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Record #104033:
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MARC recordA model of sea ice and the upper ocean mixed layer off Labrador / T. Yao, M. Ikeda.
| Title: | A model of sea ice and the upper ocean mixed layer off Labrador / T. Yao, M. Ikeda. |
| Author(s): | Yao, T. Ikeda, M. |
| Date: | 1990. |
| In: | Journal of Geophysical Research. (1990.), Vol. 95(C7) (1990) |
| Abstract: | Existing dynamic/thermodynamic ice model is coupled to existing bulk mixed-layer model of upper ocean, and applied to seasonal evolution of ice in marginal ice zone off Labrador. Coupled model simulates growth phase of ice and evolution of upper ocean temperature and salinity quite well. Results show that mixed-layer deepening can account for offshore ice extent. Southern extent of ice is influenced more by meridional gradients in atmospheric heat flux and ocean heat content. Lateral advection within ocean is important in determining southern ice extent. |
| Notes: | Journal of Geophysical Research. Vol. 95(C7) :11, 603-11, 612 (1990). |
| Keywords: | 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 551.326.1 -- Floating ice, distribution and movement. 551.326.12 -- Floating ice, distribution, seasonal. 551.326.14 -- Floating ice, movement. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*62) -- Canadian Arctic waters. (*620) -- Labrador Sea. (*61) -- North Atlantic Ocean. |
| SPRI record no.: | 104033 |
LDR 01709naa#a2200000#a#4500 001 SPRI-104033 005 20230327201512.0 007 ta 008 230327s1990####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-104033 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aYao, T. 245 12 ‡aA model of sea ice and the upper ocean mixed layer off Labrador /‡cT. Yao, M. Ikeda. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1990. 300 ## ‡ap. 11, 603-11, 612 :‡bdiags., map. 500 ## ‡aJournal of Geophysical Research. Vol. 95(C7) :11, 603-11, 612 (1990). 520 3# ‡aExisting dynamic/thermodynamic ice model is coupled to existing bulk mixed-layer model of upper ocean, and applied to seasonal evolution of ice in marginal ice zone off Labrador. Coupled model simulates growth phase of ice and evolution of upper ocean temperature and salinity quite well. Results show that mixed-layer deepening can account for offshore ice extent. Southern extent of ice is influenced more by meridional gradients in atmospheric heat flux and ocean heat content. Lateral advection within ocean is important in determining southern ice extent. 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a551.326.1 -- Floating ice, distribution and movement.‡2udc 650 07 ‡a551.326.12 -- Floating ice, distribution, seasonal.‡2udc 650 07 ‡a551.326.14 -- Floating ice, movement.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*62) -- Canadian Arctic waters.‡2udc 651 #7 ‡a(*620) -- Labrador Sea.‡2udc 651 #7 ‡a(*61) -- North Atlantic Ocean.‡2udc 700 1# ‡aIkeda, M. 773 0# ‡7nnas ‡tJournal of Geophysical Research. ‡gVol. 95(C7) (1990) ‡wSPRI-35252 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20230327