Results 1 to 10 of about 776 (180)

Thermal conductivity of polar firn [PDF]

open access: goldJournal of Glaciology, 2022
The vast Greenland and Antarctic Ice Sheets are covered by many tens of meters of polar firn, which is snow that is years to centuries old and has experienced significant metamorphism. Both ice-sheet modeling and decoding satellite data require knowledge
Simon E. Oster, Mary R. Albert
doaj   +3 more sources

The Onset of Recrystallization in Polar Firn [PDF]

open access: goldGeophysical Research Letters, 2023
Constraining the onset of dynamic recrystallization (DRX) and its effects on the mechanical properties of firn is crucial for firn densification modeling.
Ayobami Ogunmolasuyi   +2 more
doaj   +3 more sources

Historical porosity data in polar firn [PDF]

open access: goldEarth System Science Data, 2020
In the 1990s, closed and open porosity volumes of firn samples were measured by J.-M. Barnola using the technique of gas pycnometry, on firn from three different polar sites.
K. Fourteau   +6 more
doaj   +7 more sources

Observations of the creep of polar firn [PDF]

open access: goldJournal of Glaciology, 2022
Constant-load creep tests were performed at −10°C at various compressive stresses from 0.05 to 0.75 MPa on specimens taken every 10 m along a firn core extracted at Summit, Greenland in June 2017.
Yuan Li, Ian Baker
doaj   +3 more sources

Evidence of dynamic recrystallization in polar firn [PDF]

open access: bronzeJournal of Geophysical Research, 2009
Microstructural analyses have been performed on polar firn from the European Project for Ice Coring in Antarctica drilling site in Dronning Maud Land, Antarctica. The results derived from images of the firn structure in microscopic resolution indicate that dynamic recrystallization is active in firn at all depths, and it dominates the evolution of the ...
Sepp Kipfstuhl   +2 more
exaly   +8 more sources

Observations of creep of polar firn at different temperatures [PDF]

open access: goldThe Cryosphere
To improve our understanding of firn compaction and deformation processes, constant-load compressive creep tests were performed on specimens from a Summit, Greenland (72°35′ N, 38°25′ W) firn core that was extracted in June 2017.
Y. Li, Y. Li, K. Keegan, I. Baker
doaj   +4 more sources

Direct and Inverse Problem for Gas Diffusion in Polar Firn [PDF]

open access: greenCommunications on Analysis and Computation, 2022
41 pages, 18 ...
Sophie Moufawad   +2 more
openalex   +5 more sources

On the impact of impurities on the densification of polar firn [PDF]

open access: yesEarth and Planetary Science Letters, 2012
Understanding polar firn densification is crucial for reconstructing the age of greenhouse gas concentrations extracted from ice cores, and for the interpretation of air in ice as a dating tool or as a climate proxy. Firn densification is generally modeled as a steady burial and sintering process of defined layers, where the structure of the layering ...
Thomas Laepple   +2 more
exaly   +4 more sources

Polar firn properties in Greenland and Antarctica and related effects on microwave brightness temperatures [PDF]

open access: goldThe Cryosphere, 2023
In studying the mass balance of polar ice sheets, fluctuations in firn density near the surface is a major uncertainty. In this paper, we explore these variations at locations on the Greenland Ice Sheet and at the Dome C location in Antarctica.
H. Xu   +6 more
doaj   +2 more sources

Concerning the Deposition and Diagenesis of Strata in Polar Firn [PDF]

open access: bronzeJournal of Glaciology, 1988
Abstract Depth hoar in polar firn forms when large temperature gradients act on low-density firn, but high-density firn does not develop into depth hoar. Low densities in firn may be depositional (burial of surface hoar or still-air snowfall) or diagenetic (mass loss to the free atmosphere, typically in autumn); however, diagenesis is
Richard B. Alley
openalex   +2 more sources

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