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Record #129392:

A nonlinear steady-state model of the North Water Polynya, Baffin Bay / M.S. Darby, Andrew J. Willmott, Lawrence A. Mysak.

Title: A nonlinear steady-state model of the North Water Polynya, Baffin Bay / M.S. Darby, Andrew J. Willmott, Lawrence A. Mysak.
Author(s): Darby, M. S.
Willmott, Andrew J.
Mysak, Lawrence A.
Date: 1994.
In: Journal of Physical Oceanography. (1994.), Vol. 24(5) (1994)
Abstract: Presents model based on that of Mysak and Huang (ibid., 1992, 22(6) :596-608), but extended in several ways: finite amplitude displacements of upper-layer thickness are allowed; channel walls diverge to south; sensible-heat flux from lower layer is physically well defined in terms of vertical entrainment velocity; and free-drifting frazil ice to north of ice edge of North Water polynya is allowed to nove to right of northerly winds. Discusses results; one is that with exception of late spring, asymptotic southern ice-edge position of polynya can be simulated in terms of latent heat model alone.
Notes:

Journal of Physical Oceanography. Vol. 24(5) :1011-1020 (1994).

Keywords: 551.32 -- Glaciology.
551.326 -- Floating ice.
551.326.7 -- Sea ice.
551.326.31 -- Polynyas.
551.465 -- Oceanography, dynamics.
.000(410) -- British author.
519.673 -- Modelling.
E6 -- Glaciology: floating ice.
(*60) -- Arctic Ocean and adjacent waters.
(*624) -- Baffin Bay and Davis Strait.
SPRI record no.: 129392

MARCXML

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245 12 ‡aA nonlinear steady-state model of the North Water Polynya, Baffin Bay /‡cM.S. Darby, Andrew J. Willmott, Lawrence A. Mysak.
260 ## ‡a[S.l.] :‡b[s.n.],‡c1994.
300 ## ‡ap. 1011-1020 :‡bdiags., map.
500 ## ‡aJournal of Physical Oceanography. Vol. 24(5) :1011-1020 (1994).
520 3# ‡aPresents model based on that of Mysak and Huang (ibid., 1992, 22(6) :596-608), but extended in several ways: finite amplitude displacements of upper-layer thickness are allowed; channel walls diverge to south; sensible-heat flux from lower layer is physically well defined in terms of vertical entrainment velocity; and free-drifting frazil ice to north of ice edge of North Water polynya is allowed to nove to right of northerly winds. Discusses results; one is that with exception of late spring, asymptotic southern ice-edge position of polynya can be simulated in terms of latent heat model alone.
650 07 ‡a551.32 -- Glaciology.‡2udc
650 07 ‡a551.326 -- Floating ice.‡2udc
650 07 ‡a551.326.7 -- Sea ice.‡2udc
650 07 ‡a551.326.31 -- Polynyas.‡2udc
650 07 ‡a551.465 -- Oceanography, dynamics.‡2udc
650 07 ‡a.000(410) -- British author.‡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(*624) -- Baffin Bay and Davis Strait.‡2udc
700 1# ‡aWillmott, Andrew J.
700 1# ‡aMysak, Lawrence A.
773 0# ‡7nnas ‡tJournal of Physical Oceanography. ‡gVol. 24(5) (1994) ‡wSPRI-78712
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