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Books on the topic 'Rossby and Kelvin waves'

Author: Grafiati
Published: 4 June 2021
Last updated: 6 February 2022

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1

Volland, Hans. Atmospheric tidal and planetary waves. Kluwer Academic Publishers, 1988.

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2

John, Stanford. Rossby-gravity waves in tropical total ozone data. National Aeronautics and Space Administration, 1993.

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3

John, Stanford. Rossby-gravity waves in tropical total ozone data. National Aeronautics and Space Administration, 1993.

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4

Chiu, Ching-Sang. Estimation of planetary wave parameters from the data of the 1981 Ocean Acoustic Tomography Experiment. Woods Hole Oceanographic Institution, 1985.

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5

Kessler, William S. Observations of long Rossby waves in the northern tropical Pacific. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1989.

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6

Kelley, Michael C. Aspects of weather and space weather in the earth's upper atmosphere: The role of internal atmospheric waves. National Academy Press, 1997.

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7

Haack, Tracy. Mixed convective/dynamic roll vortices and their effects on initial wind and temperature profiles. Dept. of Meteorology, Pennsylvania State University, 1991.

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8

Barnell, Alexander. Far-field features of the Kelvin wake. David W. Taylor Naval Ship Research and Development Center, 1986.

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9

Grigorkina, R. G. Vozdeĭstvie taĭfunov na okean. Gidrometeoizdat, 1986.

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10

Grigorkina, R. G. Vozdeĭstvie taĭfunov na okean. Gidrometeoizdat, 1986.

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11

Swart, H. E. de. Vacillation and predictability properties of low-order atmospheric spectral models. Centrum voor Wiskunde en Informatica, 1989.

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12

Zhu, Yong. Geostrophic wave circulations. 2nd ed. New Knowledge Pub., 2002.

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13

N, Snezhkin E., ред. Vikhri Rossbi i spiralʹnye struktury: Astrofizika i fizika plazmy v opytakh na melkoĭ vode. "Nauka," Glav. red. fiziko-matematicheskoĭ lit-ry, 1990.

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14

Goretzki, Bernd. Untersuchungen zur Ausbreitung und Entwicklung von Rossby-Wellen in einem dreidimensionalen, globalen numerischen Modell bei Anwesenheit einer subtropischen kritischen Schicht. D. Reimer, 1988.

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15

Kamenkovich, Igor V. Radiating instability of nonzonal ocean currents. Massachusetts Institute of Technology, Woods Hole Oceanographic Institution, Joint Program in Oceanography/Applied Ocean Science and Engineering, 1997.

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16

Phillips, Norman A. Dispersion processes in large scale weather prediction. World Meteorological Organization, 1990.

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17

Phillips, Norman A. Dispersion processes in large-scale weather prediction. Secretariat of the World Meteorological Organization, 1990.

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18

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 classi
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19

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 Chap
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20

Zeitlin, Vladimir. Wave Motions in Rotating Shallow Water with Boundaries, Topography, at the Equator, and in Laboratory. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0004.

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The chapter illustrates the influence of lateral boundaries, bottom topography, outcroppings, equatorial tangent plane approximation, and cylindrical channel geometry in laboratory experiments on the wave spectrum, and characteristics of waves in rotating shallow-water model. It is shown that all these effects lead to appearance of wave-guide modes, localised in one spatial direction, and freely propagating in another one. These modes are coastal and equatorial Kelvin waves, topographic and equatorial Rossby waves, shelf and edge waves, equatorial Yanai and inertia–gravity waves, and frontal w
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21

United States. National Aeronautics and Space Administration., ed. Investigation of tropical transport with UARS data: Final report : contract no. NAS5-32862. Northwest Research Associates, 1999.

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22

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
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23

Atmospheric Tidal and Planetary Waves. Springer, 2011.

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24

Volland, Hans. Atmospheric Tidal and Planetary Waves. Springer, 2011.

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25

R, Ziemke J., and United States. National Aeronautics and Space Administration., eds. Rossby-gravity waves in tropical total ozone data. National Aeronautics and Space Administration, 1993.

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26

United States. National Aeronautics and Space Administration., ed. Waves and instability in the atmosphere of Mars: Final report, July 1, 1987 - December 31, 1990. National Aeronautics and Space Administration, 1990.

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27

Hollingsworth, Jeffery L. Modeling of forced planetary waves in the Mars atmosphere. 1992.

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28

United States. National Aeronautics and Space Administration., ed. Waves and instability in the atmosphere of Mars: Final report, July 1, 1987 - December 31, 1990. National Aeronautics and Space Administration, 1990.

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29

R, Stanford J., and United States. National Aeronautics and Space Administration., eds. Kelvin waves in tropical total ozone data. National Aeronautics and Space Administration, 1993.

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30

United States. National Aeronautics and Space Administration., ed. Large-scale dynamics and transport in the stratosphere. National Aeronautics and Space Administration, 1990.

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31

United States. National Aeronautics and Space Administration., ed. Large-scale dynamics and transport in the stratosphere. National Aeronautics and Space Administration, 1990.

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32

R, Reiter Elmar, and United States. National Aeronautics and Space Administration., eds. Atmospheric planetary wave response to external forcing: Final technical report, NASA grant NAG 5-136. National Aeronautics and Space Administration, 1985.

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33

Pacific Marine Environmental Laboratory (U.S.), ed. Observations of long Rossby waves in the northern tropical Pacific. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, Pacific Marine Environmental Laboratory, 1989.

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34

National Research Council and the Office of Naval Research. Aspects of Weather and Space Weather in the Earth's Upper Atmosphere: The Role of Internal Atmospheric Waves (International Science Lecture Series, 6th Lecture). National Academies Press, 1997.

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35

1940-, Gruber Arnold, and United States. National Environmental Satellite, Data, and Information Service, eds. Spurious semi-diurnal variation in the E.R.B.E. outgoing longwave radiation. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1995.

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36

1940-, Gruber Arnold, and United States. National Environmental Satellite, Data, and Information Service., eds. Spurious semi-diurnal variation in the E.R.B.E. outgoing longwave radiation. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1995.

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37

1940-, Gruber Arnold, and United States. National Environmental Satellite, Data, and Information Service, eds. Spurious semi-diurnal variation in the E.R.B.E. outgoing longwave radiation. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1995.

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38

Twining, David S. The relationship of precipitation in the western United States to variations in the outgoing long-wave radiation field over the tropical Pacific: The role of the mid-latitude circulation. 1995.

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39

1940-, Gruber Arnold, and United States. National Environmental Satellite, Data, and Information Service., eds. Spurious semi-diurnal variation in the E.R.B.E. outgoing longwave radiation. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1995.

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40

1940-, Gruber Arnold, and United States. National Environmental Satellite, Data, and Information Service., eds. Spurious semi-diurnal variation in the E.R.B.E. outgoing longwave radiation. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Environmental Satellite, Data, and Information Service, 1995.

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41

I, Ivanovskiĭ A., and Gosudarstvennyĭ komitet SSSR po gidrometeorologii i kontroli͡u︡ prirodnoĭ sredy., eds. Fizika verkhneĭ atmosfery. Moskovskoe otd-nie Gidrometeoizdata, 1985.

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42

Influence of El Nino on the biennial and annual Rossby waves propagation in the Indian Ocean with special emphasis on Indian Ocean dipole. Indian Institute of Tropical Meteorology, 2006.

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43

A Mathematical Theory of Large-scale Atmosphere/ocean Flow. Imperial College Press, 2006.

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44

Homayoun, Karimabadi, Krauss-Varban Dietmar, and United States. National Aeronautics and Space Administration., eds. Physics of boundaries and their interactions in space plasmas: Final contractor report #19, 5/01/98-5/31/98. SciberNet, Inc., 1998.

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45

Homayoun, Karimabadi, Krauss-Varban Dietmar, and United States. National Aeronautics and Space Administration., eds. Physics of boundaries and their interactions in space plasmas: Interim contractor report #32 (final), 6/01/99-6/30/99. SciberNet, Inc., 1999.

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46

Homayoun, Karimabadi, Krauss-Varban Dietmar, and United States. National Aeronautics and Space Administration., eds. Physics of boundaries and their interactions in space plasmas: Interim contractor report #32 (final), 6/01/99-6/30/99. SciberNet, Inc., 1999.

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47

Homayoun, Karimabadi, Krauss-Varban Dietmar, and United States. National Aeronautics and Space Administration., eds. Physics of boundaries and their interactions in space plasmas: Final contractor report #19, 5/01/98-5/31/98. SciberNet, Inc., 1998.

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48

Zeitlin, Vladimir. Wave Turbulence. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0013.

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Main notions and ideas of wave (weak) turbulence theory are explained with the help of Hamiltonian approach to wave dynamics, and are applied to waves in RSW model. Derivation of kinetic equations under random-phase approximation is explained. Short inertia–gravity waves on the f plane, short equatorial inertia–gravity waves, and Rossby waves on the beta plane are then considered along these lines. In all of these cases, approximate solutions of kinetic equation, annihilating the collision integral, can be obtained by scaling arguments, giving power-law energy spectra. The predictions of turbu
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49

Zeitlin, Vladimir. Resonant Wave Interactions and Resonant Excitation of Wave-guide Modes. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0012.

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The idea of resonant nonlinear interactions of waves, and of resonant wave triads, is first explained using the example of Rossby waves, and then used to highlight a mechanism of excitation of wave-guide modes, by impinging free waves at the oceanic shelf, and at the equator. Physics and mathematics of the mechanism, which is related to the phenomena of parametric resonance and wave modulation, are explained in detail in both cases. The resulting modulation equations, of Ginzburg–Landau or nonlinear Schrodinger type, are obtained by multi-scale asymptotic expansions and elimination of resonanc
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50

Tibaldi, Stefano, and Franco Molteni. Atmospheric Blocking in Observation and Models. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.611.

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The atmospheric circulation in the mid-latitudes of both hemispheres is usually dominated by westerly winds and by planetary-scale and shorter-scale synoptic waves, moving mostly from west to east. A remarkable and frequent exception to this “usual” behavior is atmospheric blocking. Blocking occurs when the usual zonal flow is hindered by the establishment of a large-amplitude, quasi-stationary, high-pressure meridional circulation structure which “blocks” the flow of the westerlies and the progression of the atmospheric waves and disturbances embedded in them. Such blocking structures can hav
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