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- W2479800322 abstract "Although we will be mostly interested in turbulent conditions, it is instructive to consider weaker solutions near theonset of convection. Without rotation, convection occurs inthe form of roll pairs with up-ow and down-ow regionsalternating periodically in space. With rotation, bulk convection is suppressed, and the form of the convection is substantially modied into vortical structures such as illustrated inFigure 38.1, where black shading indicates cyclonic (with therotation direction) circulation and gray shading indicates anticyclonic (counter to the rotation direction) circulation. esense of the rotation of the ow is determined by the action ofthe Coriolis force on ow that is either converging or diverging38.1 Introduction 50538.2Principles 50738.3Examples 50838.4Methods of Analysis 51038.5Major Challenges 512References 512" @default.
- W2479800322 created "2016-08-23" @default.
- W2479800322 creator A5085610187 @default.
- W2479800322 date "2012-12-12" @default.
- W2479800322 modified "2023-10-14" @default.
- W2479800322 title "Sediment Transport ................................................................................................................................................ Jørgen Fredsøe" @default.
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- W2479800322 doi "https://doi.org/10.1201/b14241-42" @default.
- W2479800322 hasPublicationYear "2012" @default.
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