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Record #122428:

The "flickering switch" of Late Pleistocene climate change / Kendrick C. Taylor, and 7 others.

Title: The "flickering switch" of Late Pleistocene climate change / Kendrick C. Taylor, and 7 others.
Author(s): Taylor, Kendrick C.
Date: 1993.
In: Nature. (1993.), Vol. 361(6411) (1993)
Abstract: Previous Greenland ice cores have documented relatively warm interstadial periods during last glaciation and short returns to colder conditions during glacial to interglacial warming. Here, electrical conductivity measurements are reported from new (GISP2) Greenland ice core which confirms previous observations and also reveals hitherto urecognized mode of rapid climatic variation. Fluctuations in ice conductivity on scales of <5 to 20 years reflect rapid oscillations in dust content of atmosphere. This "flickering" between two preferred states seems to require rapid reorganizations in atmospheric circulations.
Notes:

Nature. Vol. 361(6411) :432-435 (1993).

Keywords: 551.321.2 -- Snow and ice, methods of sampling, excavating, drilling, etc.
622.14 -- Core sampling, ice and snow.
551.32 -- Glaciology.
551.324 -- Land ice.
551.324.24 -- Ice sheets and caps.
537.311 -- Ice, electrical conductivity.
551.58 -- Climatology.
551.583 -- Climatic changes.
551.583.3 -- Climatic changes, Quaternary.
550.93 -- Geochronology.
E9 -- Glaciology: meteorology and climatology.
(*38) -- Greenland.
SPRI record no.: 122428

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245 15 ‡aThe "flickering switch" of Late Pleistocene climate change /‡cKendrick C. Taylor, and 7 others.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 432-435 :‡bdiags.
500 ## ‡aNature. Vol. 361(6411) :432-435 (1993).
520 3# ‡aPrevious Greenland ice cores have documented relatively warm interstadial periods during last glaciation and short returns to colder conditions during glacial to interglacial warming. Here, electrical conductivity measurements are reported from new (GISP2) Greenland ice core which confirms previous observations and also reveals hitherto urecognized mode of rapid climatic variation. Fluctuations in ice conductivity on scales of <5 to 20 years reflect rapid oscillations in dust content of atmosphere. This "flickering" between two preferred states seems to require rapid reorganizations in atmospheric circulations.
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 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.324 -- Land ice.‡2udc
650 07 ‡a551.324.24 -- Ice sheets and caps.‡2udc
650 07 ‡a537.311 -- Ice, electrical conductivity.‡2udc
650 07 ‡a551.58 -- Climatology.‡2udc
650 07 ‡a551.583 -- Climatic changes.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡2udc
650 07 ‡a550.93 -- Geochronology.‡2udc
650 07 ‡aE9 -- Glaciology: meteorology and climatology.‡2local
651 #7 ‡a(*38) -- Greenland.‡2udc
773 0# ‡7nnas ‡tNature. ‡gVol. 361(6411) (1993) ‡wSPRI-1046
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