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Folds in firn

Geological Society of America Bulletin, 1981
Folds in firn on glaciers of the Gilkey Trench, Alaska, have been observed during years of heavy snowfall and reduced ablation. The firn folds were formed by up-buckling and decollement resulting from intense lateral shortening within the underlying glacier ice.
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Assessing firn water storage from a multi-data firn-model inversion

2022
<p>The ESA 4DGreenland project has the objective of performing an integrated assessment of Greenland’s hydrology through maximizing the use of Earth observation (EO) data. However, as meltwater is activated on the surface of the Greenland ice sheet and percolates into the firn, the firn water storage and delayed runoff are ...
Sebastian B. Simonsen   +4 more
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Microstructural characterization of firn

Hydrological Processes, 2007
AbstractIn this paper, we use a scanning electron microscope (SEM) coupled with X‐ray spectroscopy and electron back‐scattered diffraction patterns to examine firn in cores retrieved by the United States International Trans‐Antarctic Scientific Expedition.
I. Baker   +3 more
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Characterizing the influence of idealized atmospheric forcings on firn using the SNOWPACK firn model

2023
The porous layer of snow and firn that blankets ice sheets can store meltwater and buffer an ice sheet’s contribution to sea level rise. A warming climate threatens this buffering capacity and will likely lead to depletion of the air-filled pore space, known as the firn air content.
Megan Thompson-Munson   +2 more
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Studying Firn Properties with Radiometer, Radar, and the Community Firn Model

IGARSS 2023 - 2023 IEEE International Geoscience and Remote Sensing Symposium, 2023
Haokui Xu, Brooke Medley, Leung Tsang
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Calibrating a compressible firn rheology and application to firn in shear zones

Most existing firn densification models are one-dimensional and empirical, limiting their ability to accurately represent complex stress regimes. For instance, they fail to account for enhanced densification in shear zones. In contrast, the Gagliardini and Meysonnier 1997 (GM97) model offers a more comprehensive approach by incorporating a compressible
Aslak Grinsted   +2 more
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Simulating Greenland Ice Slabs and Firn Aquifers with a 1D Firn Model

The Greenland Ice Sheet (GrIS) has been losing mass at an accelerating rate, primarily due to meltwater runoff to the ocean. Firn, a porous transition layer between snow and ice, has the potential to buffer the GrIS’s contribution to sea level rise by retaining this meltwater.
Nikola Jovanovic   +2 more
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Firn

2020
Christo Buizert, Michiel Helsen
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Gas Diffusion in Firn

1996
Different components and properties of the ice deposits on the earth (glaciers, ice sheets) store information on the climate and environment. We can mainly distinguish between three storage types: a) properties and isotopie composition of the ice itself, b) solid (and liquid) trace substances in the ice, and c) gaseous and volatile components.
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Firn

2011
Rachel W. Obbard   +2 more
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