The hydrostatic control of load-induced height changes above subglacial Lake Vostok
Lake Vostok, East Antarctica, represents an extensive water surface at the base of the ice sheet. Snow, ice and atmospheric pressure loads applied anywhere within the lake area produce a hydrostatic response, involving deformations of the ice surface, ice–water interface and particle horizons. A mod...
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2022
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ftdoajarticles:oai:doaj.org/article:75ee611a875f48ae811a11ebf362bc48 2023-05-15T13:52:30+02:00 The hydrostatic control of load-induced height changes above subglacial Lake Vostok Andreas Richter Ludwig Schröder Mirko Scheinert Sergey V. Popov Andreas Groh Matthias Willen Martin Horwath Reinhard Dietrich 2022-10-01T00:00:00Z https://doi.org/10.1017/jog.2022.2 https://doaj.org/article/75ee611a875f48ae811a11ebf362bc48 EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143022000028/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.2 0022-1430 1727-5652 https://doaj.org/article/75ee611a875f48ae811a11ebf362bc48 Journal of Glaciology, Vol 68, Pp 849-866 (2022) Ice dynamics laser altimetry subglacial lakes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2022 ftdoajarticles https://doi.org/10.1017/jog.2022.2 2023-03-12T01:30:54Z Lake Vostok, East Antarctica, represents an extensive water surface at the base of the ice sheet. Snow, ice and atmospheric pressure loads applied anywhere within the lake area produce a hydrostatic response, involving deformations of the ice surface, ice–water interface and particle horizons. A modelling scheme is developed to derive height changes of these surfaces for a given load pattern. It is applied to a series of load scenarios, and predictions based on load fields derived from a regional climate model are compared to observational datasets. Our results show that surface height changes due to snow-buildup anomalies are damped over the lake area, reducing the spatial standard deviation by one-third. The response to air pressure variations, in turn, adds surface height variability. Atmospheric pressure loads may produce height changes of up to $\pm$4 cm at daily resolution, but decay rapidly with integration time. The hydrostatic load response has no significant impact neither on ICESat laser campaign biases determined over the lake area nor on vertical particle movements derived from GNSS observations. Article in Journal/Newspaper Antarc* Antarctica East Antarctica Ice Sheet Journal of Glaciology Directory of Open Access Journals: DOAJ Articles East Antarctica Lake Vostok ENVELOPE(106.000,106.000,-77.500,-77.500) Journal of Glaciology 1 18 |
institution |
Open Polar |
collection |
Directory of Open Access Journals: DOAJ Articles |
op_collection_id |
ftdoajarticles |
language |
English |
topic |
Ice dynamics laser altimetry subglacial lakes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
spellingShingle |
Ice dynamics laser altimetry subglacial lakes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 Andreas Richter Ludwig Schröder Mirko Scheinert Sergey V. Popov Andreas Groh Matthias Willen Martin Horwath Reinhard Dietrich The hydrostatic control of load-induced height changes above subglacial Lake Vostok |
topic_facet |
Ice dynamics laser altimetry subglacial lakes Environmental sciences GE1-350 Meteorology. Climatology QC851-999 |
description |
Lake Vostok, East Antarctica, represents an extensive water surface at the base of the ice sheet. Snow, ice and atmospheric pressure loads applied anywhere within the lake area produce a hydrostatic response, involving deformations of the ice surface, ice–water interface and particle horizons. A modelling scheme is developed to derive height changes of these surfaces for a given load pattern. It is applied to a series of load scenarios, and predictions based on load fields derived from a regional climate model are compared to observational datasets. Our results show that surface height changes due to snow-buildup anomalies are damped over the lake area, reducing the spatial standard deviation by one-third. The response to air pressure variations, in turn, adds surface height variability. Atmospheric pressure loads may produce height changes of up to $\pm$4 cm at daily resolution, but decay rapidly with integration time. The hydrostatic load response has no significant impact neither on ICESat laser campaign biases determined over the lake area nor on vertical particle movements derived from GNSS observations. |
format |
Article in Journal/Newspaper |
author |
Andreas Richter Ludwig Schröder Mirko Scheinert Sergey V. Popov Andreas Groh Matthias Willen Martin Horwath Reinhard Dietrich |
author_facet |
Andreas Richter Ludwig Schröder Mirko Scheinert Sergey V. Popov Andreas Groh Matthias Willen Martin Horwath Reinhard Dietrich |
author_sort |
Andreas Richter |
title |
The hydrostatic control of load-induced height changes above subglacial Lake Vostok |
title_short |
The hydrostatic control of load-induced height changes above subglacial Lake Vostok |
title_full |
The hydrostatic control of load-induced height changes above subglacial Lake Vostok |
title_fullStr |
The hydrostatic control of load-induced height changes above subglacial Lake Vostok |
title_full_unstemmed |
The hydrostatic control of load-induced height changes above subglacial Lake Vostok |
title_sort |
hydrostatic control of load-induced height changes above subglacial lake vostok |
publisher |
Cambridge University Press |
publishDate |
2022 |
url |
https://doi.org/10.1017/jog.2022.2 https://doaj.org/article/75ee611a875f48ae811a11ebf362bc48 |
long_lat |
ENVELOPE(106.000,106.000,-77.500,-77.500) |
geographic |
East Antarctica Lake Vostok |
geographic_facet |
East Antarctica Lake Vostok |
genre |
Antarc* Antarctica East Antarctica Ice Sheet Journal of Glaciology |
genre_facet |
Antarc* Antarctica East Antarctica Ice Sheet Journal of Glaciology |
op_source |
Journal of Glaciology, Vol 68, Pp 849-866 (2022) |
op_relation |
https://www.cambridge.org/core/product/identifier/S0022143022000028/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2022.2 0022-1430 1727-5652 https://doaj.org/article/75ee611a875f48ae811a11ebf362bc48 |
op_doi |
https://doi.org/10.1017/jog.2022.2 |
container_title |
Journal of Glaciology |
container_start_page |
1 |
op_container_end_page |
18 |
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1766256786861457408 |