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Record #149188:

Preliminary investigation of palaeoclimate signals recorded in the ice core from Dome Fuji station, east Dronning Maud Land, Antarctica / Dome-F Ice Core Research Group.

Title: Preliminary investigation of palaeoclimate signals recorded in the ice core from Dome Fuji station, east Dronning Maud Land, Antarctica / Dome-F Ice Core Research Group.
Author (corporate): Dome-F Ice Core Research Group.
Date: 1998.
In: Annals of Glaciology. (1998.), Vol. 27 (1998)
Abstract: Ice core drilled 1995-96 at Dome Fuji, Dronning Maud Land, Antarctica, indicates two warm stages and one cold stage from surface down to 1800 m depth. Chemical constituents of ice core show differences between warm and cold periods. Depth-age relationship is obtained. Metamorphism of snow at surface may modify chemical signals indicative of atmospheric conditions.
Notes:

Annals of Glaciology. Vol. 27 :338-342 (1998).

International Symposium on Antarctica and Global Change: Interactions and Impacts, W.F. Budd (Editor), 13--18 July 1997, Hobart, Tasmania, Australia.

Keywords: 551.32 -- Glaciology.
54 -- Chemistry.
551.324 -- Land ice.
551.324.43 -- Land ice, regime and mass balance.
551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
551.578.46 -- Snow cover and snow patches.
551.583.3 -- Climatic changes, Quaternary.
551.794 -- Holocene.
E9 -- Glaciology: meteorology and climatology.
(*7) -- Antarctic regions.
(*73) -- Dronning Maud Land.
SPRI record no.: 149188

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245 10 ‡aPreliminary investigation of palaeoclimate signals recorded in the ice core from Dome Fuji station, east Dronning Maud Land, Antarctica /‡cDome-F Ice Core Research Group.
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500 ## ‡aAnnals of Glaciology. Vol. 27 :338-342 (1998).
500 ## ‡aInternational Symposium on Antarctica and Global Change: Interactions and Impacts, W.F. Budd (Editor), 13--18 July 1997, Hobart, Tasmania, Australia.
520 3# ‡aIce core drilled 1995-96 at Dome Fuji, Dronning Maud Land, Antarctica, indicates two warm stages and one cold stage from surface down to 1800 m depth. Chemical constituents of ice core show differences between warm and cold periods. Depth-age relationship is obtained. Metamorphism of snow at surface may modify chemical signals indicative of atmospheric conditions.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a54 -- Chemistry.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.43 -- Land ice, regime and mass balance.‡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 ‡a551.578.46 -- Snow cover and snow patches.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a551.794 -- Holocene.‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(*7) -- Antarctic regions.‡2udc
651 #7 ‡a(*73) -- Dronning Maud Land.‡2udc
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