Table 3.1 Content and composition of air in an ice profile from Camp III i Greenland

The air trapped in freshly formed ice gives information concerning the ice formation processes as weH as concerning severa,l environmental parameters at the time of ice formation. Air arnount, air composition, and the size and form of bubbles may change with time. Possible processes responsible for...

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Bibliographic Details
Main Author: Stauffer, Bernhard
Format: Dataset
Language:English
Published: PANGAEA 1981
Subjects:
Air content
Argon
CAMP_III
Carbon dioxide
DEPTH
ice/snow
EGIG
Expédition Glaciologique Internationale au Groenlande
Greenland
ICE
Ice station
Nitrogen
gas
Oxygen
Sampling/drilling ice
glacier
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.803120
https://doi.org/10.1594/PANGAEA.803120
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.803120
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.803120 2023-05-15T16:21:19+02:00 Table 3.1 Content and composition of air in an ice profile from Camp III i Greenland Stauffer, Bernhard LATITUDE: 69.725000 * LONGITUDE: -50.048000 * MINIMUM DEPTH, ice/snow: 1.93 m * MAXIMUM DEPTH, ice/snow: 21.00 m 1981-11-28 text/tab-separated-values, 50 data points https://doi.pangaea.de/10.1594/PANGAEA.803120 https://doi.org/10.1594/PANGAEA.803120 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.803120 https://doi.org/10.1594/PANGAEA.803120 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Stauffer, Bernhard (1981): Die Zusammensetzung der Luft in natürlichem Eis. Zeitschrift für Gletscherkunde und Glazialgeologie, 17(1), 57-78, hdl:10013/epic.40237.d001 Air content Argon CAMP_III Carbon dioxide DEPTH ice/snow EGIG Expédition Glaciologique Internationale au Groenlande Greenland ICE Ice station Nitrogen gas Oxygen Sampling/drilling ice Dataset 1981 ftpangaea https://doi.org/10.1594/PANGAEA.803120 2023-01-20T08:59:47Z The air trapped in freshly formed ice gives information concerning the ice formation processes as weH as concerning severa,l environmental parameters at the time of ice formation. Air arnount, air composition, and the size and form of bubbles may change with time. Possible processes responsible for such changes are discussed. In very cold ice air content and air composition remain almost unchanged. Samples of ancient atmospheric air are therefore very weH preserved in cold ice. In temperate ice changes of the air amount and air composition depend on the intergranular water fiow through the glacier. This waterfiow can be estimated by measuring air amount and air composition in ice sampIes. Dataset glacier Greenland PANGAEA - Data Publisher for Earth & Environmental Science Greenland ENVELOPE(-50.048000,-50.048000,69.725000,69.725000)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic Air content
Argon
CAMP_III
Carbon dioxide
DEPTH
ice/snow
EGIG
Expédition Glaciologique Internationale au Groenlande
Greenland
ICE
Ice station
Nitrogen
gas
Oxygen
Sampling/drilling ice
spellingShingle Air content
Argon
CAMP_III
Carbon dioxide
DEPTH
ice/snow
EGIG
Expédition Glaciologique Internationale au Groenlande
Greenland
ICE
Ice station
Nitrogen
gas
Oxygen
Sampling/drilling ice
Stauffer, Bernhard
Table 3.1 Content and composition of air in an ice profile from Camp III i Greenland
topic_facet Air content
Argon
CAMP_III
Carbon dioxide
DEPTH
ice/snow
EGIG
Expédition Glaciologique Internationale au Groenlande
Greenland
ICE
Ice station
Nitrogen
gas
Oxygen
Sampling/drilling ice
description The air trapped in freshly formed ice gives information concerning the ice formation processes as weH as concerning severa,l environmental parameters at the time of ice formation. Air arnount, air composition, and the size and form of bubbles may change with time. Possible processes responsible for such changes are discussed. In very cold ice air content and air composition remain almost unchanged. Samples of ancient atmospheric air are therefore very weH preserved in cold ice. In temperate ice changes of the air amount and air composition depend on the intergranular water fiow through the glacier. This waterfiow can be estimated by measuring air amount and air composition in ice sampIes.
format Dataset
author Stauffer, Bernhard
author_facet Stauffer, Bernhard
author_sort Stauffer, Bernhard
title Table 3.1 Content and composition of air in an ice profile from Camp III i Greenland
title_short Table 3.1 Content and composition of air in an ice profile from Camp III i Greenland
title_full Table 3.1 Content and composition of air in an ice profile from Camp III i Greenland
title_fullStr Table 3.1 Content and composition of air in an ice profile from Camp III i Greenland
title_full_unstemmed Table 3.1 Content and composition of air in an ice profile from Camp III i Greenland
title_sort table 3.1 content and composition of air in an ice profile from camp iii i greenland
publisher PANGAEA
publishDate 1981
url https://doi.pangaea.de/10.1594/PANGAEA.803120
https://doi.org/10.1594/PANGAEA.803120
op_coverage LATITUDE: 69.725000 * LONGITUDE: -50.048000 * MINIMUM DEPTH, ice/snow: 1.93 m * MAXIMUM DEPTH, ice/snow: 21.00 m
long_lat ENVELOPE(-50.048000,-50.048000,69.725000,69.725000)
geographic Greenland
geographic_facet Greenland
genre glacier
Greenland
genre_facet glacier
Greenland
op_source Supplement to: Stauffer, Bernhard (1981): Die Zusammensetzung der Luft in natürlichem Eis. Zeitschrift für Gletscherkunde und Glazialgeologie, 17(1), 57-78, hdl:10013/epic.40237.d001
op_relation https://doi.pangaea.de/10.1594/PANGAEA.803120
https://doi.org/10.1594/PANGAEA.803120
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_rightsnorm CC-BY
op_doi https://doi.org/10.1594/PANGAEA.803120
_version_ 1766009330674434048

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