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Record #122777:

Formation of Denmark Strait overflow water by mixing in the East Greenland Current / Volker H. Strass, Eberhard Fahrbach, Ursula Schauer, Lutz Sellman.

Title: Formation of Denmark Strait overflow water by mixing in the East Greenland Current / Volker H. Strass, Eberhard Fahrbach, Ursula Schauer, Lutz Sellman.
Author(s): Strass, Volker H.
Fahrbach, Eberhard.
Schauer, Ursula.
Sellman, Lutz.
Date: 1993.
In: Journal of Geophysical Research. (1993.), Vol. 98(C4) (1993)
Abstract: Hydrographic data and current meter records from East Greenland Current collected 1987-1989 near central Greenland Sea reveal formation of water mass with temperature, salinity and density characteristics of Denmark Strait Overflow Water (DSOW). Downstream (SW) flow of this mass can be half DSOW and results from isopycnic mixing of recirculated Atlantic water and Upper Arctic Intermediate water. Substantial formation occurs in conditions of instability and eddies, varying from year to year.
Notes:

Journal of Geophysical Research. Vol. 98(C4) :6907-6919 (1993).

Keywords: 551.46 -- Oceanography, physical.
551.465.45 -- Water masses.
551.465.5 -- Ocean currents.
551.464.5 -- Salinity.
551.465.15 -- Turbulence and eddies.
C -- Oceanography, hydrography and hydrology.
(*60) -- Arctic Ocean and adjacent waters.
(*614) -- Greenland waters.
SPRI record no.: 122777

MARCXML

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005 20240328141802.0
007 ta
008 240328s1993####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-122777
040 ## ‡aUkCU-P‡beng‡eaacr
245 00 ‡aFormation of Denmark Strait overflow water by mixing in the East Greenland Current /‡cVolker H. Strass, Eberhard Fahrbach, Ursula Schauer, Lutz Sellman.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 6907-6919 :‡bdiags., tables, map.
500 ## ‡aJournal of Geophysical Research. Vol. 98(C4) :6907-6919 (1993).
520 3# ‡aHydrographic data and current meter records from East Greenland Current collected 1987-1989 near central Greenland Sea reveal formation of water mass with temperature, salinity and density characteristics of Denmark Strait Overflow Water (DSOW). Downstream (SW) flow of this mass can be half DSOW and results from isopycnic mixing of recirculated Atlantic water and Upper Arctic Intermediate water. Substantial formation occurs in conditions of instability and eddies, varying from year to year.
650 07 ‡a551.46 -- Oceanography, physical.‡2udc
650 07 ‡a551.465.45 -- Water masses.‡2udc
650 07 ‡a551.465.5 -- Ocean currents.‡2udc
650 07 ‡a551.464.5 -- Salinity.‡2udc
650 07 ‡a551.465.15 -- Turbulence and eddies.‡2udc
650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local
651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc
651 #7 ‡a(*614) -- Greenland waters.‡2udc
700 1# ‡aStrass, Volker H.
700 1# ‡aFahrbach, Eberhard.
700 1# ‡aSchauer, Ursula.
700 1# ‡aSellman, Lutz.
773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 98(C4) (1993) ‡wSPRI-35252
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240328