Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr

We reconstruct the pattern of surface accumulation in the region around Dome C, East Antarctica, since the last glacial. We use a set of 18 isochrones spanning all observable depths of the ice column, interpreted from various ice-penetrating radar surveys and a 1-D ice flow model to invert for accum...

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Published in:The Cryosphere
Main Authors: Cavitte, MGP, Parrenin, F, Ritz, C, Young, A, Van Liefferinge, B, Blankenship, DD, Frezzotti, M, Roberts, JL
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus GmbH 2018
Subjects:
Online Access:https://eprints.utas.edu.au/29936/
https://eprints.utas.edu.au/29936/1/131769%20-%20Accumulation%20patterns%20around%20Dome%20C,%20East%20Antarctica,%20in%20the%20last%2073%20kyr.pdf
id ftunivtasmania:oai:eprints.utas.edu.au:29936
record_format openpolar
spelling ftunivtasmania:oai:eprints.utas.edu.au:29936 2023-05-15T13:31:53+02:00 Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr Cavitte, MGP Parrenin, F Ritz, C Young, A Van Liefferinge, B Blankenship, DD Frezzotti, M Roberts, JL 2018 application/pdf https://eprints.utas.edu.au/29936/ https://eprints.utas.edu.au/29936/1/131769%20-%20Accumulation%20patterns%20around%20Dome%20C,%20East%20Antarctica,%20in%20the%20last%2073%20kyr.pdf en eng Copernicus GmbH https://eprints.utas.edu.au/29936/1/131769%20-%20Accumulation%20patterns%20around%20Dome%20C,%20East%20Antarctica,%20in%20the%20last%2073%20kyr.pdf Cavitte, MGP, Parrenin, F, Ritz, C, Young, A, Van Liefferinge, B, Blankenship, DD, Frezzotti, M and Roberts, JL 2018 , 'Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr' , Cryosphere, vol. 12, no. 4 , pp. 1401-1414 , doi:10.5194/tc-12-1401-2018 <http://dx.doi.org/10.5194/tc-12-1401-2018>. Dome C Antarctica ice core Article PeerReviewed 2018 ftunivtasmania https://doi.org/10.5194/tc-12-1401-2018 2021-09-13T22:19:30Z We reconstruct the pattern of surface accumulation in the region around Dome C, East Antarctica, since the last glacial. We use a set of 18 isochrones spanning all observable depths of the ice column, interpreted from various ice-penetrating radar surveys and a 1-D ice flow model to invert for accumulation rates in the region. The shallowest four isochrones are then used to calculate paleoaccumulation rates between isochrone pairs using a 1-D assumption where horizontal advection is negligible in the time interval of each layer. We observe that the large-scale (100skm) surface accumulation gradient is spatially stable through the last 73kyr, which reflects current modeled and observed precipitation gradients in the region. We also observe small-scale (10skm) accumulation variations linked to snow redistribution at the surface, due to changes in its slope and curvature in the prevailing wind direction that remain spatially stationary since the last glacial. Article in Journal/Newspaper Antarc* Antarctica East Antarctica ice core University of Tasmania: UTas ePrints East Antarctica The Cryosphere 12 4 1401 1414
institution Open Polar
collection University of Tasmania: UTas ePrints
op_collection_id ftunivtasmania
language English
topic Dome C
Antarctica
ice core
spellingShingle Dome C
Antarctica
ice core
Cavitte, MGP
Parrenin, F
Ritz, C
Young, A
Van Liefferinge, B
Blankenship, DD
Frezzotti, M
Roberts, JL
Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr
topic_facet Dome C
Antarctica
ice core
description We reconstruct the pattern of surface accumulation in the region around Dome C, East Antarctica, since the last glacial. We use a set of 18 isochrones spanning all observable depths of the ice column, interpreted from various ice-penetrating radar surveys and a 1-D ice flow model to invert for accumulation rates in the region. The shallowest four isochrones are then used to calculate paleoaccumulation rates between isochrone pairs using a 1-D assumption where horizontal advection is negligible in the time interval of each layer. We observe that the large-scale (100skm) surface accumulation gradient is spatially stable through the last 73kyr, which reflects current modeled and observed precipitation gradients in the region. We also observe small-scale (10skm) accumulation variations linked to snow redistribution at the surface, due to changes in its slope and curvature in the prevailing wind direction that remain spatially stationary since the last glacial.
format Article in Journal/Newspaper
author Cavitte, MGP
Parrenin, F
Ritz, C
Young, A
Van Liefferinge, B
Blankenship, DD
Frezzotti, M
Roberts, JL
author_facet Cavitte, MGP
Parrenin, F
Ritz, C
Young, A
Van Liefferinge, B
Blankenship, DD
Frezzotti, M
Roberts, JL
author_sort Cavitte, MGP
title Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr
title_short Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr
title_full Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr
title_fullStr Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr
title_full_unstemmed Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr
title_sort accumulation patterns around dome c, east antarctica, in the last 73 kyr
publisher Copernicus GmbH
publishDate 2018
url https://eprints.utas.edu.au/29936/
https://eprints.utas.edu.au/29936/1/131769%20-%20Accumulation%20patterns%20around%20Dome%20C,%20East%20Antarctica,%20in%20the%20last%2073%20kyr.pdf
geographic East Antarctica
geographic_facet East Antarctica
genre Antarc*
Antarctica
East Antarctica
ice core
genre_facet Antarc*
Antarctica
East Antarctica
ice core
op_relation https://eprints.utas.edu.au/29936/1/131769%20-%20Accumulation%20patterns%20around%20Dome%20C,%20East%20Antarctica,%20in%20the%20last%2073%20kyr.pdf
Cavitte, MGP, Parrenin, F, Ritz, C, Young, A, Van Liefferinge, B, Blankenship, DD, Frezzotti, M and Roberts, JL 2018 , 'Accumulation patterns around Dome C, East Antarctica, in the last 73 kyr' , Cryosphere, vol. 12, no. 4 , pp. 1401-1414 , doi:10.5194/tc-12-1401-2018 <http://dx.doi.org/10.5194/tc-12-1401-2018>.
op_doi https://doi.org/10.5194/tc-12-1401-2018
container_title The Cryosphere
container_volume 12
container_issue 4
container_start_page 1401
op_container_end_page 1414
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