By Walker O. Smith Jr.

Polar Oceanography is an built-in synthesis of the organic, actual, geological, and chemical methods that ensue within the polar oceans. The booklet represents the 1st smooth interdisciplinary synthesis during this box

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A. 1970. The mathematical representation of wind speed, and temperature profiles in the unstable atmospheric surface layer. J. Appl. Math. 9: 857-861. Pease, C. H. 1987. The size of wind-driven coastal polynyas. /. Geophys. Res. 92:7040-7059. 46 Robert A. Brown Pease, C. , S. A. Salo & J. E. Overland. 1983. Drag measurements forfirst-yearsea ice over a shallow sea. J. Geophys. Res. 88: 2853-2862. Prandtl, L. 1904. Überflussigkeitsbewegungbei sehr kleiner reibung. Proc. Int. Math. , 3rd, Heidelberg.

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Cavalieri, D. J. & C. L. Parkinson. 1981. Large-scale variations in observed Antarctic sea ice extent and associated atmospheric circulation. Mon. Weather Rev. 109: 2323-2336. Clark, R. H. 1970. Observational studies in the atmospheric boundary layer. R. Meteorol. Soc. 96:91-114. Clark, R. H. & G. D. Hess. 1974. Geostrophic departure and the functions A and B of Rossbynumber similarity theory. Boundary-Layer Meteorol. 7:267-287. Crane, R. G. 1978. Seasonal variations of sea ice extent in the Davis Strait-Labrador Sea area and relationships with synoptic-scale atmospheric circulation.

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