Geoscience Reference
In-Depth Information
Martin, S., Kauffman, P., and Parkinson, C.: The movement and decay of ice edge bands in the
winter bering sea. J. Geophys. Res., 88, 2803-2812 (1983)
McPhee, M. G.:The effect of theoceanic boundary layer on the mean drift of sea ice: Application
of a simple model. J. Phys. Oceanogr., 9, 388-400 (1979)
McPhee,M.G.:Ananalyticsimilaritytheoryfortheplanetaryboundarylayerstabilizedbysurface
buoyancy. Boundary-Layer Meterol., 21, 325-339 (1981)
McPhee, M. G.:Turbulent heat and momentum transfer inthe oceanic boundary layer under melt-
ing pack ice. J. Geophys. Res., 88, 2827-2835 (1983)
McPhee, M. G.: Physics of early summer ice/ocean exchanges in the western Weddell Sea during
ISPOL, Deep-Sea Res., II, doi:10.1016/j.dsr2.2007.12.022, in press (2008)
McPhee, M. G., Kottmeier, C., and Morison, J. H.: Ocean heat flux in the central Weddell Sea in
winter. J. Phys. Oceanogr., 29, 1166-1179 (1999)
McPhee,M.G.andMartinson,D.G.:TurbulentmixingunderdriftingpackiceintheWeddellSea.
Science, 263, 218-221 (1994)
McPhee, M. G. and Smith, J. D.: Measurements of the turbulent boundary layer under pack ice. J.
Phys. Oceanogr., 6, 696-711 (1976)
McPhee, M. G., Maykut, G. A., and Morison, J. H.: Dynamics and thermodynamics of the
ice/upper ocean system in the marginal ice zone of the Greenland Sea. J. Geophys. Res., 92,
7017-7031 (1987)
Mellor, G. L., McPhee, M. G., and Steele, M.: Ice-seawater turbulent boundary layer interaction
withmeltingorfreezing. J. Phys. Oceanogr., 16, 1829-1846 (1986)
Obukhov, A. M.: Turbulence in an atmosphere with a non-uniform temperature. Boundary-Layer
Meteorol., 2, 7-29 (1971)
Wadhams, P.: A mechanism for the formation of ice edge bands. J. Geophys. Res., 88, 2813-
2818 (1983)
Nomenclature
φ
m
Dimensionlesscurrent(wind)shear
κ
Von K´arm´an'sconstant(0.4)
ξ
Dimensionlessverticalcoordinate(z/H)
Φ
Complexdimensionlesscurrentshear
z
0
Surfaceroughnesslength
u
∗
0
3
w
b
0
)
L
0
Obukhovlengthscale basedonboundaryfluxes
L
0
=
/
(
κ
ζ
Surfacelayerdimensionlessverticalcoordinate
ζ
=
z
/
L
0
λ
sl
Surface-layermixinglength,
κ
z
/
φ
m
λ
max
Maximummixinglengthin theIOBL
U
0
Complexdimensionlesssurfacevelocity
V
s
/
u
∗
0
Ro
∗
Surface-frictionRossbynumber
(
u
∗
0
/
f
)
/
z
0
A
and
B
Rossby-similarityfunctions
Λ
∗
Similarityparameter
R
c
CriticalfluxRichardsonnumber(0.2)
µ
∗
Stabilityparameter
(
u
∗
0
/
f
)
/
L
0
η
∗
Similarityscale factorforthestablystratified IOBL