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...

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Published in:The Cryosphere
Main Authors: 서기원, Kim, Byeong-Hoon, Lee, Choon-Ki, Seo, Ki-Weon, Lee, Won Sang, Scambos, Ted
Other Authors: 김병훈, 이춘기, 이원상
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Group 2018
Subjects:
Online Access:https://hdl.handle.net/10371/117522
https://doi.org/10.5194/tc-10-2971-2016
id ftseoulnuniv:oai:s-space.snu.ac.kr:10371/117522
record_format openpolar
spelling 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
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