Quantifying meltwater refreezing along a transect of sites on the Greenland ice sheet

On the Greenland ice sheet, a significant quantity of surface meltwater refreezes within the firn, creating uncertainty in surface mass balance estimates. This refreezing has the potential to buffer seasonal runoff to future increases in melting, but direct measurement of the process remains difficu...

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Published in:The Cryosphere
Main Authors: Cox, C., Humphrey, N., Harper, J.
Format: Text
Language:English
Published: 2018
Subjects:
Online Access:https://doi.org/10.5194/tc-9-691-2015
https://tc.copernicus.org/articles/9/691/2015/
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spelling ftcopernicus:oai:publications.copernicus.org:tc27201 2023-05-15T16:27:01+02:00 Quantifying meltwater refreezing along a transect of sites on the Greenland ice sheet Cox, C. Humphrey, N. Harper, J. 2018-09-27 application/pdf https://doi.org/10.5194/tc-9-691-2015 https://tc.copernicus.org/articles/9/691/2015/ eng eng doi:10.5194/tc-9-691-2015 https://tc.copernicus.org/articles/9/691/2015/ eISSN: 1994-0424 Text 2018 ftcopernicus https://doi.org/10.5194/tc-9-691-2015 2020-07-20T16:24:40Z On the Greenland ice sheet, a significant quantity of surface meltwater refreezes within the firn, creating uncertainty in surface mass balance estimates. This refreezing has the potential to buffer seasonal runoff to future increases in melting, but direct measurement of the process remains difficult. We present a method for quantifying refreezing at point locations using in situ firn temperature observations. A time series of sub-hourly firn temperature profiles were collected over the course of two melt seasons from 2007 to 2009 along a transect of 11 sites in the accumulation zone of Greenland. Seasonal changes in temperature profiles combined with heat flux estimates based on high-temporal-resolution temperature gradients enable us to isolate the heat released by refreezing using conservation of energy. Our method is verified from winter data when no refreezing takes place, and uncertainty is estimated using a Monte Carlo technique. While we limit our method to a subsection of firn between depths of 1 and 10 m, our refreezing estimates appear to differ significantly from model-based estimates. Furthermore, results indicate that a significant amount of refreezing takes place at depths greater than 1 m and that lateral migration of meltwater significantly complicates the relationship between total surface melt and total refreezing. Text Greenland Ice Sheet Copernicus Publications: E-Journals Greenland The Cryosphere 9 2 691 701
institution Open Polar
collection Copernicus Publications: E-Journals
op_collection_id ftcopernicus
language English
description On the Greenland ice sheet, a significant quantity of surface meltwater refreezes within the firn, creating uncertainty in surface mass balance estimates. This refreezing has the potential to buffer seasonal runoff to future increases in melting, but direct measurement of the process remains difficult. We present a method for quantifying refreezing at point locations using in situ firn temperature observations. A time series of sub-hourly firn temperature profiles were collected over the course of two melt seasons from 2007 to 2009 along a transect of 11 sites in the accumulation zone of Greenland. Seasonal changes in temperature profiles combined with heat flux estimates based on high-temporal-resolution temperature gradients enable us to isolate the heat released by refreezing using conservation of energy. Our method is verified from winter data when no refreezing takes place, and uncertainty is estimated using a Monte Carlo technique. While we limit our method to a subsection of firn between depths of 1 and 10 m, our refreezing estimates appear to differ significantly from model-based estimates. Furthermore, results indicate that a significant amount of refreezing takes place at depths greater than 1 m and that lateral migration of meltwater significantly complicates the relationship between total surface melt and total refreezing.
format Text
author Cox, C.
Humphrey, N.
Harper, J.
spellingShingle Cox, C.
Humphrey, N.
Harper, J.
Quantifying meltwater refreezing along a transect of sites on the Greenland ice sheet
author_facet Cox, C.
Humphrey, N.
Harper, J.
author_sort Cox, C.
title Quantifying meltwater refreezing along a transect of sites on the Greenland ice sheet
title_short Quantifying meltwater refreezing along a transect of sites on the Greenland ice sheet
title_full Quantifying meltwater refreezing along a transect of sites on the Greenland ice sheet
title_fullStr Quantifying meltwater refreezing along a transect of sites on the Greenland ice sheet
title_full_unstemmed Quantifying meltwater refreezing along a transect of sites on the Greenland ice sheet
title_sort quantifying meltwater refreezing along a transect of sites on the greenland ice sheet
publishDate 2018
url https://doi.org/10.5194/tc-9-691-2015
https://tc.copernicus.org/articles/9/691/2015/
geographic Greenland
geographic_facet Greenland
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_source eISSN: 1994-0424
op_relation doi:10.5194/tc-9-691-2015
https://tc.copernicus.org/articles/9/691/2015/
op_doi https://doi.org/10.5194/tc-9-691-2015
container_title The Cryosphere
container_volume 9
container_issue 2
container_start_page 691
op_container_end_page 701
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