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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Bibliographic Details
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:
WEST ANTARCTICA
GROUNDING-LINE
SHEET
STAGNATION
SURFACE
CRYOSAT-2
ELEVATION
MELTWATER
SHELVES
RADAR
West Antarctica
Ross Ice Shelf
Kamb Ice Stream
Antarc*
Antarctica
Ice Shelf
Online Access:https://hdl.handle.net/10371/117522
https://doi.org/10.5194/tc-10-2971-2016
Description
Summary: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

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