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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #112482:

An initial numerical investigation of the extent of sea-ice ridging / Gregory M. Flato, William D. Hibler, III.

Title: An initial numerical investigation of the extent of sea-ice ridging / Gregory M. Flato, William D. Hibler, III.
Author(s): Flato, Gregory M.
Hibler, William D.,
Date: 1991.
In: Annals of Glaciology. (1991.), Vol. 15 (1991)
Abstract: Two-level, viscoplastic, sea-ice model is modified to allow ridged and unridged ice to be treated separately, by introducing third continuity equation with additional terms to transform level ice into ridged ice during deformation. Standard model is run for three years using observed forcing from 1981-83, along with three sensitivity runs, to investigate ridge production.
Notes:

Annals of Glaciology. Vol. 15 :31-36 (1991).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.326.3 -- Floating ice, structure and surface features.
519.673 -- Modelling.
539.3 -- Ice, mechanical properties.
E6 -- Glaciology: floating ice.
SPRI record no.: 112482

MARCXML

LDR 01315naa#a2200000#a#4500
001 SPRI-112482
005 20240221021124.0
007 ta
008 240221s1991####xx#ab#|##|###|0||#0|eng#d
035 ## ‡aSPRI-112482
040 ## ‡aUkCU-P‡beng‡eaacr
100 1# ‡aFlato, Gregory M.
245 13 ‡aAn initial numerical investigation of the extent of sea-ice ridging /‡cGregory M. Flato, William D. Hibler, III.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1991.
300 ## ‡ap. 31-36 :‡bdiags., maps.
500 ## ‡aAnnals of Glaciology. Vol. 15 :31-36 (1991).
520 3# ‡aTwo-level, viscoplastic, sea-ice model is modified to allow ridged and unridged ice to be treated separately, by introducing third continuity equation with additional terms to transform level ice into ridged ice during deformation. Standard model is run for three years using observed forcing from 1981-83, along with three sensitivity runs, to investigate ridge production.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.326.3 -- Floating ice, structure and surface features.‡2udc
650 07 ‡a519.673 -- Modelling.‡2udc
650 07 ‡a539.3 -- Ice, mechanical properties.‡2udc
650 07 ‡aE6 -- Glaciology: floating ice.‡2local
700 1# ‡aHibler, William D.,‡cIII.
773 0# ‡7nnas ‡tAnnals of Glaciology. ‡gVol. 15 (1991) ‡wSPRI-60773
917 ## ‡aUnenhanced record from Muscat, imported 2019
948 3# ‡a20240221