Scott Polar Research InstituteSPRI library catalogue
Search the catalogue
Browse recordsView 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 It is no longer being updated, so does not reliably reflect our current library holdings.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 #110175:
- #110175
Main publication details
MARC recordA two-dimensional thermodynamic model for sea ice advance and retreat in the Newfoundland marginal ice zone / C.L. Tang.
| Title: | A two-dimensional thermodynamic model for sea ice advance and retreat in the Newfoundland marginal ice zone / C.L. Tang. |
| Author(s): | Tang, C. L. |
| Date: | 1991. |
| In: | Journal of Geophysical Research. (1991.), Vol. 96(C3) (1991) |
| Abstract: | Emphasis is on time-dependent and two-dimensional aspects of ice decay and oceanic response to ice movement. Goal is to apply model to Newfoundland shelf using realistic input parameters to study variability of ice. For this reason, extensive set of variables are included in model: ice and snow thicknesses, ice concentration, mixed-layer depth, stratification in lower layer, air temperature and atmospheric heat fluxes, and precipitation. |
| Notes: | Journal of Geophysical Research. Vol. 96(C3) :4723-4737 (1991). |
| Keywords: | 519.673 -- Modelling. 551.326.7 -- Sea ice. 551.326.2 -- Floating ice, formation and decay. 551.326 -- Floating ice. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*61) -- North Atlantic Ocean. |
| SPRI record no.: | 110175 |
LDR 01399naa#a2200000#a#4500 001 SPRI-110175 005 20231201035327.0 007 ta 008 231201s1991####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-110175 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aTang, C. L. 245 12 ‡aA two-dimensional thermodynamic model for sea ice advance and retreat in the Newfoundland marginal ice zone /‡cC.L. Tang. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1991. 300 ## ‡ap. 4723-4737 :‡bdiags., tables, map. 500 ## ‡aJournal of Geophysical Research. Vol. 96(C3) :4723-4737 (1991). 520 3# ‡aEmphasis is on time-dependent and two-dimensional aspects of ice decay and oceanic response to ice movement. Goal is to apply model to Newfoundland shelf using realistic input parameters to study variability of ice. For this reason, extensive set of variables are included in model: ice and snow thicknesses, ice concentration, mixed-layer depth, stratification in lower layer, air temperature and atmospheric heat fluxes, and precipitation. 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326.2 -- Floating ice, formation and decay.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 96(C3) (1991) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231201