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Record #91909:

A numerical study of mesoscale ocean eddy interaction with a marginal ice zone / David C. Smith, IV, Arlene A. Bird, W. Paul Budgell.

Title: A numerical study of mesoscale ocean eddy interaction with a marginal ice zone / David C. Smith, IV, Arlene A. Bird, W. Paul Budgell.
Author(s): Smith, David C.,
Bird, Arlene A.
Budgell, W. Paul.
Date: 1988.
In: Journal of Geophysical Research. (1988.), Vol. 93(C10) (1988)
Abstract: Based on observations made during marginal ice zone experiment in Greenland Sea. Results obtained with two-layer nonlinear primitive equation ocean model and coupled free-drift ice model. In absence of winds, ice equilibrates rapidly to ocean-eddy velocity, resulting in radial ice motion. Ocean sea-surface slope provides important force in ice momentum balance in no-wind simulations. With along-ice edge winds of 10 m s⁻¹, ice responds largely to wind and, to lesser extent, to ocean eddy. Under ice, ocean eddy can be rapidly eroded by wind-driven ice motion.
Notes:

Journal of Geophysical Research. Vol. 93(C10) :12, 461-12, 473 (1988).

Keywords: 551.466 -- Waves and tides, marine.
551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.14 -- Floating ice, movement.
E6 -- Glaciology: floating ice.
SPRI record no.: 91909

MARCXML

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100 1# ‡aSmith, David C.,‡cIV.
245 12 ‡aA numerical study of mesoscale ocean eddy interaction with a marginal ice zone /‡cDavid C. Smith, IV, Arlene A. Bird, W. Paul Budgell.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1988.
300 ## ‡ap. 12, 461-12, 473 :‡bdiags., tables.
500 ## ‡aJournal of Geophysical Research. Vol. 93(C10) :12, 461-12, 473 (1988).
520 3# ‡aBased on observations made during marginal ice zone experiment in Greenland Sea. Results obtained with two-layer nonlinear primitive equation ocean model and coupled free-drift ice model. In absence of winds, ice equilibrates rapidly to ocean-eddy velocity, resulting in radial ice motion. Ocean sea-surface slope provides important force in ice momentum balance in no-wind simulations. With along-ice edge winds of 10 m s⁻¹, ice responds largely to wind and, to lesser extent, to ocean eddy. Under ice, ocean eddy can be rapidly eroded by wind-driven ice motion.
650 07 ‡a551.466 -- Waves and tides, marine.‡2udc
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
700 1# ‡aBird, Arlene A.
700 1# ‡aBudgell, W. Paul.
773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 93(C10) (1988) ‡wSPRI-35252
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240328