Formation of a large ice depression on Dålk Glacier (Larsemann Hills, East Antarctica) caused by the rapid drainage of an englacial cavity

In the afternoon of 30 January 2017, a catastrophic outburst flood occurred in the Larsemann Hills (Princess Elizabeth Land, East Antarctica). The rapid drainage of both a thin supraglacial layer of water (near Boulder Lake) and Lake Ledyanoe into the englacial Lake Dålk provoked its overfill and ou...

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Published in:Journal of Glaciology
Main Authors: Alina Boronina, Sergey Popov, Galina Pryakhina, Antonina Chetverova, Ekaterina Ryzhova, Svetlana Grigoreva
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press 2021
Subjects:
Online Access:https://doi.org/10.1017/jog.2021.58
https://doaj.org/article/80464d34a1534eb79eeccc786e52414a
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spelling ftdoajarticles:oai:doaj.org/article:80464d34a1534eb79eeccc786e52414a 2023-05-15T14:01:35+02:00 Formation of a large ice depression on Dålk Glacier (Larsemann Hills, East Antarctica) caused by the rapid drainage of an englacial cavity Alina Boronina Sergey Popov Galina Pryakhina Antonina Chetverova Ekaterina Ryzhova Svetlana Grigoreva 2021-12-01T00:00:00Z https://doi.org/10.1017/jog.2021.58 https://doaj.org/article/80464d34a1534eb79eeccc786e52414a EN eng Cambridge University Press https://www.cambridge.org/core/product/identifier/S0022143021000587/type/journal_article https://doaj.org/toc/0022-1430 https://doaj.org/toc/1727-5652 doi:10.1017/jog.2021.58 0022-1430 1727-5652 https://doaj.org/article/80464d34a1534eb79eeccc786e52414a Journal of Glaciology, Vol 67, Pp 1121-1136 (2021) Antarctic glaciology glacier hazards glacier hydrology glacier modelling ground-penetrating radar Environmental sciences GE1-350 Meteorology. Climatology QC851-999 article 2021 ftdoajarticles https://doi.org/10.1017/jog.2021.58 2023-03-12T01:30:57Z In the afternoon of 30 January 2017, a catastrophic outburst flood occurred in the Larsemann Hills (Princess Elizabeth Land, East Antarctica). The rapid drainage of both a thin supraglacial layer of water (near Boulder Lake) and Lake Ledyanoe into the englacial Lake Dålk provoked its overfill and outburst. As a result, a depression of 183 m × 220 m was formed in the place where Lake Dålk was located. This study summarises and clarifies the current state of knowledge on the flood that occurred in 2017. We present a phenomenological model of depression formation. We specify the reasons for the outburst of the system of lakes Boulder, Ledyanoe and Dålk. In addition, we carry out mathematical modelling of the outburst of each of the three lakes and estimate the flood severity. Outburst hydrographs, channel diameters, volume and duration of floods were calculated. Particular simulation results were validated with field data. In conclusion, we give an overview of the new outburst cycle of the lake system, which began in 2020 with the drainage of the lakes Boulder and Ledyanoe, and the new formation of Lake Dålk. Further research is required to improve our understanding of the lake system responses to changing external factors. Article in Journal/Newspaper Antarc* Antarctic Antarctica East Antarctica Journal of Glaciology Princess Elizabeth Land Directory of Open Access Journals: DOAJ Articles Antarctic East Antarctica Larsemann Hills ENVELOPE(76.217,76.217,-69.400,-69.400) Princess Elizabeth Land ENVELOPE(80.367,80.367,-68.500,-68.500) Dålk Glacier ENVELOPE(76.472,76.472,-69.426,-69.426) Boulder Lake ENVELOPE(76.391,76.391,-69.411,-69.411) Journal of Glaciology 67 266 1121 1136
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Antarctic glaciology
glacier hazards
glacier hydrology
glacier modelling
ground-penetrating radar
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
spellingShingle Antarctic glaciology
glacier hazards
glacier hydrology
glacier modelling
ground-penetrating radar
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
Alina Boronina
Sergey Popov
Galina Pryakhina
Antonina Chetverova
Ekaterina Ryzhova
Svetlana Grigoreva
Formation of a large ice depression on Dålk Glacier (Larsemann Hills, East Antarctica) caused by the rapid drainage of an englacial cavity
topic_facet Antarctic glaciology
glacier hazards
glacier hydrology
glacier modelling
ground-penetrating radar
Environmental sciences
GE1-350
Meteorology. Climatology
QC851-999
description In the afternoon of 30 January 2017, a catastrophic outburst flood occurred in the Larsemann Hills (Princess Elizabeth Land, East Antarctica). The rapid drainage of both a thin supraglacial layer of water (near Boulder Lake) and Lake Ledyanoe into the englacial Lake Dålk provoked its overfill and outburst. As a result, a depression of 183 m × 220 m was formed in the place where Lake Dålk was located. This study summarises and clarifies the current state of knowledge on the flood that occurred in 2017. We present a phenomenological model of depression formation. We specify the reasons for the outburst of the system of lakes Boulder, Ledyanoe and Dålk. In addition, we carry out mathematical modelling of the outburst of each of the three lakes and estimate the flood severity. Outburst hydrographs, channel diameters, volume and duration of floods were calculated. Particular simulation results were validated with field data. In conclusion, we give an overview of the new outburst cycle of the lake system, which began in 2020 with the drainage of the lakes Boulder and Ledyanoe, and the new formation of Lake Dålk. Further research is required to improve our understanding of the lake system responses to changing external factors.
format Article in Journal/Newspaper
author Alina Boronina
Sergey Popov
Galina Pryakhina
Antonina Chetverova
Ekaterina Ryzhova
Svetlana Grigoreva
author_facet Alina Boronina
Sergey Popov
Galina Pryakhina
Antonina Chetverova
Ekaterina Ryzhova
Svetlana Grigoreva
author_sort Alina Boronina
title Formation of a large ice depression on Dålk Glacier (Larsemann Hills, East Antarctica) caused by the rapid drainage of an englacial cavity
title_short Formation of a large ice depression on Dålk Glacier (Larsemann Hills, East Antarctica) caused by the rapid drainage of an englacial cavity
title_full Formation of a large ice depression on Dålk Glacier (Larsemann Hills, East Antarctica) caused by the rapid drainage of an englacial cavity
title_fullStr Formation of a large ice depression on Dålk Glacier (Larsemann Hills, East Antarctica) caused by the rapid drainage of an englacial cavity
title_full_unstemmed Formation of a large ice depression on Dålk Glacier (Larsemann Hills, East Antarctica) caused by the rapid drainage of an englacial cavity
title_sort formation of a large ice depression on dålk glacier (larsemann hills, east antarctica) caused by the rapid drainage of an englacial cavity
publisher Cambridge University Press
publishDate 2021
url https://doi.org/10.1017/jog.2021.58
https://doaj.org/article/80464d34a1534eb79eeccc786e52414a
long_lat ENVELOPE(76.217,76.217,-69.400,-69.400)
ENVELOPE(80.367,80.367,-68.500,-68.500)
ENVELOPE(76.472,76.472,-69.426,-69.426)
ENVELOPE(76.391,76.391,-69.411,-69.411)
geographic Antarctic
East Antarctica
Larsemann Hills
Princess Elizabeth Land
Dålk Glacier
Boulder Lake
geographic_facet Antarctic
East Antarctica
Larsemann Hills
Princess Elizabeth Land
Dålk Glacier
Boulder Lake
genre Antarc*
Antarctic
Antarctica
East Antarctica
Journal of Glaciology
Princess Elizabeth Land
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Journal of Glaciology
Princess Elizabeth Land
op_source Journal of Glaciology, Vol 67, Pp 1121-1136 (2021)
op_relation https://www.cambridge.org/core/product/identifier/S0022143021000587/type/journal_article
https://doaj.org/toc/0022-1430
https://doaj.org/toc/1727-5652
doi:10.1017/jog.2021.58
0022-1430
1727-5652
https://doaj.org/article/80464d34a1534eb79eeccc786e52414a
op_doi https://doi.org/10.1017/jog.2021.58
container_title Journal of Glaciology
container_volume 67
container_issue 266
container_start_page 1121
op_container_end_page 1136
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