Results 31 to 40 of about 314,168 (203)

Composition of firn air at the North Greenland Ice Core Project (NGRIP) site [PDF]

open access: yes, 2021
Reconstructions of the past variations of atmospheric composition are important for better understanding of the changes in climate and atmospheric chemistry.

core  

Gas isotope thermometry in the South Pole and Dome Fuji ice cores provides evidence for seasonal rectification of ice core gas records [PDF]

open access: yesThe Cryosphere, 2022
Gas isotope thermometry using the isotopes of molecular nitrogen and argon has been used extensively to reconstruct past surface temperature change from Greenland ice cores. The gas isotope ratios δ15N and δ40Ar in the ice core are each set by the amount
J. D. Morgan   +7 more
doaj   +1 more source

Spatial Distribution of Crusts in Antarctic and Greenland Snowpacks and Implications for Snow and Firn Studies

open access: yesFrontiers in Earth Science, 2021
The occurrence of snowpack features has been used in the past to classify environmental regimes on the polar ice sheets. Among these features are thin crusts with high density, which contribute to firn stratigraphy and can have significant impact on firn
Alexander H. Weinhart   +5 more
doaj   +1 more source

Modelling L-band microwave brightness temperature time series for firn aquifers [PDF]

open access: yesThe Cryosphere
Firn aquifers are important in polar ice sheet hydrology and the associated mass and energy transport processes. Although the firn aquifer extent has been mapped using passive microwave satellite observations, models for predicting the L-band brightness ...
H. Xu   +4 more
doaj   +1 more source

Gas diffusivity and permeability through the firn column at Summit, Greenland: measurements and comparison to microstructural properties [PDF]

open access: yesThe Cryosphere, 2014
The physical structure of polar firn plays a key role in the mechanisms by which glaciers and ice sheets preserve a natural archive of past atmospheric composition. This study presents the first measurements of gas diffusivity and permeability along with
A. C. Adolph, M. R. Albert
doaj   +1 more source

Investigations of meltwater refreezing and density variations in the snowpack and firn within the percolation zone of the Greenland ice sheet [PDF]

open access: yes, 2007
The mass balance of polythermal ice masses is critically dependent on the proportion of surface-generated meltwater that subsequently refreezes in the snowpack and firn.
Nienow, Peter   +12 more
core   +1 more source

Pore morphology of polar firn around closure revealed by X-ray tomography [PDF]

open access: yesThe Cryosphere, 2018
Understanding the slow densification process of polar firn into ice is essential in order to constrain the age difference between the ice matrix and entrapped gases.
A. Burr   +7 more
doaj   +1 more source

BUBBLE VOLUMES IN FIRN-ICE TRANSITION LAYER OF ICE CORES FROM POLAR ICE SHEETS [PDF]

open access: yes, 1994
P(論文)The air bubble formation process has been studied experimentally by using five ice cores from the Greenland and Antarctic ice sheets. Bubble volumes in firn-ice samples were measured by a classical method based on the Boyle-Charles law for an ideal ...
カメダ, タカオ   +3 more
core   +1 more source

Comparison of elastic moduli from seismic diving-wave and ice-core microstructure analysis in Antarctic polar firn

open access: yesAnnals of Glaciology, 2019
We compared elastic moduli in polar firn derived from diving wave refraction seismic velocity analysis, firn-core density measurements and microstructure modelling based on firn-core data.
Rebecca Schlegel   +8 more
doaj   +1 more source

Modelling the transition from grain-boundary sliding to power-law creep in dry snow densification

open access: yesJournal of Glaciology, 2022
This paper presents a physics-based macroscale model for the densification of dry snow which provides for a smooth transition between densification by grain-boundary sliding (stage 1) and densification by power-law creep (stage 2).
Elizabeth M. Morris   +2 more
doaj   +1 more source

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