A mechanism for ice layer formation in glacial firn ...

There is ample evidence for ice layers and lenses within glacial firn. The standard model19 for ice layer formation localizes the refreezing by perching of meltwater on pre-existing20 discontinuities. Here we argue that even extreme melting events provide insufficient flux21 for this mechanism. Usin...

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Main Author: Surendra Adhikari
Format: Dataset
Language:unknown
Published: Root 2024
Subjects:
Online Access:https://dx.doi.org/10.48577/jpl.xrl4l9
http://dataverse.jpl.nasa.gov/citation?persistentId=doi:10.48577/jpl.XRL4L9
id ftdatacite:10.48577/jpl.xrl4l9
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spelling ftdatacite:10.48577/jpl.xrl4l9 2024-09-15T18:09:43+00:00 A mechanism for ice layer formation in glacial firn ... Surendra Adhikari 2024 https://dx.doi.org/10.48577/jpl.xrl4l9 http://dataverse.jpl.nasa.gov/citation?persistentId=doi:10.48577/jpl.XRL4L9 unknown Root dataset Dataset 2024 ftdatacite https://doi.org/10.48577/jpl.xrl4l9 2024-08-01T11:59:46Z There is ample evidence for ice layers and lenses within glacial firn. The standard model19 for ice layer formation localizes the refreezing by perching of meltwater on pre-existing20 discontinuities. Here we argue that even extreme melting events provide insufficient flux21 for this mechanism. Using a thermomechanical model we demonstrate a different mech22 anism of ice layer formation. After a melting event when the drying front catches up with23 the wetting front and arrests melt percolation, conductive heat loss freezes the remain24 ing melt in place to form an ice layer. This model reproduces the depth of a new ice layer25 at the Dye-2 site in Greenland. It provides a deeper insight into the interpretation of firn26 stratigraphy and past climate variability. It also improves the simulation of firn densi27 fication processes, a key source of uncertainty in assessing and attributing ice sheet mass28 balance based on satellite altimetry and gravimetry data. ... Dataset Greenland Ice Sheet DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language unknown
description There is ample evidence for ice layers and lenses within glacial firn. The standard model19 for ice layer formation localizes the refreezing by perching of meltwater on pre-existing20 discontinuities. Here we argue that even extreme melting events provide insufficient flux21 for this mechanism. Using a thermomechanical model we demonstrate a different mech22 anism of ice layer formation. After a melting event when the drying front catches up with23 the wetting front and arrests melt percolation, conductive heat loss freezes the remain24 ing melt in place to form an ice layer. This model reproduces the depth of a new ice layer25 at the Dye-2 site in Greenland. It provides a deeper insight into the interpretation of firn26 stratigraphy and past climate variability. It also improves the simulation of firn densi27 fication processes, a key source of uncertainty in assessing and attributing ice sheet mass28 balance based on satellite altimetry and gravimetry data. ...
format Dataset
author Surendra Adhikari
spellingShingle Surendra Adhikari
A mechanism for ice layer formation in glacial firn ...
author_facet Surendra Adhikari
author_sort Surendra Adhikari
title A mechanism for ice layer formation in glacial firn ...
title_short A mechanism for ice layer formation in glacial firn ...
title_full A mechanism for ice layer formation in glacial firn ...
title_fullStr A mechanism for ice layer formation in glacial firn ...
title_full_unstemmed A mechanism for ice layer formation in glacial firn ...
title_sort mechanism for ice layer formation in glacial firn ...
publisher Root
publishDate 2024
url https://dx.doi.org/10.48577/jpl.xrl4l9
http://dataverse.jpl.nasa.gov/citation?persistentId=doi:10.48577/jpl.XRL4L9
genre Greenland
Ice Sheet
genre_facet Greenland
Ice Sheet
op_doi https://doi.org/10.48577/jpl.xrl4l9
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