Glacier surge as a trigger for the fastest delta growth in the
Arctic

J 2024

Glacier surge as a trigger for the fastest delta growth in the Arctic

KAVAN, Jan; M. C. STRZELECKI; D. I. BENN; A. LUCKMAN; Matěj ROMAN et al.

Základní údaje

Originální název

Glacier surge as a trigger for the fastest delta growth in the Arctic

Autoři

KAVAN, Jan; M. C. STRZELECKI; D. I. BENN; A. LUCKMAN; Matěj ROMAN a P. ZAGÓRSKI

Vydání

Communications Earth & Environment, Nature Publishing Group, 2024, 2662-4435

Další údaje

Jazyk

angličtina

Typ výsledku

Článek v odborném periodiku

Obor

10505 Geology

Stát vydavatele

Velká Británie a Severní Irsko

Utajení

není předmětem státního či obchodního tajemství

Odkazy

URL

Impakt faktor

Impact factor: 8.900

Označené pro přenos do RIV

Ano

Kód RIV

RIV/00216224:14310/24:00138007

Organizační jednotka

Přírodovědecká fakulta

Klíčová slova anglicky

TIDEWATER GLACIER; BERING GLACIER; MASS-LOSS; SVALBARD; RECHERCHEFJORDEN; DEGLACIATION; EVOLUTION; DYNAMICS; RETREAT; SURFACE

Štítky

14315030, rivok

Příznaky

Mezinárodní význam, Recenzováno

Změněno: 13. 12. 2024 12:28, Mgr. Marie Novosadová Šípková, DiS.

Anotace

V originále

The widespread retreat of Svalbard glaciers has been frequently interrupted by short-lived surge advances. In the case of marine-terminating glaciers this is often expressed in the remodelling of coastal zones. Here, we analyzed the coastal zone changes in front of the recently surging Recherchebreen. The glacier advanced ca 1200 m since 2018 and suddenly stopped in June 2020 followed by the rapid formation of a delta system in front of its subglacial meltwater outlet. The delta advanced by ca 450 m with probably the fastest progradation rate ever detected in the Arctic region (ca 7 m/day). The synchroneity of the final slow-down of the glacier with the delta building indicates that this event records the release of stored water and sediments from beneath the glacier and thus provides direct evidence of drainage reorganisation at the termination of a surge. Such behaviour is likely common among Svalbard surging glaciers, but it only rarely leaves any direct geomorphic evidence.

Návaznosti

GN22-20621O, projekt VaV

Název: Souvislost kvartérních a současných geomorfologických procesů v geosystémech přiléhajících k polárním ledovcům a ledovcovým štítům

Investor: Grantová agentura ČR, Souvislost kvartérních a současných geomorfologických procesů v geosystémech přiléhajících k polárním ledovcům a ledovcovým štítům, Outgoing

Citovat

KAVAN, Jan; M. C. STRZELECKI; D. I. BENN; A. LUCKMAN; Matěj ROMAN a P. ZAGÓRSKI. Glacier surge as a trigger for the fastest delta growth in the Arctic. Communications Earth & Environment. Nature Publishing Group, 2024, roč. 5, č. 1, s. 1-8. ISSN 2662-4435. Dostupné z: https://doi.org/10.1038/s43247-024-01877-8.

@article{2459899,
   author = {Kavan, Jan and Strzelecki, M. C. and Benn, D. I. and Luckman, A. and Roman, Matěj and Zagórski, P.},
   article_number = {1},
   doi = {https://doi.org/10.1038/s43247-024-01877-8},
   keywords = {TIDEWATER GLACIER; BERING GLACIER; MASS-LOSS; SVALBARD; RECHERCHEFJORDEN; DEGLACIATION; EVOLUTION; DYNAMICS; RETREAT; SURFACE},
   language = {eng},
   issn = {2662-4435},
   journal = {Communications Earth & Environment},
   title = {Glacier surge as a trigger for the fastest delta growth in the Arctic},
   url = {https://www.nature.com/articles/s43247-024-01877-8},
   volume = {5},
   year = {2024}
}

TY  - JOUR
ID  - 2459899
AU  - Kavan, Jan - Strzelecki, M. C. - Benn, D. I. - Luckman, A. - Roman, Matěj - Zagórski, P.
PY  - 2024
TI  - Glacier surge as a trigger for the fastest delta growth in the Arctic
JF  - Communications Earth & Environment
VL  - 5
IS  - 1
SP  - 1-8
EP  - 1-8
PB  - Nature Publishing Group
SN  - 26624435
KW  - TIDEWATER GLACIER
KW  - BERING GLACIER
KW  - MASS-LOSS
KW  - SVALBARD
KW  - RECHERCHEFJORDEN
KW  - DEGLACIATION
KW  - EVOLUTION
KW  - DYNAMICS
KW  - RETREAT
KW  - SURFACE
UR  - https://www.nature.com/articles/s43247-024-01877-8
N2  - The widespread retreat of Svalbard glaciers has been frequently interrupted by short-lived surge advances. In the case of marine-terminating glaciers this is often expressed in the remodelling of coastal zones. Here, we analyzed the coastal zone changes in front of the recently surging Recherchebreen. The glacier advanced ca 1200 m since 2018 and suddenly stopped in June 2020 followed by the rapid formation of a delta system in front of its subglacial meltwater outlet. The delta advanced by ca 450 m with probably the fastest progradation rate ever detected in the Arctic region (ca 7 m/day). The synchroneity of the final slow-down of the glacier with the delta building indicates that this event records the release of stored water and sediments from beneath the glacier and thus provides direct evidence of drainage reorganisation at the termination of a surge. Such behaviour is likely common among Svalbard surging glaciers, but it only rarely leaves any direct geomorphic evidence.
ER  -

KAVAN, Jan; M. C. STRZELECKI; D. I. BENN; A. LUCKMAN; Matěj ROMAN a P. ZAGÓRSKI. Glacier surge as a trigger for the fastest delta growth in the Arctic. \textit{Communications Earth \&{}amp; Environment}. Nature Publishing Group, 2024, roč.~5, č.~1, s.~1-8. ISSN~2662-4435. Dostupné z: https://doi.org/10.1038/s43247-024-01877-8.

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