. Steiner, N. Fettweis, X. Willis, I. Bayou, N. Banwell, A. 2012 https://dx.doi.org/10.7916/d8np24bq https://academiccommons.columbia.edu/doi/10.7916/D8NP24BQ unknown Columbia University https://dx.doi.org/10.1029/2011gl049882 Glacial lakes Ablation Aerothermodynamics Meltwater Water temperature Ice sheets Geology FOS Earth and related environmental sciences Geomorphology Hydrology article-journal ScholarlyArticle Text 2012 ftdatacite https://doi.org/10.7916/d8np24bq https://doi.org/10.1029/2011gl049882 2022-03-10T12:27:56Z We report measurements of ablation rates of the bottom of two supraglacial lakes and of temperatures at different depths collected during the summers of 2010 and 2011 in west Greenland. To our knowledge, this is the first time that such data sets are reported and discussed in the literature. The measured ablation rates at the bottom of the two lakes are of the order of ∼6 cm/day, versus a rate of ∼2.5–3 cm/day in the case of bare ice of surrounding areas. Though our measurements suggest the presence of a vertical temperature gradient, it is not possible to draw final conclusions as the measured gradient is smaller than the accuracy of our temperature sensors. In-situ measurements are compared with the results of a thermodynamic model forced with the outputs of a regional climate model. In general, the model is able to satisfactorily reproduce the measured quantities with RMSE of the order of 3–4 cm for the ablation and ∼1.5°C in the case of water temperature. Our results confirm that the ablation at the bottom of supraglacial lakes plays an important role on the overall lake volume with the ablation in the case of ice covered by a lake being 110–135% of that over bare ice at nearby locations. Beside ice sheet hydrological implications, melting at the bottom of a supraglacial lake might affect estimates of lake volume from spaceborne visible and near-infrared measurements. Text Greenland Ice Sheet DataCite Metadata Store (German National Library of Science and Technology) Greenland |
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Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
unknown |
topic |
Glacial lakes Ablation Aerothermodynamics Meltwater Water temperature Ice sheets Geology FOS Earth and related environmental sciences Geomorphology Hydrology |
spellingShingle |
Glacial lakes Ablation Aerothermodynamics Meltwater Water temperature Ice sheets Geology FOS Earth and related environmental sciences Geomorphology Hydrology Tedesco, Marco Lüthje, M. Steffen, K. Steiner, N. Fettweis, X. Willis, I. Bayou, N. Banwell, A. Measurement and modeling of ablation of the bottom of supraglacial lakes in western Greenland |
topic_facet |
Glacial lakes Ablation Aerothermodynamics Meltwater Water temperature Ice sheets Geology FOS Earth and related environmental sciences Geomorphology Hydrology |
description |
We report measurements of ablation rates of the bottom of two supraglacial lakes and of temperatures at different depths collected during the summers of 2010 and 2011 in west Greenland. To our knowledge, this is the first time that such data sets are reported and discussed in the literature. The measured ablation rates at the bottom of the two lakes are of the order of ∼6 cm/day, versus a rate of ∼2.5–3 cm/day in the case of bare ice of surrounding areas. Though our measurements suggest the presence of a vertical temperature gradient, it is not possible to draw final conclusions as the measured gradient is smaller than the accuracy of our temperature sensors. In-situ measurements are compared with the results of a thermodynamic model forced with the outputs of a regional climate model. In general, the model is able to satisfactorily reproduce the measured quantities with RMSE of the order of 3–4 cm for the ablation and ∼1.5°C in the case of water temperature. Our results confirm that the ablation at the bottom of supraglacial lakes plays an important role on the overall lake volume with the ablation in the case of ice covered by a lake being 110–135% of that over bare ice at nearby locations. Beside ice sheet hydrological implications, melting at the bottom of a supraglacial lake might affect estimates of lake volume from spaceborne visible and near-infrared measurements. |
format |
Text |
author |
Tedesco, Marco Lüthje, M. Steffen, K. Steiner, N. Fettweis, X. Willis, I. Bayou, N. Banwell, A. |
author_facet |
Tedesco, Marco Lüthje, M. Steffen, K. Steiner, N. Fettweis, X. Willis, I. Bayou, N. Banwell, A. |
author_sort |
Tedesco, Marco |
title |
Measurement and modeling of ablation of the bottom of supraglacial lakes in western Greenland |
title_short |
Measurement and modeling of ablation of the bottom of supraglacial lakes in western Greenland |
title_full |
Measurement and modeling of ablation of the bottom of supraglacial lakes in western Greenland |
title_fullStr |
Measurement and modeling of ablation of the bottom of supraglacial lakes in western Greenland |
title_full_unstemmed |
Measurement and modeling of ablation of the bottom of supraglacial lakes in western Greenland |
title_sort |
measurement and modeling of ablation of the bottom of supraglacial lakes in western greenland |
publisher |
Columbia University |
publishDate |
2012 |
url |
https://dx.doi.org/10.7916/d8np24bq https://academiccommons.columbia.edu/doi/10.7916/D8NP24BQ |
geographic |
Greenland |
geographic_facet |
Greenland |
genre |
Greenland Ice Sheet |
genre_facet |
Greenland Ice Sheet |
op_relation |
https://dx.doi.org/10.1029/2011gl049882 |
op_doi |
https://doi.org/10.7916/d8np24bq https://doi.org/10.1029/2011gl049882 |
_version_ |
1766017979871395840 |