SPRI library catalogue
View a record
Please note: You are viewing the legacy database of the Scott Polar Research Institute Library catalogue. It is no longer being updated, so does not reliably reflect our current library holdings.
Please search for material in iDiscover for up-to-date information about the library collection.
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 |
LDR 01505naa#a2200000#a#4500 001 SPRI-91909 005 20240328181957.0 007 ta 008 240328s1988####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-91909 040 ## ‡aUkCU-P‡beng‡eaacr 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