Results 101 to 110 of about 99,097 (202)
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]
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
An energy-balance model for debris-covered glaciers including heat conduction through the debris layer [PDF]
Extensive covers of supraglacial debris are often present in glacier ablation areas, and it is essential to assess exactly how the debris affects glacier melt rates.
Brock, B.W. +5 more
core +1 more source
Motion and calving at LeConte Glacier, Alaska [PDF]
Thesis (M.S.) University of Alaska Fairbanks, 2000An analysis of motion and calving in the terminus region of LeConte Glacier delineates controls which are important to tidewater glacier stability.
O'Neel, Shad
core
Grounding Zone of Helheim Glacier, Greenland, From Terrestrial Radar Interferometry
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 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
Modeling the Controls on the Front Position of a Tidewater Glacier in Svalbard
Calving is an important mass-loss process at ice sheet and marine-terminating glacier margins, but identifying and quantifying its principal driving mechanisms remains challenging.
Jaime Otero +5 more
doaj +1 more source
The aftermath of Petermann Glacier calving events (2008-2012): Ice island size distributions and meltwater dispersal. [PDF]
Three large calving events occurred at Petermann Glacier in northwest Greenland between 2008 and 2012 that generated ice islands (large tabular icebergs) that ranged from ~30 to 300 km2 in areal extent.
Myers, Paul G. +3 more
core +1 more source
Data from Columbia Glacier are used to identify processes that control calving from a temperate tidewater glacier and to re-evaluate models that have been proposed to describe iceberg calving.
С.J. Van Der Veen
core +2 more sources
Synchronous terminus change of East Antarctic outlet glaciers linked to climatic forcing [PDF]
In recent years there has been a growing trend of acceleration, thinning and retreat of ocean-terminating outlet glaciers in both the Greenland and West Antarctic Ice Sheets, resulting in an increasing contribution to sea level rise.
MILES, BERTIE
core

