By Matthias Tomczak, J. Stuart Godfrey
`The Tomczak and Godfrey textbook on nearby oceanography is especially appreciated... The chapters specialise in ocean weather concerns yet supply a easy appreciation of local oceanography that may serve all these attracted to the ocean...While thetextbook is geared to the undergraduate, it comprises adequate element for the pro oceanographer and graduate student.' Bulletin of the yank Meteorological Society 'It is a superb textual content for either scholars and researchers looking a descriptionof ocean physics and i've no hesitation in recommending it ... Tomczak and Godfrey current an outline of the oceans that's equipped on a minimal, but enough, set of actual and mathematical ideas ... the normal of presentation and enhancing ishigh all through this e-book ... The e-book is very good researched' - Australian Meteorological journal 'an very good e-book for either the newbie climatologist who must learn about the ocean.' - foreign magazine of Climatology
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Additional info for Regional Oceanography: An Introduction
A useful quantity for the description of the oceanic circulation is mass transport. The basic definition is M* = ρ v . 1) Here, M* is the mass transport through an area of unit width (1 m 2 ) perpendicular to the direction of the flow and v the velocity vector with components (u,v,w) along the (x,y,z) axes. M* is therefore a vector which points in the same direction as velocity and has units of mass per unit area and unit time, or kg m-2 s-1. e. integrated over the width and the depth of the current.
C) The corresponding map of steric height at constant pressure p = p 1 . The diagram requires some study, but it is well worth it; understanding these principles is the basis for the interpretation of many features found in the oceanic circulation. 0 (December 2001) 26 Regional Oceanography: an Introduction A quantity widely found in oceanographic literature is the dynamic height D. e. the product of gravity and steric height. Maps of dynamic height, also known as dynamic topography maps, are therefore maps of steric height scaled by the factor g or pressure maps scaled by the factor ρo .
The western boundary currents (Gulf Stream, Brazil Current, Kuroshio, East Australian Current, Agulhas Current) and the Circumpolar Current stand out as regions of particularly high eddy energy. Eddies in these regions are so energetic that the associated currents can reverse the direction of flow. In the western boundary currents they turn the water movement from poleward to equatorward; poleward mean flow is only observed if the study area is larger than the typical eddy size, which is of the order of 200 km diameter.
Regional Oceanography: An Introduction by Matthias Tomczak, J. Stuart Godfrey