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Record #112535:

Changes in Arctic Ocean surface water properties and ice covers in response to global climate change during the last 20,000 years / R.F. Spielhagen, S. Köhler, U. Pagels, Jörn Thiede.

Title: Changes in Arctic Ocean surface water properties and ice covers in response to global climate change during the last 20,000 years / R.F. Spielhagen, S. Köhler, U. Pagels, Jörn Thiede.
Author(s): Spielhagen, R. F.
Köhler, S.
Pagels, U.
Thiede, Jörn.
Date: 1991.
In: Eos : transactions, American Geophysical Union. (1991.), Vol. 72(44, supplement) (1991)
Abstract: AGU Fall Meeting Program and Abstracts, December 9-13, 1991. Results indicate that surface drift regime in eastern Arctic Ocean and western Fram Strait did not change significantly during last glacial--interglacial transition, whereas in eastern Fram Strait conversion of surface drift occurred. Sedimentation rates were very low during last glacial and increased afterwards. AMS datings indicate postglacial time lag of 2 to 3 ka for establishment of present-day ¹⁸O composition of uppermost water column.
Notes:

Eos : transactions, American Geophysical Union. Vol. 72(44, supplement) :238 (1991).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.326.14 -- Floating ice, movement.
551.46 -- Oceanography, physical.
551.464 -- Sea water, chemical properties.
E6 -- Glaciology: floating ice.
(*60) -- Arctic Ocean and adjacent waters.
(*617) -- Greenland Sea and Fram Strait.
SPRI record no.: 112535

MARCXML

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245 00 ‡aChanges in Arctic Ocean surface water properties and ice covers in response to global climate change during the last 20,000 years /‡cR.F. Spielhagen, S. Köhler, U. Pagels, Jörn Thiede.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 238.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 72(44, supplement) :238 (1991).
520 3# ‡aAGU Fall Meeting Program and Abstracts, December 9-13, 1991. Results indicate that surface drift regime in eastern Arctic Ocean and western Fram Strait did not change significantly during last glacial--interglacial transition, whereas in eastern Fram Strait conversion of surface drift occurred. Sedimentation rates were very low during last glacial and increased afterwards. AMS datings indicate postglacial time lag of 2 to 3 ka for establishment of present-day ¹⁸O composition of uppermost water column.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.464 -- Sea water, chemical properties.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc
700 1# ‡aSpielhagen, R. F.
700 1# ‡aKöhler, S.
700 1# ‡aPagels, U.
700 1# ‡aThiede, Jörn.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 72(44, supplement) (1991) ‡wSPRI-1028
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