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Books on the topic 'Baroclinic'

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Published: 4 June 2021
Last updated: 1 February 2022

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1

Mooers, Christopher N. K., ed. Baroclinic Processes on Continental Shelves. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/co003.

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2

Nataliya, Stashchuk, and Hutter Kolumban, eds. Baroclinic tides: Theoretical modeling and observational evidence. New York: Cambridge University Press, 2005.

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3

Antar, B. N. Three-dimensional baroclinic instability of a Hadley cell for small Richardson number. [Washington, D.C.]: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1985.

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4

Antar, B. N. Three-dimensional baroclinic instability of a Hadley cell for small Richardson number. [Washington, D.C.]: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1985.

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5

Bruner, Barry L. A numerical study of baroclinic circulation in Monterey Bay. Monterey, California: Naval Postgraduate School, 1988.

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6

Smith, Wendy Marie. The effects of double-diffusion on a baroclinic vortex. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1987.

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7

Smith, Wendy Marie. The effects of double-diffusion on a baroclinic vortex. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1987.

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8

Arbic, Brian K. Generation of mid-ocean eddies: The local baroclinic instability hypothesis. Cambridge, Mass: Massachusetts Institute of Technology, 2000.

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9

Arbic, Brian K. Generation of mid-ocean eddies: The local baroclinic instability hypothesis. Cambridge, Mass: Massachusetts Institute of Technology, 2000.

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10

Vennell, M. Ross. The influence of a steady baroclinic deep ocean on the shelf. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1988.

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11

Kamada, Ray. Amending the w* velocity scale for surface layer, entrainment zone, and baroclinic shear in mixed forced/free turbulent convection. Monterey, Calif: Naval Postgraduate School, 1992.

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12

K, Mooers C. N., ed. Baroclinic processes on continental shelves. Washington, D.C: American Geophysical Union, 1986.

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13

University of Arizona. Dept. of Atmospheric Sciences. and United States. National Aeronautics and Space Administration., eds. Computer studies of baroclinic flow: Final report. Tucson, AZ: Dept. of Atmospheric Sciences, University of Arizona, 1985.

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14

Vlasenko, Vasiliy, Nataliya Stashchuk, and Kolumban Hutter. Baroclinic Tides: Theoretical Modeling and Observational Evidence. University of Cambridge ESOL Examinations, 2012.

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15

University of Arizona. Dept. of Atmospheric Sciences and United States. National Aeronautics and Space Administration, eds. Computer studies of baroclinic flow: Final report. Tucson, AZ: Dept. of Atmospheric Sciences, University of Arizona, 1985.

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16

University of Arizona. Dept. of Atmospheric Sciences. and United States. National Aeronautics and Space Administration., eds. Computer studies of baroclinic flow: Final report. Tucson, AZ: Dept. of Atmospheric Sciences, University of Arizona, 1985.

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17

United States. National Aeronautics and Space Administration., ed. Wavenumber selection and hysteresis in nonlinear baroclinic flows. [Washington, D.C: National Aeronautics and Space Administration, 1995.

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18

W, Fowlis William, and United States. National Aeronautics and Space Administration. Scientific and Technical Information Branch., eds. Three-dimensional baroclinic instability of a Hadley cell for small Richardson number. [Washington, D.C.]: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1985.

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19

Sinclair, Mark R. A diagnostic study of baroclinic disturbances in polar air streams. 1985.

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20

United States. National Aeronautics and Space Administration. Scientific and Technical Information Branch., ed. Linear baroclinic instability in the presence of large scale topography. [Washington, DC]: National Aeronautics and Space Administration, Scientific and Technical Information Branch, 1987.

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21

Lee, Dong-kyu. The linear and non-linear baroclinic instability in the eastern North Pacific. 1987.

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22

Lee, Dong-kyu. The linear and non-linear baroclinic instability in the eastern North Pacific. 1987.

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23

Olivier, David A. Numerical simulations of the California Current: Filament formation as related to baroclinic instability. 1987.

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24

Wang, Chunzai. Numerical simulations of nonlinear baroclinic instability with a spherical wave-mean flow model. 1991.

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25

Craig, George C. On the interaction of baroclinic instability and cumulus convection in polar air stream cyclones. 1991.

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26

Zeitlin, Vladimir. Instabilities of Jets and Fronts and their Nonlinear Evolution. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0010.

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Notions of linear and nonlinear hydrodynamic (in)stability are explained and criteria of instability of plane-parallel flows are presented. Instabilities of jets are investigated by direct pseudospectral collocation method in various flow configurations, starting from the classical barotropic and baroclinic instabilities. Characteristic features of instabilities are displayed, as well as typical patterns of their nonlinear saturation. It is shown that in the Phillips model of Chapter 5, new ageostrophic Rossby–Kelvin and shear instabilities appear at finite Rossby numbers. These instabilities are interpreted in terms of resonances among waves counter-propagating in the flow. It is demonstrated that the classical inertial instability is a specific case of ageostrophic baroclinic instability. At the equator it appears also in the barotropic configuration, and is related to resonances of Yanai waves. The nature of the inertial instability in terms of trapped modes is established. A variety of instabilities of density fronts is displayed.
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27

Shapiro, Bruce G. A study of finite difference and finite element vertical discretization schemes for baroclinic prediction equations. 1987.

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28

Sloniker, Donn E. An investigation of finite difference and finite element vertical schemes for the baroclinic prediction equations. 1988.

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29

Zeitlin, Vladimir. Instabilities in Cylindrical Geometry: Vortices and Laboratory Flows. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0011.

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Vortex solutions in cyclo-geostrophic equilibrium are described and their geostrophic and ageostrophic barotropic and baroclinic instabilities are studied along the lines of Chapter 10. Special attention is paid to centrifugal instability which, as the inertial instability of jets, is due to modes trapped in the anticyclonic shear in the vortex, and has asymmetric counterparts. Saturation of this instability is shown to exhibit some specific patterns. Instabilities of intense hurricane-like vortices are analysed and shown to be sensitive to fine details of the vortex profile. Nonlinear saturation of such instabilities exhibits typical secondary meso-vortex structures, and leads to intensification of the vortex. Special attention is paid to instabilities in laboratory flows in rotating cylindrical channels. Classification of these instabilities is given, and their nature, in terms of resonances between different wave modes, is established. Rigid-lid and free-surface configuration with topography are considered and compared with experiments.
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30

Zeitlin, Vladimir. Getting Rid of Fast Waves: Slow Dynamics. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0005.

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After analysis of general properties of horizontal motion in primitive equations and introduction of principal parameters, the key notion of geostrophic equilibrium is introduced. Quasi-geostrophic reductions of one- and two-layer rotating shallow-water models are obtained by a direct filtering of fast inertia–gravity waves through a choice of the time scale of motions of interest, and by asymptotic expansions in Rossby number. Properties of quasi-geostrophic models are established. It is shown that in the beta-plane approximations the models describe Rossby waves. The first idea of the classical baroclinic instability is given, and its relation to Rossby waves is explained. Modifications of quasi-geostrophic dynamics in the presence of coastal, topographic, and equatorial wave-guides are analysed. Emission of mountain Rossby waves by a flow over topography is demonstrated. The phenomena of Kelvin wave breaking, and of soliton formation by long equatorial and topographic Rossby waves due to nonlinear effects are explained.
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31

Zeitlin, Vladimir. Geostrophic Adjustment and Wave–Vortex (Non)Interaction. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0008.

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The fundamental process of geostrophic adjustment is treated by the method of multi-scale asymptotic expansions in Rossby number and fast-time averaging (which is explained), first in the barotropic one-layer case, and then in the baroclinic two-layer case. Together with the standard quasi-geostrophic regime of parameters, the frontal (or semi-) geostrophic regime is considered. Dynamical separation of slow and fast motions is demonstrated in both regimes. The former obey quasi-geostrophic or frontal-geostrophic equations, thus providing formal justification of the heuristic derivation of Chapter 5. Fast motions are inertia-gravity waves in quasi-geostrophic case, and inertial oscillations in the frontal-geostrophic case. Geostrophic adjustment is also considered in the presence of coastal, topographic, and equatorial wave-guides, and, again, separation of fast and slow motions is demonstrated, the latter now including long Kelvin waves in the first case, long topographic waves in the second case, and long Kelvin and Rossby waves in the third case.
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32

Zeitlin, Vladimir. Rotating Shallow-Water Models with Moist Convection. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0015.

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It is shown how the standard RSW can be ’augmented’ to include phase transitions of water. This chapter explains how to incorporate extra (convective) vertical fluxes in the model. By using Lagrangian conservation of equivalent potential temperature condensation of the water vapour, which is otherwise a passive tracer, is included in the model and linked to convective fluxes. Simple relaxational parameterisation of condensation permits the closure of the system, and surface evaporation can be easily included. Physical and mathematical properties of thus obtained model are explained, and illustrated on the example of wave scattering on the moisture front. The model is applied to ’moist’ baroclinic instability of jets and vortices. Condensation is shown to produce a transient increase of the growth rate. Special attention is paid to the moist instabilities of hurricane-like vortices, which are shown to enhance intensification of the hurricane, increase gravity wave emission, and generate convection-coupled waves.
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33

R, Allen D., and United States. National Aeronautics and Space Administration., eds. The 4-day wave as observed from the Upper Atmosphere Research Satellite microwave limb sounder. [Washington, DC: National Aeronautics and Space Administration, 1998.

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