Results 81 to 90 of about 918 (177)

The Impact of Subglacial Drainage System Evolution and Glacier Lake Outburst on Arctic Fjord Macronutrient Dynamics

open access: yesJournal of Geophysical Research: Biogeosciences, Volume 131, Issue 7, July 2026.
Abstract Global warming is amplified in the Arctic, accelerating glacier melt and freshwater runoff. At tidewater glaciers, runoff typically enters fjords at depth and generates buoyancy‐driven circulation that enhances glacier‐ocean exchanges of energy and matter, influencing macronutrient delivery and marine primary production.
Andreas Alexander   +19 more
wiley   +1 more source

Warm Surface Waters Dominate Melting of the Denman‐Shackleton Ice Shelf System

open access: yesJournal of Geophysical Research: Oceans, Volume 131, Issue 7, July 2026.
Abstract The ocean dynamics controlling the melting of the Denman‐Shackleton ice shelf system are investigated using a high‐resolution regional ocean‐sea ice‐ice shelf model. Our results show that basal meltwater production exhibits strong seasonal variability, driven by the ocean heat supply toward the ice shelf system, and occurs through two distinct
Yuhang Liu   +4 more
wiley   +1 more source

Internal tsunamigenesis and ocean mixing driven by glacier calving in Antarctica. [PDF]

open access: yesSci Adv, 2022
Meredith MP   +17 more
europepmc   +1 more source

Thermal flexure and glacier calving

open access: yes, 2019
Glaciers and ice sheets that terminate in bodies of water are expected to undergo thermal expansion as ice comes into contact with much warmer liquid water. Here, I investigate the roll that this thermal expansion plays in the fracturing processes that give rise to glacier calving.
openaire   +1 more source

Calving front positions for 42 key glaciers of the Antarctic Peninsula Ice Sheet: a sub-seasonal record from 2013 to 2023 based on deep-learning application to Landsat multi-spectral imagery [PDF]

open access: yesEarth System Science Data
Calving front positions of marine-terminating glaciers are an essential parameter for understanding dynamic glacier changes and constraining ice modelling.
E. Loebel   +5 more
doaj   +1 more source

A dramatic 800-m retreat of a lake-terminating glacier on the Tibetan Plateau during 2014–2015, caused by glacier calving

open access: yesJournal of Glaciology
Compared to land-terminating glaciers, lake-terminating glaciers generally experience a higher mass loss due to the feedback from processes such as calving, dynamic thinning and flow acceleration associated with proglacial lakes.
Xuanru Zhao   +6 more
doaj   +1 more source

Surface dynamics and history of the calving cycle of Astrolabe Glacier (Adélie Coast, Antarctica) derived from satellite imagery [PDF]

open access: yesThe Cryosphere
The recent calving of Astrolabe Glacier on the Adélie Coast (East Antarctica) in November 2021 presents an opportunity to better understand the processes leading to ice tongue fracturing.
F. Provost   +7 more
doaj   +1 more source

Responses of a polar predator to a glacier calving event [PDF]

open access: yesRoyal Society Open Science
Extreme episodic changes in Antarctic continental shelf regions, such as glacier calving or iceberg grounding, can fundamentally reshape regional sea-ice conditions.
Adélie Antoine   +16 more
doaj   +1 more source

Grounding Zone of Helheim Glacier, Greenland, From Terrestrial Radar Interferometry

open access: yesGeophysical Research Letters
Helheim Glacier, in East Greenland, is a major outlet glacier that discharges about 33 Gigatons of ice per year into the ocean. Helheim has been undergoing a retreat since 2003.
Jae Hun Kim   +4 more
doaj   +1 more source

Calving as a Source of Acute and Persistent Kinetic Energy to Enhance Submarine Melting of Tidewater Glaciers

open access: yesGeophysical Research Letters
Calving icebergs at tidewater glaciers release large amounts of potential energy. This energy—in principle—could be a source for submarine melting, which scales with near‐terminus water temperature and velocity.
M. F. Shaya   +6 more
doaj   +1 more source

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