Active subglacial lakes and channelized water flow beneath the Kamb Ice Stream
We identify two previously unknown subglacial lakes beneath the stagnated trunk of the Kamb Ice Stream (KIS). Rapid fill-drain hydrologic events over several months are inferred from surface height changes measured by CryoSat-2 altimetry and indicate that the lakes are probably connected by a subgla...
Published in: | The Cryosphere |
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Language: | English |
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2018
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Online Access: | https://hdl.handle.net/10371/117522 https://doi.org/10.5194/tc-10-2971-2016 |
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ftseoulnuniv:oai:s-space.snu.ac.kr:10371/117522 2024-01-14T09:59:27+01:00 Active subglacial lakes and channelized water flow beneath the Kamb Ice Stream 서기원 Kim, Byeong-Hoon Lee, Choon-Ki Seo, Ki-Weon Lee, Won Sang Scambos, Ted 김병훈 이춘기 서기원 이원상 Seo, Ki-Weon 2018-08-20 https://hdl.handle.net/10371/117522 https://doi.org/10.5194/tc-10-2971-2016 영어 en eng Copernicus Group Cryosphere, Vol.10 No.6, pp.2971-2980 1994-0416 https://hdl.handle.net/10371/117522 doi:10.5194/tc-10-2971-2016 000389217700002 2-s2.0-85002615610 44802 T201501631 WEST ANTARCTICA GROUNDING-LINE SHEET STAGNATION SURFACE CRYOSAT-2 ELEVATION MELTWATER SHELVES RADAR Article ART 2018 ftseoulnuniv https://doi.org/10.5194/tc-10-2971-2016 2023-12-15T01:38:15Z We identify two previously unknown subglacial lakes beneath the stagnated trunk of the Kamb Ice Stream (KIS). Rapid fill-drain hydrologic events over several months are inferred from surface height changes measured by CryoSat-2 altimetry and indicate that the lakes are probably connected by a subglacial drainage network, whose structure is inferred from the regional hydraulic potential and probably links the lakes. The sequential fill-drain behavior of the subglacial lakes and concurrent rapid thinning in a channel-like topographic feature near the grounding line implies that the subglacial water repeatedly flows from the region above the trunk to the KIS grounding line and out beneath the Ross Ice Shelf. Ice shelf elevation near the hypothesized outlet is observed to decrease slowly during the study period. Our finding supports a previously published conceptual model of the KIS shutdown stemming from a transition from distributed flow to well-drained channelized flow of subglacial water. However, a water-piracy hypothesis in which the KIS subglacial water system is being starved by drainage in adjacent ice streams is also supported by the fact that the degree of KIS trunk subglacial lake activity is relatively weaker than those of the upstream lakes. OAIID:RECH_ACHV_DSTSH_NO:T201501631 RECH_ACHV_FG:RR00200001 ADJUST_YN: EMP_ID:A079127 CITE_RATE:4.906 FILENAME:2016_Kim_TC.pdf DEPT_NM:지구과학교육과 EMAIL:seokiweon@snu.ac.kr SCOPUS_YN:Y FILEURL:https://srnd.snu.ac.kr/eXrepEIR/fws/file/0f782ccb-87d7-4af5-89fc-9ed5599fd0f7/link CONFIRM:Y Y 1 Article in Journal/Newspaper Antarc* Antarctica Ice Shelf Kamb Ice Stream Ross Ice Shelf West Antarctica Seoul National University: S-Space West Antarctica Ross Ice Shelf Kamb Ice Stream ENVELOPE(-145.000,-145.000,-82.250,-82.250) The Cryosphere 10 6 2971 2980 |
institution |
Open Polar |
collection |
Seoul National University: S-Space |
op_collection_id |
ftseoulnuniv |
language |
English |
topic |
WEST ANTARCTICA GROUNDING-LINE SHEET STAGNATION SURFACE CRYOSAT-2 ELEVATION MELTWATER SHELVES RADAR |
spellingShingle |
WEST ANTARCTICA GROUNDING-LINE SHEET STAGNATION SURFACE CRYOSAT-2 ELEVATION MELTWATER SHELVES RADAR 서기원 Kim, Byeong-Hoon Lee, Choon-Ki Seo, Ki-Weon Lee, Won Sang Scambos, Ted Active subglacial lakes and channelized water flow beneath the Kamb Ice Stream |
topic_facet |
WEST ANTARCTICA GROUNDING-LINE SHEET STAGNATION SURFACE CRYOSAT-2 ELEVATION MELTWATER SHELVES RADAR |
description |
We identify two previously unknown subglacial lakes beneath the stagnated trunk of the Kamb Ice Stream (KIS). Rapid fill-drain hydrologic events over several months are inferred from surface height changes measured by CryoSat-2 altimetry and indicate that the lakes are probably connected by a subglacial drainage network, whose structure is inferred from the regional hydraulic potential and probably links the lakes. The sequential fill-drain behavior of the subglacial lakes and concurrent rapid thinning in a channel-like topographic feature near the grounding line implies that the subglacial water repeatedly flows from the region above the trunk to the KIS grounding line and out beneath the Ross Ice Shelf. Ice shelf elevation near the hypothesized outlet is observed to decrease slowly during the study period. Our finding supports a previously published conceptual model of the KIS shutdown stemming from a transition from distributed flow to well-drained channelized flow of subglacial water. However, a water-piracy hypothesis in which the KIS subglacial water system is being starved by drainage in adjacent ice streams is also supported by the fact that the degree of KIS trunk subglacial lake activity is relatively weaker than those of the upstream lakes. OAIID:RECH_ACHV_DSTSH_NO:T201501631 RECH_ACHV_FG:RR00200001 ADJUST_YN: EMP_ID:A079127 CITE_RATE:4.906 FILENAME:2016_Kim_TC.pdf DEPT_NM:지구과학교육과 EMAIL:seokiweon@snu.ac.kr SCOPUS_YN:Y FILEURL:https://srnd.snu.ac.kr/eXrepEIR/fws/file/0f782ccb-87d7-4af5-89fc-9ed5599fd0f7/link CONFIRM:Y Y 1 |
author2 |
김병훈 이춘기 서기원 이원상 Seo, Ki-Weon |
format |
Article in Journal/Newspaper |
author |
서기원 Kim, Byeong-Hoon Lee, Choon-Ki Seo, Ki-Weon Lee, Won Sang Scambos, Ted |
author_facet |
서기원 Kim, Byeong-Hoon Lee, Choon-Ki Seo, Ki-Weon Lee, Won Sang Scambos, Ted |
author_sort |
서기원 |
title |
Active subglacial lakes and channelized water flow beneath the Kamb Ice Stream |
title_short |
Active subglacial lakes and channelized water flow beneath the Kamb Ice Stream |
title_full |
Active subglacial lakes and channelized water flow beneath the Kamb Ice Stream |
title_fullStr |
Active subglacial lakes and channelized water flow beneath the Kamb Ice Stream |
title_full_unstemmed |
Active subglacial lakes and channelized water flow beneath the Kamb Ice Stream |
title_sort |
active subglacial lakes and channelized water flow beneath the kamb ice stream |
publisher |
Copernicus Group |
publishDate |
2018 |
url |
https://hdl.handle.net/10371/117522 https://doi.org/10.5194/tc-10-2971-2016 |
long_lat |
ENVELOPE(-145.000,-145.000,-82.250,-82.250) |
geographic |
West Antarctica Ross Ice Shelf Kamb Ice Stream |
geographic_facet |
West Antarctica Ross Ice Shelf Kamb Ice Stream |
genre |
Antarc* Antarctica Ice Shelf Kamb Ice Stream Ross Ice Shelf West Antarctica |
genre_facet |
Antarc* Antarctica Ice Shelf Kamb Ice Stream Ross Ice Shelf West Antarctica |
op_relation |
Cryosphere, Vol.10 No.6, pp.2971-2980 1994-0416 https://hdl.handle.net/10371/117522 doi:10.5194/tc-10-2971-2016 000389217700002 2-s2.0-85002615610 44802 T201501631 |
op_doi |
https://doi.org/10.5194/tc-10-2971-2016 |
container_title |
The Cryosphere |
container_volume |
10 |
container_issue |
6 |
container_start_page |
2971 |
op_container_end_page |
2980 |
_version_ |
1788059161342246912 |