skip to primary navigation skip to content
 

 

You are not currently logged in

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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #122802:

A comparison of the mass-loading and elastic plate models of an ice field / Vernon A. Squire.

Title: A comparison of the mass-loading and elastic plate models of an ice field / Vernon A. Squire.
Author(s): Squire, Vernon A.
Date: 1993.
In: Cold Regions Science and Technology. (1993.), Vol. 21(3) (1993)
Abstract: Compares two most common surface boundary conditions used to represent marginal ice zone through which ocean waves are propagating. Discusses consequences of choosing one or other boundary condition: with no rigidity, wavelength in ice is less than that in open sea, whereas with rigidity typical of ice plate, it is usually greater. This has concomitant effect that waves bend towards normal incidence at entry to ice field in mass-loading theory, but bend away when ice field is assumed to behave as elastic plate, thereby allowing critical angle of incidence beyond which incoming waves cannot enter ice cover. Existing data indicate that critical angle does occur, suggesting that full plate theory may be necessary.
Notes:

Cold Regions Science and Technology. Vol. 21(3) :219-229 (1993).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.466 -- Waves and tides, marine.
519.673 -- Modelling.
E6 -- Glaciology: floating ice.
SPRI record no.: 122802

MARCXML

LDR 01567naa#a2200000#a#4500
001 SPRI-122802
005 20240329054825.0
007 ta
008 240329s1993####xx#a##|##|###|0||#0|eng#d
035 ## ‡aSPRI-122802
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aSquire, Vernon A.
245 12 ‡aA comparison of the mass-loading and elastic plate models of an ice field /‡cVernon A. Squire.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1993.
300 ## ‡ap. 219-229 :‡bdiags.
500 ## ‡aCold Regions Science and Technology. Vol. 21(3) :219-229 (1993).
520 3# ‡aCompares two most common surface boundary conditions used to represent marginal ice zone through which ocean waves are propagating. Discusses consequences of choosing one or other boundary condition: with no rigidity, wavelength in ice is less than that in open sea, whereas with rigidity typical of ice plate, it is usually greater. This has concomitant effect that waves bend towards normal incidence at entry to ice field in mass-loading theory, but bend away when ice field is assumed to behave as elastic plate, thereby allowing critical angle of incidence beyond which incoming waves cannot enter ice cover. Existing data indicate that critical angle does occur, suggesting that full plate theory may be necessary.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.466 -- Waves and tides, marine.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
773 0# ‡7nnas ‡tCold Regions Science and Technology. ‡gVol. 21(3) (1993) ‡wSPRI-59075
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240329