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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #122801:
The breakup of shore fast sea ice / Vernon A. Squire.
Title: | The breakup of shore fast sea ice / Vernon A. Squire. |
Author(s): | Squire, Vernon A. |
Date: | 1993. |
In: | Cold Regions Science and Technology. (1993.), Vol. 21(3) (1993) |
Abstract: | Recent theoretical studies of reflection and transmission of ocean waves at shore fast-ice boundary have demonstrated that it is necessary to include complete set of wave modes in open water region and beneath sea ice. Here, studies are extended by including viscosity in model, so that theory conforms to available data. Consequential changes to properties of ice-coupled waves are then reported and, in particular, mechanism for breakup of sea ice plates is proposed which agrees with observations. |
Notes: | Cold Regions Science and Technology. Vol. 21(3) :211-218 (1993). |
Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.2 -- Floating ice, formation and decay. 551.326.7 -- Sea ice. 519.673 -- Modelling. E6 -- Glaciology: floating ice. |
SPRI record no.: | 122801 |
LDR 01319naa#a2200000#a#4500 001 SPRI-122801 005 20231128170840.0 007 ta 008 231128s1993####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-122801 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aSquire, Vernon A. 245 14 ‡aThe breakup of shore fast sea ice /‡cVernon A. Squire. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1993. 300 ## ‡ap. 211-218 :‡bdiags. 500 ## ‡aCold Regions Science and Technology. Vol. 21(3) :211-218 (1993). 520 3# ‡aRecent theoretical studies of reflection and transmission of ocean waves at shore fast-ice boundary have demonstrated that it is necessary to include complete set of wave modes in open water region and beneath sea ice. Here, studies are extended by including viscosity in model, so that theory conforms to available data. Consequential changes to properties of ice-coupled waves are then reported and, in particular, mechanism for breakup of sea ice plates is proposed which agrees with observations. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.2 -- Floating ice, formation and decay.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡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# ‡a20231128