Simple relations for the close-off depth and age in dry-snow densification

A physical model for the snow/firn densification process (Salamatin and others, 2006) and Martinerie and others' (1992, 1994) correlation for the firn density at the pore closure are employed to perform a scale analysis and computational experiments in order to deduce simplified relations for t...

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Main Authors: Salamatin A., Lipenkov V.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2008
Subjects:
Online Access:https://openrepository.ru/article?id=130775
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spelling ftneicon:oai:rour.neicon.ru:rour/130775 2023-05-15T13:29:11+02:00 Simple relations for the close-off depth and age in dry-snow densification Salamatin A. Lipenkov V. 2008 https://openrepository.ru/article?id=130775 unknown Annals of Glaciology 71 49 0260-3055 https://openrepository.ru/article?id=130775 SCOPUS02603055-2008-49-SID58249089794 Article 2008 ftneicon 2020-07-21T11:47:33Z A physical model for the snow/firn densification process (Salamatin and others, 2006) and Martinerie and others' (1992, 1994) correlation for the firn density at the pore closure are employed to perform a scale analysis and computational experiments in order to deduce simplified relations for the close-off depth and ice age in quasi-stationary ice formation conditions. The critical snow density at which ice-grain rearrangement stops is used to take into account variability of snow structures subjected to densification. The results obtained are validated on a representative set of ice-core data from 22 sites which covers wide ranges of present-day temperatures and ice accumulation rates. A simple analytical approximation for the density-depth profile is proposed. Article in Journal/Newspaper Annals of Glaciology ice core NORA (National aggregator of open repositories of Russian universities)
institution Open Polar
collection NORA (National aggregator of open repositories of Russian universities)
op_collection_id ftneicon
language unknown
description A physical model for the snow/firn densification process (Salamatin and others, 2006) and Martinerie and others' (1992, 1994) correlation for the firn density at the pore closure are employed to perform a scale analysis and computational experiments in order to deduce simplified relations for the close-off depth and ice age in quasi-stationary ice formation conditions. The critical snow density at which ice-grain rearrangement stops is used to take into account variability of snow structures subjected to densification. The results obtained are validated on a representative set of ice-core data from 22 sites which covers wide ranges of present-day temperatures and ice accumulation rates. A simple analytical approximation for the density-depth profile is proposed.
format Article in Journal/Newspaper
author Salamatin A.
Lipenkov V.
spellingShingle Salamatin A.
Lipenkov V.
Simple relations for the close-off depth and age in dry-snow densification
author_facet Salamatin A.
Lipenkov V.
author_sort Salamatin A.
title Simple relations for the close-off depth and age in dry-snow densification
title_short Simple relations for the close-off depth and age in dry-snow densification
title_full Simple relations for the close-off depth and age in dry-snow densification
title_fullStr Simple relations for the close-off depth and age in dry-snow densification
title_full_unstemmed Simple relations for the close-off depth and age in dry-snow densification
title_sort simple relations for the close-off depth and age in dry-snow densification
publishDate 2008
url https://openrepository.ru/article?id=130775
genre Annals of Glaciology
ice core
genre_facet Annals of Glaciology
ice core
op_source SCOPUS02603055-2008-49-SID58249089794
op_relation Annals of Glaciology
71
49
0260-3055
https://openrepository.ru/article?id=130775
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