Geoscience Reference
In-Depth Information
References
Barenblatt, G. I.: Scaling, Self-Similarity, and Intermediate Asymptotics. Cambridge University
Press, Cambridge (1996)
Batchelor, G. K.: The Theory of Homogeneous Turbulence. Cambridge University Press,
Cambridge (1967)
Bloomfield, P.:Fourier Analysis of Time Series: An Introduction. Wiley, New York (1976)
Bowker, A. H. and Lieberman, G. J.: Engineering Statistics. Prentice-Hall, Englewood Cliffs,
NJ (1959)
Busch, N. E. and Panofsky, H. A.: Recent spectra of atmospheric turbulence. Quart. J. R. Met.
Soc., 94, 132-147 (1968)
Edson, J. B., Fairall, C. W., Mestayer, P. G., and Larsen, S. E.: A study of the inertial-dissipation
method for computing air-sea fluxes. J. Geophys. Res., 96, 10689-10711 (1991)
Efron, B. and Gong, G.:A leisurely look at the bootstrap, thejackknife, and cross-validation. Am.
Statistician, 37, 36-48 (1983)
Emery, W. J. and Thomson, R. E.: Data Analysis Methods in Physical Oceanography, Second and
Revised Edition. Elsevier, Amsterdam (2001)
Frisch, U.:Turbulence. Cambridge University Press, Cambridge (1995)
Hinze, J.O.:Turbulence, Second Edition.McGraw-Hill,New York (1975)
Jenkins, G. M. and Watts, D. G.: Spectral Analysis and Its Applications. Holden-Day, San Fran-
cisco (1968)
McPhee, M. G.: Greenland Sea Ice/Ocean Margin. EOS, Trans. Am. Geophys. Union, 64 (9), 82-
83 (1983)
McPhee, M. G.: On the Turbulent Mixing Length in the Oceanic Boundary Layer. J. Phys.
Oceanogr., 24, 2014-2031 (1994)
McPhee, M. G.: A spectral technique for estimating turbulent stress, scalar flux magnitude, and
eddy viscosity in the ocean boundary layer under pack ice. J. Phys. Oceanogr., 34, 2180-
2188 (2004)
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. and Stanton, T. P.: Turbulence in the statically unstable oceanic boundary layer
under Arctic leads. J. Geophys. Res., 101, 6409-6428 (1996)
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)
McPhee,M.G.,Morison,J.H.,andNilsen,F.:Revisitingheatandsaltexchangeattheice-oceanin-
terface:Oceanfluxandmodelingconsiderations.J.Geophys.Res.,doi:10.1029/2007JC004383,
in press (2008)
Tennekes, H. and Lumley, J. L.: AFirst Course inTurbulence. MIT, Cambridge, MA(1972)
Nomenclature
c
p
Specificheatofseawateratconstantpressure(approx.4
.
0
×
10
3
Jkg
−
1
K
−
1
forseawateratfreezing)
w
T
Covarianceestimateofkinematicturbulentheatflux
u
w
+
v
w
τ
=
i
ComplexformofkinematicReynoldsstress
1
/
2
u
∗
=
|
τ
|
Frictionspeed(local)
10
−
5
rads
−
1
Ω
Angularvelocityoftheearth
(
7
.
292
×
)
δ
ij
Kroneckerdelta
