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Record #152533:

Density log of a 181 m long ice core from Berkner Island, Antarctica / S. Gerland, H. Oerter, J. Kipfstuhl, F. Wilhelms, H. Miller, W.D. Miners.

Title: Density log of a 181 m long ice core from Berkner Island, Antarctica / S. Gerland, H. Oerter, J. Kipfstuhl, F. Wilhelms, H. Miller, W.D. Miners.
Author(s): Gerland, S.
Oerter, H.
Kipfstuhl, J.
Wilhelms, F.
Miller, H.
Miners, W. D.
Date: 1999.
In: Annals of Glaciology. (1999.), Vol. 29 (1999)
Abstract: Measures density every 3 mm along 181 m long ice core from Berkner Island, Antarctica, using attenuation of gamma-ray beam. Shows general density increase with depth. In shallowest part of core, density of winter layers is higher than that of summer layers, though this is reversed at greater depth. Assumes densification rates are different for two types of firn. Similar density phenomena were observed on ice cores from Greenland.
Notes:

Annals of Glaciology. Vol. 29 :215-219 (1999).

Sixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor)

Keywords: 551.32 -- Glaciology.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
551.322 -- Ice and snow.
531.754 -- Ice, density.
551.324 -- Land ice.
550.837 -- Electrical survey methods.
E5 -- Glaciology: land ice.
(*7) -- Antarctic regions.
(*728.6) -- Berkener Island.
(*38) -- Greenland.
SPRI record no.: 152533

MARCXML

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245 00 ‡aDensity log of a 181 m long ice core from Berkner Island, Antarctica /‡cS. Gerland, H. Oerter, J. Kipfstuhl, F. Wilhelms, H. Miller, W.D. Miners.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1999.
300 ## ‡ap. 215-219 :‡bill., diags.
500 ## ‡aAnnals of Glaciology. Vol. 29 :215-219 (1999).
500 ## ‡aSixth International Symposium on Antarctic Glaciology (ISAG-6), 5--9 September 1998, Lanzhou, China, T.H. Jacka (Editor)
520 3# ‡aMeasures density every 3 mm along 181 m long ice core from Berkner Island, Antarctica, using attenuation of gamma-ray beam. Shows general density increase with depth. In shallowest part of core, density of winter layers is higher than that of summer layers, though this is reversed at greater depth. Assumes densification rates are different for two types of firn. Similar density phenomena were observed on ice cores from Greenland.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.‡2udc
650 07 ‡a622.14 -- Core sampling, ice and snow.‡2udc
650 07 ‡a551.322 -- Ice and snow.‡2udc
650 07 ‡a531.754 -- Ice, density.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a550.837 -- Electrical survey methods.‡2udc
650 07 ‡aE5 -- Glaciology: land ice.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*728.6) -- Berkener Island.‡2udc
651 #7 ‡a(*38) -- Greenland.‡2udc
700 1# ‡aGerland, S.
700 1# ‡aOerter, H.
700 1# ‡aKipfstuhl, J.
700 1# ‡aWilhelms, F.
700 1# ‡aMiller, H.
700 1# ‡aMiners, W. D.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 29 (1999) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20220925