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Artykuły w czasopismach na temat "Rossby waves"

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Knessl, Charles, and Joseph B. Keller. "Rossby Waves." Studies in Applied Mathematics 94, no. 4 (1995): 359–76. http://dx.doi.org/10.1002/sapm1995944359.

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Müller, Detlev. "Trapped Rossby waves." Physical Review E 61, no. 2 (2000): 1468–85. http://dx.doi.org/10.1103/physreve.61.1468.

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Cheverry, Christophe, Isabelle Gallagher, Thierry Paul, and Laure Saint-Raymond. "Trapping Rossby waves." Comptes Rendus Mathematique 347, no. 15-16 (2009): 879–84. http://dx.doi.org/10.1016/j.crma.2009.05.007.

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Fedotova, Maria, Dmitry Klimachkov, and Arakel Petrosyan. "Resonant interactions of magneto-Poincaré and magneto-Rossby waves in quasi-two-dimensional rotating astrophysical plasma." Monthly Notices of the Royal Astronomical Society 509, no. 1 (2021): 314–26. http://dx.doi.org/10.1093/mnras/stab2957.

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ABSTRACT Increased interest in research of non-linear resonant interactions of waves in rotating astrophysical plasma has taken place in recent years. This is due to the discovering solar magneto-Rossby waves and the emergence of new data on the effect of three-wave interactions of magneto-Rossby waves on solar activity. In context of large-scale magnetohydrodynamic flows in presence of rotation, magneto-Poincaré waves and magneto-Rossby waves are highlighted. The β-plane approximation is developed to simplify the theory of spherical Rossby waves. Nevertheless, the representation of the Coriol
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Biancofiore, L., and F. Gallaire. "Counterpropagating Rossby waves in confined plane wakes." Physics of Fluids 24, no. 7 (2012): 074102. http://dx.doi.org/10.1063/1.4729617.

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Song, Jian, та ShaoXia Liu. "The barotropic Rossby waves with topography on the earth’s δ-surface". International Journal of Nonlinear Sciences and Numerical Simulation 21, № 7-8 (2020): 781–88. http://dx.doi.org/10.1515/ijnsns-2019-0178.

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AbstractThe Rossby solitary waves in the barotropic vorticity model which contains the topography on the earth’s δ-surface is investigated. First, applying scale analysis method, obtained the generalized quasi-geostrophic potential vorticity equation (QGPVE). Using The Wentzel–Kramers–Brillouin (WKB) theory, the evolution equation of Rossby waves is the variable-coefficient Korteweg–de Vries (KdV) equation for the barotropic atmospheric model. In order to study the Rossby waves structural change to exist in some basic flow and topography on the δ-surface approximation, the variable coefficient
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Dikpati, Mausumi, Peter A. Gilman, Gustavo A. Guerrero, et al. "Simulating Solar Near-surface Rossby Waves by Inverse Cascade from Supergranule Energy." Astrophysical Journal 931, no. 2 (2022): 117. http://dx.doi.org/10.3847/1538-4357/ac674b.

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Abstract Rossby waves are found at several levels in the Sun, most recently in its supergranule layer. We show that Rossby waves in the supergranule layer can be excited by an inverse cascade of kinetic energy from the nearly horizontal motions in supergranules. We illustrate how this excitation occurs using a hydrodynamic shallow-water model for a 3D thin rotating spherical shell. We find that initial kinetic energy at small spatial scales inverse cascades quickly to global scales, exciting Rossby waves whose phase velocities are similar to linear Rossby waves on the sphere originally derived
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Avalos-Zuniga, R., F. Plunian та K. H. Rädler. "Rossby waves andα-effect". Geophysical & Astrophysical Fluid Dynamics 103, № 5 (2009): 375–96. http://dx.doi.org/10.1080/03091920903006099.

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Miles, John. "Resonantly Forced Rossby Waves." Journal of Physical Oceanography 15, no. 4 (1985): 467–74. http://dx.doi.org/10.1175/1520-0485(1985)015<0467:rfrw>2.0.co;2.

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KALADZE, T. D., D. J. WU, O. A. POKHOTELOV, R. Z. SAGDEEV, L. STENFLO, and P. K. SHUKLA. "Rossby-wave driven zonal flows in the ionospheric E-layer." Journal of Plasma Physics 73, no. 1 (2007): 131–40. http://dx.doi.org/10.1017/s0022377806004351.

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Abstract.A novel mechanism for the generation of large-scale zonal flows by small-scale Rossby waves in the Earth's ionospheric E-layer is considered. The generation mechanism is based on the parametric excitation of convective cells by finite amplitude magnetized Rossby waves. To describe this process a generalized Charney equation containing both vector and scalar (Korteweg–de Vries type) nonlinearities is used. The magnetized Rossby waves are supposed to have arbitrary wavelengths (as compared with the Rossby radius). A set of coupled equations describing the nonlinear interaction of magnet
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Rozprawy doktorskie na temat "Rossby waves"

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Cotto, Amaryllis. "Intermittently Forced Vortex Rossby Waves." FIU Digital Commons, 2012. http://digitalcommons.fiu.edu/etd/553.

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Wavelike spiral asymmetries are an intriguing aspect of Tropical Cyclone dynamics. Previous work hypothesized that some of them are Vortex Rossby Waves propagating on the radial gradient of mean–flow relative vorticity. In the Intermittently Forced Vortex Rossby Wave theory, intermittent convection near the eyewall wind maximum excites them so that they propagate wave energy outward and converge angular momentum inward. The waves’ energy is absorbed as the perturbation vorticity becomes filamented near the outer critical radii where their Doppler–shifted frequencies and radial group velocities
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Proehl, Jeffrey A. "Equatorial wave-mean flow interaction : the long Rossby waves /." Thesis, Connect to this title online; UW restricted, 1988. http://hdl.handle.net/1773/10960.

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Murphy, Darryl Guy. "Rossby waves in the Southern Ocean." Thesis, University of Exeter, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303178.

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Wood, R. G. "Rossby waves in mid-latitude oceans." Thesis, University of Essex, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.379474.

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Kovalam, Sujata. "MF radar observations of tides and planetary waves." Title page, contents and abstract only, 2000. http://web4.library.adelaide.edu.au/theses/09PH/09phk878.pdf.

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Copies of previously published articles inserted. Bibliography: p. 185-200. Data obtained from six radar stations covering a wide latitude range has been used to determine the global distribution of planetary waves and tides. In the process a number of data analyses techniques were considered for their characterisation.
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Fyfe, John. "A barotropic stability study of free and forced planetary waves /." Thesis, McGill University, 1987. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=75433.

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The stability of free and forced planetary waves in a $ beta$-channel is investigated with a barotropic model. The forced waves at equilibrium result from a constant mean-zonal wind interacting with a finite-amplitude topography.<br>The frequencies of all infinitesimal perturbations to the equilibrium flows are determined numerically as a function of the flow parameters. The results are interpreted using a truncated spectral model and related to those of previous studies with infinite $ beta$-planes. In contrast to some earlier analytical studies we find that unstable long waves $(L sb{x}$ $>$
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Giannitsis, Constantine 1971. "Non-linear saturation of vertically propagating Rossby waves." Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/53043.

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Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, February 2001.<br>Includes bibliographical references (p. 203-208).<br>Linear quasi-geostrophic theory predicts an exponential amplitude increase with height for Rossby waves propagating vertically through a stratified atmosphere, as a result of wave activity density conservation. At the same time layer-wise conservation of potential enstrophy constrains wave amplitudes, given the limited amount of potential enstrophy available in the initial mean flow. A break down of linear theory is t
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Ash, Ellis R. "Rossby waves and mean currents in the Southern Ocean." Thesis, University of Edinburgh, 2000. http://hdl.handle.net/1842/11542.

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Dynamics in the Southern Ocean are dominated by the Antarctic Circumpolar Current (ACC), and this large eastward current has an important influence on the earth's climate. Output from the last six years of the Fine Resolution Antarctic Model, where the mean flow is known, is used to develop techniques for quantifying Rossby waves and eddy activity. Some eastward jets in the mean flow are found to act as waveguides for Rossby waves. Phase speeds are found to increase linearly with frequency, but do not vary with the strength of mean flow. The reason for this is demonstrated using the dispersion
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Yang, Gui-Ying. "Propagation of nonstationary Rossby waves and extratropical-tropical interaction." Thesis, University of Reading, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.646005.

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The propagation of Rossby waves with positive and negative frequency, corresponding to eastward and westward phase speeds respectively, is investigated. The techniques used are theoretical analysis, ray tracing, and initial value problems in barotropic and baroclinic numerical models. It is found that the characteristics of positive and negative frequency Rossby waves can differ significantly from each other andfrom those of stationary, zero frequency Rossby waves. However, general deductions from studies of stationary Rossby waves are still found to be valid. Using an analytic Gill-type model
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Jonsson, Eskil. "Modelling the Formation and Propagation of Orographic Rossby Waves." Thesis, Uppsala universitet, Luft-, vatten och landskapslära, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-325188.

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Orographic Rossby waves are the main mechanism by which the jet streams meander aroundthe Earth and have possibly far-reaching impacts on weather and climate (chapter 1). Hence,they are of particular importance to study and this project should serve as a starting point inwhat to consider when trying to model these waves. For example, we have to account forpressure gradients, Coriolis effect, orography, potential vorticity conservation and also Earth’scurvature at this scale. These are covered in detail in ch. 2 and adapted to the Shallow WaterEquations. In addition, some entry-level numerical
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Książki na temat "Rossby waves"

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

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

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

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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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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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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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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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Części książek na temat "Rossby waves"

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Zeytounian, Radyadour. "Rossby Waves." In Asymptotic Modeling of Atmospheric Flows. Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-73800-5_4.

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Monin, A. S. "Rossby Waves." In Theoretical Geophysical Fluid Dynamics. Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-1880-1_7.

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Pedlosky, Joseph. "Rossby Waves." In Waves in the Ocean and Atmosphere. Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05131-3_14.

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Kamenkovich, V. M., M. N. Koshlyakov, and A. S. Monin. "Theory of Rossby Waves." In Synoptic Eddies in the Ocean. Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4502-9_2.

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Pierini, Stefano. "Quasigeostrophic Approximation, Rossby Waves." In UNITEXT for Physics. Springer Nature Switzerland, 2025. https://doi.org/10.1007/978-3-031-77991-6_19.

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Pedlosky, Joseph. "Rossby Waves (Continued), Quasi-Geostrophy." In Waves in the Ocean and Atmosphere. Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05131-3_15.

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Dolzhansky, Felix V. "The Obukhov–Charney Equation; Rossby Waves." In Fundamentals of Geophysical Hydrodynamics. Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31034-8_7.

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Skiba, Yuri N. "Stability of Rossby-Haurwitz (RH) Waves." In Mathematical Problems of the Dynamics of Incompressible Fluid on a Rotating Sphere. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-65412-6_5.

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Boyd, John P. "Kelvin, Yanai, Rossby and Gravity Waves." In Dynamics of the Equatorial Ocean. Springer Berlin Heidelberg, 2017. http://dx.doi.org/10.1007/978-3-662-55476-0_3.

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Pedlosky, Joseph. "Energy and Energy Flux in Rossby Waves." In Waves in the Ocean and Atmosphere. Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05131-3_16.

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Streszczenia konferencji na temat "Rossby waves"

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Zaqarashvili, T. V., and Ivan Zhelyazkov. "Rossby Waves in Rotating Magnetized Fluids." In SPACE PLASMA PHYSICS: School of Space Plasma Physics. AIP, 2009. http://dx.doi.org/10.1063/1.3137937.

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Sukoriansky, Semion, Nadejda Dikovskaya, Roger Grimshaw, and Boris Galperin. "Rossby waves and zonons in zonostrophic turbulence." In WAVES AND INSTABILITIES IN SPACE AND ASTROPHYSICAL PLASMAS. AIP, 2012. http://dx.doi.org/10.1063/1.3701355.

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Chen, Y. N., U. Haupt, U. Seidel, and M. Rautenberg. "Experimental Investigation of the Longitudinal-Vortex-Nature of Rotating Stall in Vaneless Diffusers of Centrifugal Compressors." In ASME 1991 International Gas Turbine and Aeroengine Congress and Exposition. American Society of Mechanical Engineers, 1991. http://dx.doi.org/10.1115/91-gt-099.

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Rotating stall in a vaneless diffuser of a centrifugal compressor has been found to be guided by Rossby waves, which are composed of branches of high and low pressures (Chen, Haupt and Rautenberg, 1990a). The branch of the high pressure leads the unstalled region and that of the low pressure leads the stalled region. The phase velocity of the Rossby waves is then the pattern speed of the stall cell. We report here an additional experimental result, according to which the flow of rotating stall is composed of a longitudinal spiral vortex pair. The vorticity and the axis of the longitudinal vort
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Shevkar, Prafulla P., Anoop M V, Philippe Odier, and Manikandan Mathur. "Video: Experimental visualization of Rossby waves as transport barriers." In 76th Annual Meeting of the APS Division of Fluid Dynamics. American Physical Society, 2023. http://dx.doi.org/10.1103/aps.dfd.2023.gfm.v0009.

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Campbell, L. J. "Nonlinear dynamics of Rossby waves in a western boundary current." In ADVANCES IN FLUID MECHANICS 2006. WIT Press, 2006. http://dx.doi.org/10.2495/afm06045.

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Chu, Peter C., and Chin-Lung Fang. "Observed Rossby waves in the South China Sea from satellite altimetry data." In Remote Sensing, edited by Charles R. Bostater, Jr. and Rosalia Santoleri. SPIE, 2004. http://dx.doi.org/10.1117/12.509064.

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del-Castillo-Negrete, D., J. M. Finn, and D. C. Barnes. "The modified drift-Poisson model: Analogies with geophysical flows and Rossby waves." In Non-neutral plasma physics III. AIP, 1999. http://dx.doi.org/10.1063/1.1302113.

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KALADZE, T. D., D. J. WU, O. A. POKHOTELOV, R. Z. SAGDEEV, L. STENFLO, and P. K. SHUKLA. "ZONAL FLOW GENERATION BY MAGNETIZED ROSSBY WAVES IN THE IONOPHERIC E-LAYER." In Proceedings of the 12th Regional Conference. WORLD SCIENTIFIC, 2007. http://dx.doi.org/10.1142/9789812770523_0026.

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Morey, Steve, Dmitry Dukhovskoy, and Cortis K. Cooper. "SS: Metocean: Measurements and Modeling Measurements of Topographic Rossby Waves along the Sigsbee Escarpment." In Offshore Technology Conference. Offshore Technology Conference, 2010. http://dx.doi.org/10.4043/20694-ms.

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Dai, Yuqiang, Fengxia Liu, Jintao Wu, Wei Wei, Dapeng Hu, and Xuewu Liu. "Influence of Skewing of Contact Face on Performance of Wave Rotor Refrigerators and Superchargers." In ASME 2013 International Mechanical Engineering Congress and Exposition. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/imece2013-63449.

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As a novel generation of rotational gas wave machines, wave rotor machines such as wave rotor refrigerators (WRR) and wave rotor superchargers (WRS) are unsteady flow devices. In their passages two gas streams (with different pressure or even different phases) comes into direct contact can exchange energy due to the movement of shock waves and expansion waves. A detailed study shows that, when rotor channels open to the high pressure port gradually, the contact face in rotor channels inevitably skews, which is always accompanied with reflection of shockwaves. This causes very large energy diss
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Raporty organizacyjne na temat "Rossby waves"

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Peng, Melinda S. Role of Vortex Rossby Waves on Tropical Cyclone Intensity. Defense Technical Information Center, 2008. http://dx.doi.org/10.21236/ada532809.

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Peng, Melinda S. Role of Vortex Rossby Waves on Tropical Cyclone Intensity. Defense Technical Information Center, 2007. http://dx.doi.org/10.21236/ada541436.

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Peng, Melinda S. Role of Vortex Rossby Waves on Tropical Cyclone Intensity. Defense Technical Information Center, 2006. http://dx.doi.org/10.21236/ada631046.

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Montgomery, Michael T., and Lloyd J. Shapiro. Vortex Rossby Waves and Hurricane Evolution in the Presence of Convection and Potential Vorticity and Hurricane Motion. Defense Technical Information Center, 1997. http://dx.doi.org/10.21236/ada628370.

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