Research output: Contribution to journal › Article › peer-review
Vast ice depression in Dålk Glacier, East Antarctica. / Popov, S. V.; Pryakhin, S. S.; Bliakharskii, D. P.; Pryakhina, G. V.; Tyurin, S. V.
In: Led i Sneg, Vol. 57, No. 3, 01.01.2017, p. 427-432.Research output: Contribution to journal › Article › peer-review
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TY - JOUR
T1 - Vast ice depression in Dålk Glacier, East Antarctica
AU - Popov, S. V.
AU - Pryakhin, S. S.
AU - Bliakharskii, D. P.
AU - Pryakhina, G. V.
AU - Tyurin, S. V.
PY - 2017/1/1
Y1 - 2017/1/1
N2 - In the afternoon of January 30, 2017, the wide depression in the western part of the Dålk Glacier, East Antarctica, was formed. By coincidence, aerial surveying was carried out in this area, so it is possible to assess the extent of this catastrophic phenomenon. Aerial photos were taken on January 20 and February 9, 2017, respectively. Based on the photographic data, the size of the depression were 183 × 220 m, and its area reached 40.260 m2. The depth of the depression in the early days was 20-30 meters; the maximum measured depth was 43 m. An approximate volume of the cavern was about 884, 013 m3. On preliminary conclusions, this event should be the similar jokulhlaups, when the water of Boulder Lake broke the icy border and rushed downstream under Dålk Glacier to Prudz Bay.
AB - In the afternoon of January 30, 2017, the wide depression in the western part of the Dålk Glacier, East Antarctica, was formed. By coincidence, aerial surveying was carried out in this area, so it is possible to assess the extent of this catastrophic phenomenon. Aerial photos were taken on January 20 and February 9, 2017, respectively. Based on the photographic data, the size of the depression were 183 × 220 m, and its area reached 40.260 m2. The depth of the depression in the early days was 20-30 meters; the maximum measured depth was 43 m. An approximate volume of the cavern was about 884, 013 m3. On preliminary conclusions, this event should be the similar jokulhlaups, when the water of Boulder Lake broke the icy border and rushed downstream under Dålk Glacier to Prudz Bay.
KW - Antarctic glaciology
KW - Glacier hydrology
KW - Jokulhlaups
KW - Subglacial processes
KW - Subglacier floods
UR - http://www.scopus.com/inward/record.url?scp=85032475095&partnerID=8YFLogxK
U2 - 10.15356/2076-6734-2017-3-427-432
DO - 10.15356/2076-6734-2017-3-427-432
M3 - Article
AN - SCOPUS:85032475095
VL - 57
SP - 427
EP - 432
JO - Лед и Снег
JF - Лед и Снег
SN - 2076-6734
IS - 3
ER -
ID: 35985840