Ice loss processes in the Seal Nunataks ice shelf region from satellite altimetry and imagery ...
The Seal Nunataks ice shelf (SNIS, ∼743 km² in 2013) is an unofficial name for a remnant area between the former Larsen A and Larsen B ice shelves off the northeastern Antarctic Peninsula. Analyses using Landsat 7 ETM+ and Terra ASTER images from 2001 to 13 and ICESat altimetry from 2003 to 09 show...
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Online Access: | https://dx.doi.org/10.13016/m28j8j-oywj https://mdsoar.org/handle/11603/24268 |
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ftdatacite:10.13016/m28j8j-oywj 2023-08-27T04:04:41+02:00 Ice loss processes in the Seal Nunataks ice shelf region from satellite altimetry and imagery ... Shuman, Christopher Scambos, Ted Berthier, Etienne 2016 https://dx.doi.org/10.13016/m28j8j-oywj https://mdsoar.org/handle/11603/24268 en eng Cambridge Core Creative Commons Attribution Non Commercial No Derivatives 4.0 International Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) This item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author. https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 CreativeWork article 2016 ftdatacite https://doi.org/10.13016/m28j8j-oywj 2023-08-07T14:24:23Z The Seal Nunataks ice shelf (SNIS, ∼743 km² in 2013) is an unofficial name for a remnant area between the former Larsen A and Larsen B ice shelves off the northeastern Antarctic Peninsula. Analyses using Landsat 7 ETM+ and Terra ASTER images from 2001 to 13 and ICESat altimetry from 2003 to 09 show it has retreated and thinned following the Larsen A (1995) and Larsen B (2002) disin tegrations. Despite some regional cooling and more fast ice since 2008, SNIS continues to lose ice along its margins and may be losing contact with some nunataks. Detailed analysis of data from four ICESat tracks indicates that ice shelf thinning rates range between 1.9 and 2.7 m a⁻¹ , and generally increase from west to east. An ICESat repeat track crossing the adjacent Robertson Island shows a mean elevation loss of 1.8 m a⁻¹. Two tracks crossing the SNIS’s remaining tributary, Rogosh Glacier, show sub-meter elevation losses. Comparing shelf remnant and grounded ice thinning rates implies that basal ocean melting augments SNIS ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Ice Shelf Ice Shelves Robertson Island DataCite Metadata Store (German National Library of Science and Technology) Antarctic Antarctic Peninsula Seal Nunataks ENVELOPE(-60.255,-60.255,-65.049,-65.049) Robertson Island ENVELOPE(-59.667,-59.667,-65.167,-65.167) Rogosh Glacier ENVELOPE(-61.317,-61.317,-64.917,-64.917) |
institution |
Open Polar |
collection |
DataCite Metadata Store (German National Library of Science and Technology) |
op_collection_id |
ftdatacite |
language |
English |
description |
The Seal Nunataks ice shelf (SNIS, ∼743 km² in 2013) is an unofficial name for a remnant area between the former Larsen A and Larsen B ice shelves off the northeastern Antarctic Peninsula. Analyses using Landsat 7 ETM+ and Terra ASTER images from 2001 to 13 and ICESat altimetry from 2003 to 09 show it has retreated and thinned following the Larsen A (1995) and Larsen B (2002) disin tegrations. Despite some regional cooling and more fast ice since 2008, SNIS continues to lose ice along its margins and may be losing contact with some nunataks. Detailed analysis of data from four ICESat tracks indicates that ice shelf thinning rates range between 1.9 and 2.7 m a⁻¹ , and generally increase from west to east. An ICESat repeat track crossing the adjacent Robertson Island shows a mean elevation loss of 1.8 m a⁻¹. Two tracks crossing the SNIS’s remaining tributary, Rogosh Glacier, show sub-meter elevation losses. Comparing shelf remnant and grounded ice thinning rates implies that basal ocean melting augments SNIS ... |
format |
Article in Journal/Newspaper |
author |
Shuman, Christopher Scambos, Ted Berthier, Etienne |
spellingShingle |
Shuman, Christopher Scambos, Ted Berthier, Etienne Ice loss processes in the Seal Nunataks ice shelf region from satellite altimetry and imagery ... |
author_facet |
Shuman, Christopher Scambos, Ted Berthier, Etienne |
author_sort |
Shuman, Christopher |
title |
Ice loss processes in the Seal Nunataks ice shelf region from satellite altimetry and imagery ... |
title_short |
Ice loss processes in the Seal Nunataks ice shelf region from satellite altimetry and imagery ... |
title_full |
Ice loss processes in the Seal Nunataks ice shelf region from satellite altimetry and imagery ... |
title_fullStr |
Ice loss processes in the Seal Nunataks ice shelf region from satellite altimetry and imagery ... |
title_full_unstemmed |
Ice loss processes in the Seal Nunataks ice shelf region from satellite altimetry and imagery ... |
title_sort |
ice loss processes in the seal nunataks ice shelf region from satellite altimetry and imagery ... |
publisher |
Cambridge Core |
publishDate |
2016 |
url |
https://dx.doi.org/10.13016/m28j8j-oywj https://mdsoar.org/handle/11603/24268 |
long_lat |
ENVELOPE(-60.255,-60.255,-65.049,-65.049) ENVELOPE(-59.667,-59.667,-65.167,-65.167) ENVELOPE(-61.317,-61.317,-64.917,-64.917) |
geographic |
Antarctic Antarctic Peninsula Seal Nunataks Robertson Island Rogosh Glacier |
geographic_facet |
Antarctic Antarctic Peninsula Seal Nunataks Robertson Island Rogosh Glacier |
genre |
Antarc* Antarctic Antarctic Peninsula Ice Shelf Ice Shelves Robertson Island |
genre_facet |
Antarc* Antarctic Antarctic Peninsula Ice Shelf Ice Shelves Robertson Island |
op_rights |
Creative Commons Attribution Non Commercial No Derivatives 4.0 International Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) This item is likely protected under Title 17 of the U.S. Copyright Law. Unless on a Creative Commons license, for uses protected by Copyright Law, contact the copyright holder or the author. https://creativecommons.org/licenses/by-nc-nd/4.0/legalcode cc-by-nc-nd-4.0 |
op_doi |
https://doi.org/10.13016/m28j8j-oywj |
_version_ |
1775352792471306240 |