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1968, 6th ed., McGraw-Hill series in mechanical engineering, 747
Book
1955, 1st English ed., McGraw-Hill series in mechanical engineering., 535
Book
1960, 4th ed., McGraw-Hill series in mechanical engineering., 471
Book
1968, Addison-Wesley series in aerospace., ix, 229
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1955, 1st English ed., McGraw-Hill series in mechanical engineering., xx, 535
Book
2000, 8th rev. and enl. ed., ISBN 3540662707, xxiii, 799
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1979, 7th ed. --, McGraw-Hill series in mechanical engineering, ISBN 0070553343, xxii, 817
Book
1960, 4th ed., McGraw-Hill series in mechanical engineering., 647
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1960, 4th ed., McGraw-Hill series in mechanical engineering., 647
Book
1955, McGraw-Hill series in mechanical engineering., xx, 535
Book
1968, 6th ed., McGraw-Hill series in mechanical engineering., ISBN 9780070553293, xix, 747
Book
1999, Applied mathematics and mathematical computation, ISBN 1584880155, Volume 15., 516
Book
2000, Oxford applied and engineering mathematics, ISBN 9780198506751, Volume 3, xiii, 332
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Quarterly Journal of the Royal Meteorological Society, ISSN 0035-9009, 10/2010, Volume 136, Issue 652, pp. 1665 - 1670
In the light of the plethora of definitions for the hurricane boundary layer, we advocate a dynamical definition based on the distribution of agradient flow.... 
tropical cyclone | agradient flow | friction layer | Friction layer | Tropical cyclone | Agradient flow | INTENSITY | DYNAMICS | JETS | MODEL | METEOROLOGY & ATMOSPHERIC SCIENCES | TROPICAL CYCLONE CORE | Fluid dynamics | Mathematical analysis | Vortices | Fluid flow | Aerodynamics | Hurricanes | Boundaries | Boundary layer
Journal Article
1955, University of Maryland. Institute for Fluid Dynamics and Applied Mathematics. Lecture series, no. 33, 27
Book
1955, University of Maryland. Institute for Fluid Dynamics and Applied Mathematics. Lecture series, Volume no. 33, 27
Book
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