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Record #112538:

Simulation of sea ice conditions during the "great salinity anomaly" period: 1965-1975 / J.A. Maslanik, M.C. Serreze, Gregory M. Flato.

Title: Simulation of sea ice conditions during the "great salinity anomaly" period: 1965-1975 / J.A. Maslanik, M.C. Serreze, Gregory M. Flato.
Author(s): Maslanik, J. A.
Serreze, M. C.
Flato, Gregory M.
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. This period of widespread freshening of North Atlantic surface waters has implications for reconstruction of past climatic conditions. Previous work has attempted to relate period to fresh-water inflow from rivers and to variations in atmospheric circulation in Arctic. In particular, increased anticyclonic activity over Canadian archipelago has been shown to be correlated with above-average ice-covered area in Greenland Sea. Hypothesizes that changes in atmospheric circulation in turn changed source region for ice flux through Fram Strait, increasing flow of thick, multiyear ice into East Greenland Sea.
Notes:

Eos : transactions, American Geophysical Union. Vol. 72(44, supplement) :242 (1991).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.326.14 -- Floating ice, movement.
551.46 -- Oceanography, physical.
551.465 -- Oceanography, dynamics.
551.583.3 -- Climatic changes, Quaternary.
E6 -- Glaciology: floating ice.
(*60) -- Arctic Ocean and adjacent waters.
(*617) -- Greenland Sea and Fram Strait.
(*61) -- North Atlantic Ocean.
SPRI record no.: 112538

MARCXML

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100 1# ‡aMaslanik, J. A.
245 10 ‡aSimulation of sea ice conditions during the "great salinity anomaly" period :‡b1965-1975 /‡cJ.A. Maslanik, M.C. Serreze, Gregory M. Flato.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 242.
500 ## ‡aEos : transactions, American Geophysical Union. Vol. 72(44, supplement) :242 (1991).
520 3# ‡aAGU Fall Meeting Program and Abstracts, December 9-13, 1991. This period of widespread freshening of North Atlantic surface waters has implications for reconstruction of past climatic conditions. Previous work has attempted to relate period to fresh-water inflow from rivers and to variations in atmospheric circulation in Arctic. In particular, increased anticyclonic activity over Canadian archipelago has been shown to be correlated with above-average ice-covered area in Greenland Sea. Hypothesizes that changes in atmospheric circulation in turn changed source region for ice flux through Fram Strait, increasing flow of thick, multiyear ice into East Greenland Sea.
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 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a551.583.3 -- Climatic changes, Quaternary.‡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
651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc
700 1# ‡aSerreze, M. C.
700 1# ‡aFlato, Gregory M.
773 0# ‡7nnas ‡tEos : transactions, American Geophysical Union. ‡gVol. 72(44, supplement) (1991) ‡wSPRI-1028
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