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Record #97034:
- #97034
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MARC recordA simple steady-state coupled ice-ocean model, with application to the Greenland-Norwegian sea / Andrew J. Willmott, Lawrence A. Mysak.
| Title: | A simple steady-state coupled ice-ocean model, with application to the Greenland-Norwegian sea / Andrew J. Willmott, Lawrence A. Mysak. |
| Author(s): | Willmott, Andrew J. Mysak, Lawrence A. |
| Date: | 1989. |
| In: | Journal of Physical Oceanography. (1989.), Vol. 19(4) (1989) |
| Abstract: | Thermodynamic reduced-gravity ocean model forced by steady-state surface wind stress and Haney-type heat flux was used to determine climatological ice-edge position, ice thickness, ocean circulation, and upper-ocean temperature in high-latitude meridional channel. Model is applied to Greenland and Norwegian seas, between 60 and 80°N, and between east coast of Greenland and 15°E. Exterior to narrow western boundary layer, predicted ice-edge position compares favourably with climatological 90% ice-concentration isoline obtained from analysis of 32 years of Arctic sea-ice data. |
| Notes: | Journal of Physical Oceanography. Vol. 19(4) :501-518 (1989). |
| Keywords: | 551.465.7 -- Oceanography, energy budget. 551.32 -- Glaciology. 551.326 -- Floating ice. 551.326.7 -- Sea ice. 519.673 -- Modelling. E6 -- Glaciology: floating ice. (*60) -- Arctic Ocean and adjacent waters. (*617) -- Greenland Sea and Fram Strait. (*615) -- Norwegian Sea. |
| SPRI record no.: | 97034 |
LDR 01654naa#a2200000#a#4500 001 SPRI-97034 005 20240418215849.0 007 ta 008 240418s1989####xx#ab#|##|###|0||#0|eng#d 035 ## ‡aSPRI-97034 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aWillmott, Andrew J. 245 12 ‡aA simple steady-state coupled ice-ocean model, with application to the Greenland-Norwegian sea /‡cAndrew J. Willmott, Lawrence A. Mysak. 260 ## ‡a[S.l.] :‡b[s.n.],‡c1989. 300 ## ‡ap. 501-518 :‡bdiag., map. 500 ## ‡aJournal of Physical Oceanography. Vol. 19(4) :501-518 (1989). 520 3# ‡aThermodynamic reduced-gravity ocean model forced by steady-state surface wind stress and Haney-type heat flux was used to determine climatological ice-edge position, ice thickness, ocean circulation, and upper-ocean temperature in high-latitude meridional channel. Model is applied to Greenland and Norwegian seas, between 60 and 80°N, and between east coast of Greenland and 15°E. Exterior to narrow western boundary layer, predicted ice-edge position compares favourably with climatological 90% ice-concentration isoline obtained from analysis of 32 years of Arctic sea-ice data. 650 07 ‡a551.465.7 -- Oceanography, energy budget.‡2udc 650 07 ‡a551.32 -- Glaciology.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.7 -- Sea ice.‡2udc 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡aE6 -- Glaciology: floating ice.‡2local 651 #7 ‡a(*60) -- Arctic Ocean and adjacent waters.‡2udc 651 #7 ‡a(*617) -- Greenland Sea and Fram Strait.‡2udc 651 #7 ‡a(*615) -- Norwegian Sea.‡2udc 700 1# ‡aMysak, Lawrence A. 773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 19(4) (1989) ‡wSPRI-78712 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20240418