The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles

The formation of ice platelets in supercooled water is a manifestation of basal melt processes in the cavity. These crystals accumulate in large amounts below the fast ice to form a porous layer. Despite its importance for sea ice and ecosystems in coastal Antarctica, information about its formation...

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Main Authors: Hoppmann, Mario, Nicolaus, Marcel
Format: Conference Object
Language:unknown
Published: 2014
Subjects:
Online Access:https://epic.awi.de/id/eprint/39100/
https://epic.awi.de/id/eprint/39100/2/FRISP_2014_small.pdf
https://hdl.handle.net/10013/epic.46335
https://hdl.handle.net/10013/epic.46335.d002
id ftawi:oai:epic.awi.de:39100
record_format openpolar
spelling ftawi:oai:epic.awi.de:39100 2024-09-15T17:45:03+00:00 The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles Hoppmann, Mario Nicolaus, Marcel 2014 application/pdf https://epic.awi.de/id/eprint/39100/ https://epic.awi.de/id/eprint/39100/2/FRISP_2014_small.pdf https://hdl.handle.net/10013/epic.46335 https://hdl.handle.net/10013/epic.46335.d002 unknown https://epic.awi.de/id/eprint/39100/2/FRISP_2014_small.pdf https://hdl.handle.net/10013/epic.46335.d002 Hoppmann, M. orcid:0000-0003-1294-9531 and Nicolaus, M. orcid:0000-0003-0903-1746 (2014) The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles , 28th International Forum for Ice Shelf Processes (FRISP), Schlss Wahn, Cologne, Germany, 22 June 2014 - 25 June 2014 . hdl:10013/epic.46335 EPIC328th International Forum for Ice Shelf Processes (FRISP), Schlss Wahn, Cologne, Germany, 2014-06-22-2014-06-25 Conference notRev 2014 ftawi 2024-06-24T04:13:16Z The formation of ice platelets in supercooled water is a manifestation of basal melt processes in the cavity. These crystals accumulate in large amounts below the fast ice to form a porous layer. Despite its importance for sea ice and ecosystems in coastal Antarctica, information about its formation and spatio-temporal variability is sparse. This is at least partly attributed to the lack of suitable methodology. Method: We obtained a 15 month long time-series of sea-ice temperature profiles on the fast ice of Atka Bay, a coastal sea-ice regime in the eastern Weddell Sea. We used a thermistor chain with the additional capability of actively heating its thermistor elements, taking advantage of the different thermal characteristics of the surrounding medium. Despite the rising interest in this kind of instrument, its full potential has not been assessed yet. Calculating the basal energy budget, we find a negative oceanic heat flux which accounts for 18 % of seaice growth. This corresponds to a platelet layer ice-volume fraction of 18 %, which is also confirmed by model simulations and agrees well with a previous study at the same location. In addition, this study confirmed the seasonal evolution of the platelet layer found in the previous year. Ice platelets dominated the overall sea-ice thickness gain by effectively contributing 1.28 m, or 61 %, of the total sea ice growth. Finally we use this unique dataset to assess the potential of this relatively new instrument design (Jackson 2013), highlighting its advantages and pointing out its caveats. Conference Object Antarc* Antarctica Ice Shelf Sea ice Weddell Sea Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description The formation of ice platelets in supercooled water is a manifestation of basal melt processes in the cavity. These crystals accumulate in large amounts below the fast ice to form a porous layer. Despite its importance for sea ice and ecosystems in coastal Antarctica, information about its formation and spatio-temporal variability is sparse. This is at least partly attributed to the lack of suitable methodology. Method: We obtained a 15 month long time-series of sea-ice temperature profiles on the fast ice of Atka Bay, a coastal sea-ice regime in the eastern Weddell Sea. We used a thermistor chain with the additional capability of actively heating its thermistor elements, taking advantage of the different thermal characteristics of the surrounding medium. Despite the rising interest in this kind of instrument, its full potential has not been assessed yet. Calculating the basal energy budget, we find a negative oceanic heat flux which accounts for 18 % of seaice growth. This corresponds to a platelet layer ice-volume fraction of 18 %, which is also confirmed by model simulations and agrees well with a previous study at the same location. In addition, this study confirmed the seasonal evolution of the platelet layer found in the previous year. Ice platelets dominated the overall sea-ice thickness gain by effectively contributing 1.28 m, or 61 %, of the total sea ice growth. Finally we use this unique dataset to assess the potential of this relatively new instrument design (Jackson 2013), highlighting its advantages and pointing out its caveats.
format Conference Object
author Hoppmann, Mario
Nicolaus, Marcel
spellingShingle Hoppmann, Mario
Nicolaus, Marcel
The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles
author_facet Hoppmann, Mario
Nicolaus, Marcel
author_sort Hoppmann, Mario
title The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles
title_short The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles
title_full The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles
title_fullStr The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles
title_full_unstemmed The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles
title_sort seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles
publishDate 2014
url https://epic.awi.de/id/eprint/39100/
https://epic.awi.de/id/eprint/39100/2/FRISP_2014_small.pdf
https://hdl.handle.net/10013/epic.46335
https://hdl.handle.net/10013/epic.46335.d002
genre Antarc*
Antarctica
Ice Shelf
Sea ice
Weddell Sea
genre_facet Antarc*
Antarctica
Ice Shelf
Sea ice
Weddell Sea
op_source EPIC328th International Forum for Ice Shelf Processes (FRISP), Schlss Wahn, Cologne, Germany, 2014-06-22-2014-06-25
op_relation https://epic.awi.de/id/eprint/39100/2/FRISP_2014_small.pdf
https://hdl.handle.net/10013/epic.46335.d002
Hoppmann, M. orcid:0000-0003-1294-9531 and Nicolaus, M. orcid:0000-0003-0903-1746 (2014) The seasonal cycle of an ice-shelf influenced fast-ice cover, derived from thermistor-chain temperature profiles , 28th International Forum for Ice Shelf Processes (FRISP), Schlss Wahn, Cologne, Germany, 22 June 2014 - 25 June 2014 . hdl:10013/epic.46335
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