Firn

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51

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Source URL: www.pages-igbp.org

Language: English - Date: 2009-07-29 06:55:15
52Fluctuations of GlaciersVol. V)

Fluctuations of GlaciersVol. V)

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Source URL: www.wgms.ch

Language: English - Date: 2012-04-17 03:32:00
53Fluctuations of GlaciersVol. III)

Fluctuations of GlaciersVol. III)

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Source URL: www.wgms.ch

Language: English - Date: 2012-04-18 06:24:00
54Fluctuations of GlaciersVol. IV)

Fluctuations of GlaciersVol. IV)

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Source URL: www.wgms.ch

Language: English - Date: 2012-04-17 03:44:00
55effects when the results of the stable oxygen isotopic measurements become available. R. Alley has studied the 50-meter core obtained by the Polar Ice Coring Office. He has found grain size and firn-structural variations

effects when the results of the stable oxygen isotopic measurements become available. R. Alley has studied the 50-meter core obtained by the Polar Ice Coring Office. He has found grain size and firn-structural variations

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 06:17:27
56Physical studies of firn and ice cores on the Siple Coast clearly are of interest in understanding processes occurring in and adjacent to ice streams and in interpreting geophysical data collected on the ground and from

Physical studies of firn and ice cores on the Siple Coast clearly are of interest in understanding processes occurring in and adjacent to ice streams and in interpreting geophysical data collected on the ground and from

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Language: English - Date: 2011-05-06 15:41:47
57the Allan Hills region to collect more than 100 meters of firn and ice core for later analysis. Tests of a solar-powered version of the auger were conducted at South Pole Station (figure 2). Solar panel performance was 2

the Allan Hills region to collect more than 100 meters of firn and ice core for later analysis. Tests of a solar-powered version of the auger were conducted at South Pole Station (figure 2). Solar panel performance was 2

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 05:01:04
58transition zone will be less complex, too. At a firn temperature of —50°C, the portion of gases adsorbed at the firn grain surface is expected to be minimal. Therefore, it is believed that gases enclosed in ice sample

transition zone will be less complex, too. At a firn temperature of —50°C, the portion of gases adsorbed at the firn grain surface is expected to be minimal. Therefore, it is believed that gases enclosed in ice sample

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Source URL: s3.amazonaws.com

Language: English - Date: 2011-05-06 06:16:48
59sional deposition from supercooled fogs (Linkletter and Warburton, 1976), and (2) fresh snowfall in light wind conditions. These enhanced factors are greater than those seen in samples of snow and firn collected from sha

sional deposition from supercooled fogs (Linkletter and Warburton, 1976), and (2) fresh snowfall in light wind conditions. These enhanced factors are greater than those seen in samples of snow and firn collected from sha

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Language: English - Date: 2011-05-06 03:40:04
60egu_logo_without_circle_grey

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Source URL: www.the-cryosphere.net

Language: English - Date: 2014-12-04 08:10:38