Subglacial Lake Vostok not expected to discharge water

The question whether Antarctica's largest lake, subglacial Lake Vostok, exchanges water is of interdisciplinary relevance but has been undecided so far. We present the potential pathway, outlet location, and threshold height of subglacial water discharge from this lake based on a quantitative e...

Ausführliche Beschreibung

Gespeichert in:
Bibliographische Detailangaben
Veröffentlicht in:Geophysical research letters 2014-10, Vol.41 (19), p.6772-6778
Hauptverfasser: Richter, Andreas, Popov, Sergey V., Schröder, Ludwig, Schwabe, Joachim, Ewert, Heiko, Scheinert, Mirko, Horwath, Martin, Dietrich, Reinhard
Format: Artikel
Sprache:eng
Schlagworte:
Online-Zugang:Volltext
Tags: Tag hinzufügen
Keine Tags, Fügen Sie den ersten Tag hinzu!
container_end_page 6778
container_issue 19
container_start_page 6772
container_title Geophysical research letters
container_volume 41
creator Richter, Andreas
Popov, Sergey V.
Schröder, Ludwig
Schwabe, Joachim
Ewert, Heiko
Scheinert, Mirko
Horwath, Martin
Dietrich, Reinhard
description The question whether Antarctica's largest lake, subglacial Lake Vostok, exchanges water is of interdisciplinary relevance but has been undecided so far. We present the potential pathway, outlet location, and threshold height of subglacial water discharge from this lake based on a quantitative evaluation of the fluid potential. If water left Lake Vostok, it would flow toward Ross Ice Shelf. Discharge would occur first to the east of the southern tip of the lake. At this location the bedrock threshold is 91 ± 23 m higher than the hydrostatic equipotential level of Lake Vostok. It is concluded that Lake Vostok is not likely to reach this level within climatic timescales and that no discharge of liquid water is to be expected. We show that in absence of the ice sheet the Lake Vostok depression would harbor a lake significantly deeper and larger than the present aquifer. Key Points Lake Vostok is not expected to discharge liquid water in climatic timescalesDischarge would lead from east of the lake's southern tip to Ross Ice ShelfLake Vostok would be significantly deeper and larger without ice sheet
doi_str_mv 10.1002/2014GL061433
format Article
fullrecord <record><control><sourceid>proquest_cross</sourceid><recordid>TN_cdi_proquest_miscellaneous_1642228103</recordid><sourceformat>XML</sourceformat><sourcesystem>PC</sourcesystem><sourcerecordid>4308963051</sourcerecordid><originalsourceid>FETCH-LOGICAL-a4617-a14f59d31f86b7b020f72ca52874a47db699dedc93f0b3e5b38df02f945035ef3</originalsourceid><addsrcrecordid>eNqN0clOwzAQBmALgURZbjxAJC4cCMzYjpcjQlCWCFDZjpaT2BAammKnAt6elCKEOCBOnsM3_3g0hGwh7CEA3aeAfJiDQM7YEhmg5jxVAHKZDAB0X1MpVslajE8AwIDhgIjrWfHQ2LK2TZLbsUvu2ti142TSdol7m7qyc1XStUlVx_LRhgeXvNrOhQ2y4m0T3ebXu05uj49uDk_S_HJ4eniQp5YLlKlF7jNdMfRKFLIACl7S0mZUSW65rAqhdeWqUjMPBXNZwVTlgXrNM2CZ82yd7Cxyp6F9mbnYmef-I65p7MS1s2hQcEqpQmD_oKwP5UhlT7d_0ad2Fib9IgY1gs40SPWnUoIiMsXnWbsLVYY2xuC8mYb62YZ3g2DmVzE_r9JzuuCvdePe_7RmOMozip8z0kVTHTv39t1kw9gIyWRm7i-GRl3Rs3O8uDMj9gElIJjH</addsrcrecordid><sourcetype>Aggregation Database</sourcetype><iscdi>true</iscdi><recordtype>article</recordtype><pqid>1862113847</pqid></control><display><type>article</type><title>Subglacial Lake Vostok not expected to discharge water</title><source>Wiley Online Library Journals Frontfile Complete</source><source>Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals</source><source>Wiley Free Content</source><source>Wiley-Blackwell AGU Digital Library</source><creator>Richter, Andreas ; Popov, Sergey V. ; Schröder, Ludwig ; Schwabe, Joachim ; Ewert, Heiko ; Scheinert, Mirko ; Horwath, Martin ; Dietrich, Reinhard</creator><creatorcontrib>Richter, Andreas ; Popov, Sergey V. ; Schröder, Ludwig ; Schwabe, Joachim ; Ewert, Heiko ; Scheinert, Mirko ; Horwath, Martin ; Dietrich, Reinhard</creatorcontrib><description>The question whether Antarctica's largest lake, subglacial Lake Vostok, exchanges water is of interdisciplinary relevance but has been undecided so far. We present the potential pathway, outlet location, and threshold height of subglacial water discharge from this lake based on a quantitative evaluation of the fluid potential. If water left Lake Vostok, it would flow toward Ross Ice Shelf. Discharge would occur first to the east of the southern tip of the lake. At this location the bedrock threshold is 91 ± 23 m higher than the hydrostatic equipotential level of Lake Vostok. It is concluded that Lake Vostok is not likely to reach this level within climatic timescales and that no discharge of liquid water is to be expected. We show that in absence of the ice sheet the Lake Vostok depression would harbor a lake significantly deeper and larger than the present aquifer. Key Points Lake Vostok is not expected to discharge liquid water in climatic timescalesDischarge would lead from east of the lake's southern tip to Ross Ice ShelfLake Vostok would be significantly deeper and larger without ice sheet</description><identifier>ISSN: 0094-8276</identifier><identifier>EISSN: 1944-8007</identifier><identifier>DOI: 10.1002/2014GL061433</identifier><language>eng</language><publisher>Washington: Blackwell Publishing Ltd</publisher><subject>Antarctica ; Aquifers ; Bedrock ; Climate ; Discharge ; Evaluation ; Exchanging ; Geologic depressions ; Geophysics ; Glaciation ; glaciology ; Groundwater discharge ; Harbors ; Height ; Ice ; Ice sheets ; Ice shelves ; Lake ice ; Lakes ; Land ice ; Quantitative analysis ; Ross ice shelf ; subglacial hydrology ; subglacial lake ; Subglacial water ; Thresholds ; Water ; Water discharge</subject><ispartof>Geophysical research letters, 2014-10, Vol.41 (19), p.6772-6778</ispartof><rights>2014. American Geophysical Union. All Rights Reserved.</rights><lds50>peer_reviewed</lds50><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a4617-a14f59d31f86b7b020f72ca52874a47db699dedc93f0b3e5b38df02f945035ef3</citedby><cites>FETCH-LOGICAL-a4617-a14f59d31f86b7b020f72ca52874a47db699dedc93f0b3e5b38df02f945035ef3</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://onlinelibrary.wiley.com/doi/pdf/10.1002%2F2014GL061433$$EPDF$$P50$$Gwiley$$H</linktopdf><linktohtml>$$Uhttps://onlinelibrary.wiley.com/doi/full/10.1002%2F2014GL061433$$EHTML$$P50$$Gwiley$$H</linktohtml><link.rule.ids>314,776,780,1411,1427,11494,27903,27904,45553,45554,46387,46446,46811,46870</link.rule.ids></links><search><creatorcontrib>Richter, Andreas</creatorcontrib><creatorcontrib>Popov, Sergey V.</creatorcontrib><creatorcontrib>Schröder, Ludwig</creatorcontrib><creatorcontrib>Schwabe, Joachim</creatorcontrib><creatorcontrib>Ewert, Heiko</creatorcontrib><creatorcontrib>Scheinert, Mirko</creatorcontrib><creatorcontrib>Horwath, Martin</creatorcontrib><creatorcontrib>Dietrich, Reinhard</creatorcontrib><title>Subglacial Lake Vostok not expected to discharge water</title><title>Geophysical research letters</title><addtitle>Geophys. Res. Lett</addtitle><description>The question whether Antarctica's largest lake, subglacial Lake Vostok, exchanges water is of interdisciplinary relevance but has been undecided so far. We present the potential pathway, outlet location, and threshold height of subglacial water discharge from this lake based on a quantitative evaluation of the fluid potential. If water left Lake Vostok, it would flow toward Ross Ice Shelf. Discharge would occur first to the east of the southern tip of the lake. At this location the bedrock threshold is 91 ± 23 m higher than the hydrostatic equipotential level of Lake Vostok. It is concluded that Lake Vostok is not likely to reach this level within climatic timescales and that no discharge of liquid water is to be expected. We show that in absence of the ice sheet the Lake Vostok depression would harbor a lake significantly deeper and larger than the present aquifer. Key Points Lake Vostok is not expected to discharge liquid water in climatic timescalesDischarge would lead from east of the lake's southern tip to Ross Ice ShelfLake Vostok would be significantly deeper and larger without ice sheet</description><subject>Antarctica</subject><subject>Aquifers</subject><subject>Bedrock</subject><subject>Climate</subject><subject>Discharge</subject><subject>Evaluation</subject><subject>Exchanging</subject><subject>Geologic depressions</subject><subject>Geophysics</subject><subject>Glaciation</subject><subject>glaciology</subject><subject>Groundwater discharge</subject><subject>Harbors</subject><subject>Height</subject><subject>Ice</subject><subject>Ice sheets</subject><subject>Ice shelves</subject><subject>Lake ice</subject><subject>Lakes</subject><subject>Land ice</subject><subject>Quantitative analysis</subject><subject>Ross ice shelf</subject><subject>subglacial hydrology</subject><subject>subglacial lake</subject><subject>Subglacial water</subject><subject>Thresholds</subject><subject>Water</subject><subject>Water discharge</subject><issn>0094-8276</issn><issn>1944-8007</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2014</creationdate><recordtype>article</recordtype><recordid>eNqN0clOwzAQBmALgURZbjxAJC4cCMzYjpcjQlCWCFDZjpaT2BAammKnAt6elCKEOCBOnsM3_3g0hGwh7CEA3aeAfJiDQM7YEhmg5jxVAHKZDAB0X1MpVslajE8AwIDhgIjrWfHQ2LK2TZLbsUvu2ti142TSdol7m7qyc1XStUlVx_LRhgeXvNrOhQ2y4m0T3ebXu05uj49uDk_S_HJ4eniQp5YLlKlF7jNdMfRKFLIACl7S0mZUSW65rAqhdeWqUjMPBXNZwVTlgXrNM2CZ82yd7Cxyp6F9mbnYmef-I65p7MS1s2hQcEqpQmD_oKwP5UhlT7d_0ad2Fib9IgY1gs40SPWnUoIiMsXnWbsLVYY2xuC8mYb62YZ3g2DmVzE_r9JzuuCvdePe_7RmOMozip8z0kVTHTv39t1kw9gIyWRm7i-GRl3Rs3O8uDMj9gElIJjH</recordid><startdate>20141016</startdate><enddate>20141016</enddate><creator>Richter, Andreas</creator><creator>Popov, Sergey V.</creator><creator>Schröder, Ludwig</creator><creator>Schwabe, Joachim</creator><creator>Ewert, Heiko</creator><creator>Scheinert, Mirko</creator><creator>Horwath, Martin</creator><creator>Dietrich, Reinhard</creator><general>Blackwell Publishing Ltd</general><general>John Wiley &amp; Sons, Inc</general><scope>BSCLL</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TG</scope><scope>7TN</scope><scope>8FD</scope><scope>F1W</scope><scope>FR3</scope><scope>H8D</scope><scope>H96</scope><scope>KL.</scope><scope>KR7</scope><scope>L.G</scope><scope>L7M</scope><scope>7QH</scope><scope>7UA</scope><scope>C1K</scope></search><sort><creationdate>20141016</creationdate><title>Subglacial Lake Vostok not expected to discharge water</title><author>Richter, Andreas ; Popov, Sergey V. ; Schröder, Ludwig ; Schwabe, Joachim ; Ewert, Heiko ; Scheinert, Mirko ; Horwath, Martin ; Dietrich, Reinhard</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a4617-a14f59d31f86b7b020f72ca52874a47db699dedc93f0b3e5b38df02f945035ef3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2014</creationdate><topic>Antarctica</topic><topic>Aquifers</topic><topic>Bedrock</topic><topic>Climate</topic><topic>Discharge</topic><topic>Evaluation</topic><topic>Exchanging</topic><topic>Geologic depressions</topic><topic>Geophysics</topic><topic>Glaciation</topic><topic>glaciology</topic><topic>Groundwater discharge</topic><topic>Harbors</topic><topic>Height</topic><topic>Ice</topic><topic>Ice sheets</topic><topic>Ice shelves</topic><topic>Lake ice</topic><topic>Lakes</topic><topic>Land ice</topic><topic>Quantitative analysis</topic><topic>Ross ice shelf</topic><topic>subglacial hydrology</topic><topic>subglacial lake</topic><topic>Subglacial water</topic><topic>Thresholds</topic><topic>Water</topic><topic>Water discharge</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Richter, Andreas</creatorcontrib><creatorcontrib>Popov, Sergey V.</creatorcontrib><creatorcontrib>Schröder, Ludwig</creatorcontrib><creatorcontrib>Schwabe, Joachim</creatorcontrib><creatorcontrib>Ewert, Heiko</creatorcontrib><creatorcontrib>Scheinert, Mirko</creatorcontrib><creatorcontrib>Horwath, Martin</creatorcontrib><creatorcontrib>Dietrich, Reinhard</creatorcontrib><collection>Istex</collection><collection>CrossRef</collection><collection>Meteorological &amp; Geoastrophysical Abstracts</collection><collection>Oceanic Abstracts</collection><collection>Technology Research Database</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Engineering Research Database</collection><collection>Aerospace Database</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy &amp; Non-Living Resources</collection><collection>Meteorological &amp; Geoastrophysical Abstracts - Academic</collection><collection>Civil Engineering Abstracts</collection><collection>Aquatic Science &amp; Fisheries Abstracts (ASFA) Professional</collection><collection>Advanced Technologies Database with Aerospace</collection><collection>Aqualine</collection><collection>Water Resources Abstracts</collection><collection>Environmental Sciences and Pollution Management</collection><jtitle>Geophysical research letters</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Richter, Andreas</au><au>Popov, Sergey V.</au><au>Schröder, Ludwig</au><au>Schwabe, Joachim</au><au>Ewert, Heiko</au><au>Scheinert, Mirko</au><au>Horwath, Martin</au><au>Dietrich, Reinhard</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Subglacial Lake Vostok not expected to discharge water</atitle><jtitle>Geophysical research letters</jtitle><addtitle>Geophys. Res. Lett</addtitle><date>2014-10-16</date><risdate>2014</risdate><volume>41</volume><issue>19</issue><spage>6772</spage><epage>6778</epage><pages>6772-6778</pages><issn>0094-8276</issn><eissn>1944-8007</eissn><abstract>The question whether Antarctica's largest lake, subglacial Lake Vostok, exchanges water is of interdisciplinary relevance but has been undecided so far. We present the potential pathway, outlet location, and threshold height of subglacial water discharge from this lake based on a quantitative evaluation of the fluid potential. If water left Lake Vostok, it would flow toward Ross Ice Shelf. Discharge would occur first to the east of the southern tip of the lake. At this location the bedrock threshold is 91 ± 23 m higher than the hydrostatic equipotential level of Lake Vostok. It is concluded that Lake Vostok is not likely to reach this level within climatic timescales and that no discharge of liquid water is to be expected. We show that in absence of the ice sheet the Lake Vostok depression would harbor a lake significantly deeper and larger than the present aquifer. Key Points Lake Vostok is not expected to discharge liquid water in climatic timescalesDischarge would lead from east of the lake's southern tip to Ross Ice ShelfLake Vostok would be significantly deeper and larger without ice sheet</abstract><cop>Washington</cop><pub>Blackwell Publishing Ltd</pub><doi>10.1002/2014GL061433</doi><tpages>7</tpages></addata></record>
fulltext fulltext
identifier ISSN: 0094-8276
ispartof Geophysical research letters, 2014-10, Vol.41 (19), p.6772-6778
issn 0094-8276
1944-8007
language eng
recordid cdi_proquest_miscellaneous_1642228103
source Wiley Online Library Journals Frontfile Complete; Elektronische Zeitschriftenbibliothek - Frei zugängliche E-Journals; Wiley Free Content; Wiley-Blackwell AGU Digital Library
subjects Antarctica
Aquifers
Bedrock
Climate
Discharge
Evaluation
Exchanging
Geologic depressions
Geophysics
Glaciation
glaciology
Groundwater discharge
Harbors
Height
Ice
Ice sheets
Ice shelves
Lake ice
Lakes
Land ice
Quantitative analysis
Ross ice shelf
subglacial hydrology
subglacial lake
Subglacial water
Thresholds
Water
Water discharge
title Subglacial Lake Vostok not expected to discharge water
url https://sfx.bib-bvb.de/sfx_tum?ctx_ver=Z39.88-2004&ctx_enc=info:ofi/enc:UTF-8&ctx_tim=2025-01-25T21%3A17%3A55IST&url_ver=Z39.88-2004&url_ctx_fmt=infofi/fmt:kev:mtx:ctx&rfr_id=info:sid/primo.exlibrisgroup.com:primo3-Article-proquest_cross&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.genre=article&rft.atitle=Subglacial%20Lake%20Vostok%20not%20expected%20to%20discharge%20water&rft.jtitle=Geophysical%20research%20letters&rft.au=Richter,%20Andreas&rft.date=2014-10-16&rft.volume=41&rft.issue=19&rft.spage=6772&rft.epage=6778&rft.pages=6772-6778&rft.issn=0094-8276&rft.eissn=1944-8007&rft_id=info:doi/10.1002/2014GL061433&rft_dat=%3Cproquest_cross%3E4308963051%3C/proquest_cross%3E%3Curl%3E%3C/url%3E&disable_directlink=true&sfx.directlink=off&sfx.report_link=0&rft_id=info:oai/&rft_pqid=1862113847&rft_id=info:pmid/&rfr_iscdi=true