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Record #176349:
- #176349
Main publication details
MARC recordA coupled coastal polynya-atmospheric boundary layer model / I.A. Walkington, A.J. Willmott.
| Title: | A coupled coastal polynya-atmospheric boundary layer model / I.A. Walkington, A.J. Willmott. |
| Author(s): | Walkington, I. A. Willmott, A. J. |
| Date: | 2006. |
| In: | Journal of Physical Oceanography. (2006.), Vol. 36(5) (2006) |
| Abstract: | Presents opening solutions of one-dimensional coastal polynya flux model in which frazil ice is characterised by depth and concentration. In comparison with polynya flux models in which variable frazil ice concentration is absent, model predicts smaller heat flux to atmosphere. Model exhibits wider steady-state polynya and longer opening times compared with models in which ice concentration is neglected. When coupled to lower-atmosphere boundary layer model, model demonstrates that polynya opening time and steady-state width are significantly altered in coupled, as compared with decoupled, system. |
| Notes: | Journal of Physical Oceanography. Vol. 36(5) :897-913 (2006). |
| Keywords: | 519.673 -- Modelling. 536.2 -- Heat, transmission. 551.326 -- Floating ice. 551.326.31 -- Polynyas. 551.328.4 -- Frazil ice. 551.46 -- Oceanography, physical. 551.463 -- Sea water, physical properties. 551.524 -- Air temperature. C -- Oceanography, hydrography and hydrology. (*3) -- Arctic regions. (*49) -- Alaska. (*495.6) -- St. Lawrence Island. |
| SPRI record no.: | 176349 |
LDR 01776naa#a2200000#a#4500 001 SPRI-176349 005 20231203075100.0 007 ta 008 231203s2006####xx#a##|##|###|0||#0|eng#d 035 ## ‡aSPRI-176349 040 ## ‡aUkCU-P‡beng‡eaacr 100 1# ‡aWalkington, I. A. 245 12 ‡aA coupled coastal polynya-atmospheric boundary layer model /‡cI.A. Walkington, A.J. Willmott. 260 ## ‡a[S.l.] :‡b[s.n.],‡c2006. 300 ## ‡ap. 897-913 :‡bill., diags., tables. 500 ## ‡aJournal of Physical Oceanography. Vol. 36(5) :897-913 (2006). 520 3# ‡aPresents opening solutions of one-dimensional coastal polynya flux model in which frazil ice is characterised by depth and concentration. In comparison with polynya flux models in which variable frazil ice concentration is absent, model predicts smaller heat flux to atmosphere. Model exhibits wider steady-state polynya and longer opening times compared with models in which ice concentration is neglected. When coupled to lower-atmosphere boundary layer model, model demonstrates that polynya opening time and steady-state width are significantly altered in coupled, as compared with decoupled, system. 650 07 ‡a519.673 -- Modelling.‡2udc 650 07 ‡a536.2 -- Heat, transmission.‡2udc 650 07 ‡a551.326 -- Floating ice.‡2udc 650 07 ‡a551.326.31 -- Polynyas.‡2udc 650 07 ‡a551.328.4 -- Frazil ice.‡2udc 650 07 ‡a551.46 -- Oceanography, physical.‡2udc 650 07 ‡a551.463 -- Sea water, physical properties.‡2udc 650 07 ‡a551.524 -- Air temperature.‡2udc 650 07 ‡aC -- Oceanography, hydrography and hydrology.‡2local 651 #7 ‡a(*3) -- Arctic regions.‡2udc 651 #7 ‡a(*49) -- Alaska.‡2udc 651 #7 ‡a(*495.6) -- St. Lawrence Island.‡2udc 700 1# ‡aWillmott, A. J. 773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 36(5) (2006) ‡wSPRI-78712 916 ## ‡aJW 917 ## ‡aUnenhanced record from Muscat, imported 2019 948 3# ‡a20231203 ‡bJW