Добірка наукової літератури з теми "Rossby waves"

Оформте джерело за APA, MLA, Chicago, Harvard та іншими стилями

Оберіть тип джерела:

Ознайомтеся зі списками актуальних статей, книг, дисертацій, тез та інших наукових джерел на тему "Rossby waves".

Біля кожної праці в переліку літератури доступна кнопка «Додати до бібліографії». Скористайтеся нею – і ми автоматично оформимо бібліографічне посилання на обрану працю в потрібному вам стилі цитування: APA, MLA, «Гарвард», «Чикаго», «Ванкувер» тощо.

Також ви можете завантажити повний текст наукової публікації у форматі «.pdf» та прочитати онлайн анотацію до роботи, якщо відповідні параметри наявні в метаданих.

За допомогою хмари тегів ви можете побачити ще більше пов’язаних тем досліджень, а відповідні кнопки після кожного розділу сторінки дозволяють переглянути розширені списки книг, статей тощо на обрану тему.

Пов'язані теми наукових робіт:

Статті в журналах з теми "Rossby waves":

1
Knessl, Charles, and Joseph B. Keller. "Rossby Waves." Studies in Applied Mathematics 94, no. 4 (May 1995): 359–76. http://dx.doi.org/10.1002/sapm1995944359.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2
Cheverry, Christophe, Isabelle Gallagher, Thierry Paul, and Laure Saint-Raymond. "Trapping Rossby waves." Comptes Rendus Mathematique 347, no. 15-16 (August 2009): 879–84. http://dx.doi.org/10.1016/j.crma.2009.05.007.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3
Müller, Detlev. "Trapped Rossby waves." Physical Review E 61, no. 2 (February 2000): 1468–85. http://dx.doi.org/10.1103/physreve.61.1468.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
4
Avalos-Zuniga, R., F. Plunian та K. H. Rädler. "Rossby waves andα-effect". Geophysical & Astrophysical Fluid Dynamics 103, № 5 (жовтень 2009): 375–96. http://dx.doi.org/10.1080/03091920903006099.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
5
Miles, John. "Resonantly Forced Rossby Waves." Journal of Physical Oceanography 15, no. 4 (April 1985): 467–74. http://dx.doi.org/10.1175/1520-0485(1985)015<0467:rfrw>2.0.co;2.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
6
Dukowicz, John K. "Mesh Effects for Rossby Waves." Journal of Computational Physics 119, no. 1 (June 1995): 188–94. http://dx.doi.org/10.1006/jcph.1995.1126.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
7
Persson, Anders. "Rossby waves - do they exist?" Weather 70, no. 12 (December 2015): 344–45. http://dx.doi.org/10.1002/wea.2588.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
8
Bénard, P. "Stability of Rossby–Haurwitz waves." Quarterly Journal of the Royal Meteorological Society 146, no. 727 (December 2019): 613–28. http://dx.doi.org/10.1002/qj.3696.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
9
Kloosterziel, R. C., and L. R. M. Maas. "Green’s functions for Rossby waves." Journal of Fluid Mechanics 830 (October 2017): 387–407. http://dx.doi.org/10.1017/jfm.2017.601.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
Compact solutions are presented for planetary, non-divergent, barotropic Rossby waves generated by (i) an impulsive point source and (ii) a sustained point source of curl of wind stress. Previously, only cumbersome integral expressions were known, rendering them practically useless. Our simple expressions allow for immediate numerical visualization/animation and further mathematical analysis.
10
EGGER, JOSEPH, and KLAUS FRAEDRICH. "Topographic Rossby waves over Antarctica." Tellus A 39A, no. 2 (March 1987): 110–15. http://dx.doi.org/10.1111/j.1600-0870.1987.tb00293.x.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.

Дисертації з теми "Rossby waves":

1
Cotto, Amaryllis. "Intermittently Forced Vortex Rossby Waves." Text, FIU Digital Commons, 2002. http://digitalcommons.fiu.edu/etd/553.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
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 approaches zero. This process may initiate outer wind maxima by weakening the mean–flow just inward from the critical radius. The waves are confined to a relatively narrow annular waveguide because of their slow tangential phase velocity and the narrow interval between the Rossby wave cut–off frequency, where the radial wavenumber is locally zero, and the zero frequency, where it is locally infinite.
2
Wood, R. G. "Rossby waves in mid-latitude oceans." Electronic Thesis or Dissertation, University of Essex, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.379474.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3
Murphy, Darryl Guy. "Rossby waves in the Southern Ocean." Electronic Thesis or Dissertation, University of Exeter, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.303178.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
4
Giannitsis, Constantine 1971. "Non-linear saturation of vertically propagating Rossby waves." Thesis, Massachusetts Institute of Technology, 2001. http://hdl.handle.net/1721.1/53043.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
Thesis (Ph.D.)--Massachusetts Institute of Technology, Dept. of Earth, Atmospheric, and Planetary Sciences, February 2001.
Includes bibliographical references (p. 203-208).
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 thus expected above a certain critical wave amplitude, raising the question of how the non-linear flow reacts to limit the vertical penetration of waves. Keeping in mind the potential importance for the dynamics of the winter stratosphere, where strong wave penetration and amplitude growth are often observed, the issue of wave saturation in a non-linear flow is examined in a generally abstract context, through a variety of simple model studies. We thus consider the cases of a topographically forced barotropic beta plane channel model, of vertical propagation through a three-dimensional beta plane channel model, and of a polar coordinate model with realistic basic state and geometry. In the barotropic model transient wave growth is forced through the use of bottom topography and the deviations of the non-linear flow evolution from the predictions of both a linear and a quasi-linear analytical solution are examined for strong topographic anomalies. The growth of the forced wave is found to decelerate the zonal mean flow which in turn reduces the topographic forcing. Wave-mean flow interactions are thus found to be sufficient in leading to saturation of the eddy amplitudes. Interestingly it is the formation of zonal mean easterlies, rather than the depletion of mean available potential enstrophy, that is found to be the crucial factor in the saturation dynamics. Similar results are obtained for the case of vertical propagation through a three dimensional beta plane channel. The vertical penetration of the forced wave is shown to cause a reduction of the zonal mean winds and mean potential vorticity gradients in the center of the channel, eventually leading to the formation of either a critical line or a refractive index turning surface. In both cases the penetration of the wave to high altitudes is prohibited, thus constraining wave amplitudes. While signs of non-linear behaviour are clear in synoptic maps of potential vorticity, wave-wave interactions are found to play a secondary role in the saturation process. The results of the three-dimensional beta plane channel model are then extended to a more realistic set-up, using a polar coordinate model with a basic state based on the observed winter stratosphere climatology. The basic conclusions of the idealized study are shown to remain unchanged.
by Constantine Giannitsis.
Ph.D.
5
Ash, Ellis R. "Rossby waves and mean currents in the Southern Ocean." Electronic Thesis or Dissertation, University of Edinburgh, 2000. http://hdl.handle.net/1842/11542.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
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 relation, but it is shown that Rossby waves cannot be used to measure mean flows in the ACC without a further understanding of the theory involved. A property of the time-average eddy activity, known as the eddy orientation angle, is shown to indicate the axes of the prominent eastward jets in the mean flow. This shows that eddies are acting to force these jets. Five yeas of measurements from the TOPEX/POSEIDON satellite mission are used to identify Rossby waves in the real ocean. Coherent Rossby wave propagation is again confined to localised regions, some of which act as waveguides. Phase speeds are measured in these regions, and shown to be consistent with previous measurements of Rossby waves. An improved resolution dataset, combining TOPEX/POSEIDON and ERS altimetry measurements, is used to analyse the time-average eddy activity and associated forcing on the mean flow in unprecedented detail. Current data from cruises of the World Ocean Circulation Experiment are used in conjunction with altimetry data to estimate the mean flow at locations along ship tracks. Using these estimates, and the position of temperature fronts as an indication of prominent jets in the mean flow, the eddy forcing is shown to be different to that observed in FRAM. Instead of forcing the mean flow, eddies are being generated within the jets which are likely to be maintained by topographic forcing.
6
Jonsson, Eskil. "Modelling the Formation and Propagation of Orographic Rossby Waves." Student thesis, Uppsala universitet, Luft-, vatten och landskapslära, 2017. http://urn.kb.se/resolve?urn=urn:nbn:se:uu:diva-325188.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
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 techniques for solving these equations arepresented throughout ch. 2.4 and then implemented for the global-scale Shallow WaterEquations with conserved potential vorticity in ch. 3. The model is validated to work for typicalshallow water flows in a bath tub and passes common tests like the Gaussian curve test (ch.4.1). However, when considering atmospheric flows (ch. 4.2) it becomes evident that ourmodel, as well as our numerical methods are lacking and cannot reproduce Rossby waves ina stable manner. Hence, a heavily modified version of Hogan’s model (Hogan, n.d) isemployed with a simplified numerical scheme. With these corrections, orographic Rossbywaves appear to naturally form at appropriate locations. However, they do not fully exhibit theexpected behaviours discussed in ch. 2.2. Even Hogan’s model appears to have severelimitations as waves propagate in the wrong direction. Hence, this study is not complete andwarrants further development in order to be useful.
Orografiska Rossby-vågor är den huvudsakliga mekanismen genom vilken jetströmmarnaslingrar runt jorden och kan ha en omfattande inverkan på väder och klimat (kapitel 1). Därförär de av särskild betydelse att studera och detta projekt bör fungera som en utgångspunkt förvad man måste överväga när man försöker modellera dessa vågor. Till exempel så måste vi tahänsyn till tryckgradienter, Coriolis-effekten, orografi, potentiell vorticitetsbevarande och ävenjordens krökning på denna skala. Dessa beskrivs i detalj i kap. 2 och anpassas tillrörelseekvationerna för grunt vatten (Saint-Venant-ekvationerna). Därefter presenteras någranumeriska tekniker på grundläggande nivå för att lösa dessa ekvationer i kap. 2.4, varvid desedan implementeras för de globala Saint-Venant-ekvationerna med bevarad potentiellvorticitet i kap 3. Modellen är validerad för typiska grunda vattenflöden i ett badkar ochpasserar vanliga numeriska tester så som Gauss-kurvtestet (kap. 4.1) och bore-testet. Mennär vi överväger atmosfäriska flöden (kap. 4.2) blir det tydligt att våra modeller och numeriskametoder är primitiva och inte kan reproducera Rossby-vågor på ett stabilt sätt. Därmed,modifierar vi Hogans modell (Hogan, n.d) för att passa vår modell vilket resulterar orografiskaRossby-vågor. Dock så är dessa förskjutna och stämmer inte riktigt överens med teorin i kap.2.2. Även Hogans modell visar sig ha allvarliga begränsningar då vågorna propagerar i felriktning. Därmed är denna studie ej komplett och kräver ytterligare utveckling för att varaanvändbar.
7
Yang, Gui-Ying. "Propagation of nonstationary Rossby waves and extratropical-tropical interaction." Electronic Thesis or Dissertation, University of Reading, 1997. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.646005.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
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 and a dry primitive equation model with only idealised vorticity or thermal forcing, a possible trigger mechanism for the Madden Julian Oscillation (MJO) has been studied. The results show that eastward moving forcing in the subtropics or extratropics can lead to a significant equatorial Kelvin wave response which tends to be a maximum in the African/Indian Ocean sector, and is enhanced by easterly winds in the upper troposphere. It is suggested . that one mechanism for initiating the MJO is for eastward moving extratropical waves to excite a large equatorial response, sufficient to trigger large-scale convection, in the presence of favourable easterly winds in the upper troposphere. The dry primitive equation model is used to study the possible interaction of atmospheric flow in the two hemispheres and the triggering of other equatorial waves. It is found that stationary and westward moving forcing in the Northern Hemisphere extratropics can give a significant Southern Hemisphere response. A westward moving forcing in the subtropics, with a period of several days, can trigger the equatorial mixed Rossby-gravity and n=l Rossby waves. The zonal basic flow is found to have a significant effect on these equatorial wave responses.
8
Fyfe, John. "A barotropic stability study of free and forced planetary waves /." Electronic Thesis or Dissertation, McGill University, 1987. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=75433.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
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.
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 $(L sb{x}$ $>$ $L sb{y})$ exist under superresonant conditions. We also report on the existence of an interesting travelling topographic instability.
The linear instability of a weakly non-zonal flow is investigated numerically and analytically (via WKB theory). The theory reproduces the qualitative nature of the numerically-determined fastest-growing mode.
Nonlinear integrations, involving many degrees of freedom, reveal that initially-infinitesimal disturbances may grow explosively to finite-amplitude. The longer-term integrations are interpreted using a statistical mechanical model.
9
Choboter, Paul F. "Forced Rossby waves in a zero absolute vorticity gradient environment." Electronic Thesis or Dissertation, McGill University, 1997. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=27509.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
Observations show the presence of localized regions in the atmosphere with diminished potential vorticity gradients, like in the tropical upper troposphere where outflow from deep convective regions plays an important role. The present work investigates the effect of forcing on the evolution of Rossby waves in a zero potential vorticity gradient environment. As a preliminary investigation, the barotropic case is studied, where the analogue of potential vorticity is absolute vorticity.
The analytic solution of the linearized problem shows that the streamfunction grows algebraically in time, and eventually develops a nonlinear critical layer. The numerical solution of the nonlinear problem within the critical layer shows that the nonlinearity and the forcing act together to halt the growth as coherent vortices are put in a nonlinear oscillatory regime. At long times, the critical layer solution settles to a quasi-steady state consisting of relatively large amplitude stationary vortices, with a set of small amplitude steadily-propagating vortices superimposed. These results are contrasted with the results of previous unforced problems.
10
Choboter, Paul F. "Forced Rossby waves in a zero absolute vorticity gradient environment." Electronic thesis or dissertation, National Library of Canada = Bibliothèque nationale du Canada, 1997. http://www.collectionscanada.ca/obj/s4/f2/dsk2/ftp03/MQ37107.pdf.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.

Книги з теми "Rossby waves":

1
Volland, Hans. Atmospheric tidal and planetary waves. Dordrecht: Kluwer Academic Publishers, 1988.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2
Stanford, John. Rossby-gravity waves in tropical total ozone data. [Washington, DC: National Aeronautics and Space Administration, 1993.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3
Stanford, John. Rossby-gravity waves in tropical total ozone data. [Washington, DC: National Aeronautics and Space Administration, 1993.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
4
Chiu, Ching-Sang. Estimation of planetary wave parameters from the data of the 1981 Ocean Acoustic Tomography Experiment. Woods Hole, Mass: Woods Hole Oceanographic Institution, 1985.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
5
Kessler, William S. Observations of long Rossby waves in the northern tropical Pacific. Seattle, Wash: U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, Environmental Research Laboratories, 1989.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
6
Kelley, Michael C. Aspects of weather and space weather in the earth's upper atmosphere: The role of internal atmospheric waves. Washington, D.C: National Academy Press, 1997.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
7
Haack, Tracy. Mixed convective/dynamic roll vortices and their effects on initial wind and temperature profiles. University Park, PA: Dept. of Meteorology, Pennsylvania State University, 1991.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
8
Grigorkina, R. G. Vozdeĭstvie taĭfunov na okean. Leningrad: Gidrometeoizdat, 1986.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
9
Grigorkina, R. G. Vozdeĭstvie taĭfunov na okean. Leningrad: Gidrometeoizdat, 1986.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
10
Swart, H. E. de. Vacillation and predictability properties of low-order atmospheric spectral models. Amsterdam, the Netherlands: Centrum voor Wiskunde en Informatica, 1989.
Знайти повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.

Частини книг з теми "Rossby waves":

1
Monin, A. S. "Rossby Waves." In Theoretical Geophysical Fluid Dynamics, 237–75. Dordrecht: Springer Netherlands, 1990. http://dx.doi.org/10.1007/978-94-009-1880-1_7.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2
Zeytounian, Radyadour. "Rossby Waves." In Asymptotic Modeling of Atmospheric Flows, 44–62. Berlin, Heidelberg: Springer Berlin Heidelberg, 1990. http://dx.doi.org/10.1007/978-3-642-73800-5_4.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3
Pedlosky, Joseph. "Rossby Waves." In Waves in the Ocean and Atmosphere, 149–58. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05131-3_14.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
4
Kamenkovich, V. M., M. N. Koshlyakov, and A. S. Monin. "Theory of Rossby Waves." In Synoptic Eddies in the Ocean, 34–130. Dordrecht: Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-009-4502-9_2.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
5
Pedlosky, Joseph. "Rossby Waves (Continued), Quasi-Geostrophy." In Waves in the Ocean and Atmosphere, 159–71. Berlin, Heidelberg: Springer Berlin Heidelberg, 2003. http://dx.doi.org/10.1007/978-3-662-05131-3_15.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
6
Boyd, John P. "Kelvin, Yanai, Rossby and Gravity Waves." In Dynamics of the Equatorial Ocean, 35–67. Berlin, Heidelberg: Springer Berlin Heidelberg, 2017. http://dx.doi.org/10.1007/978-3-662-55476-0_3.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
7
Skiba, Yuri N. "Stability of Rossby-Haurwitz (RH) Waves." In Mathematical Problems of the Dynamics of Incompressible Fluid on a Rotating Sphere, 109–33. Cham: Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-65412-6_5.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
8
Dolzhansky, Felix V. "The Obukhov–Charney Equation; Rossby Waves." In Fundamentals of Geophysical Hydrodynamics, 61–70. Berlin, Heidelberg: Springer Berlin Heidelberg, 2013. http://dx.doi.org/10.1007/978-3-642-31034-8_7.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
9
Sardeshmukh, Prashant, Cécile Penland, and Matthew Newman. "Rossby waves in a stochastically fluctuating medium." In Stochastic Climate Models, 369–84. Basel: Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8287-3_17.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
10
Hirooka, Toshihiko, and Isamu Hirota. "Further Evidence of Normal Mode Rossby Waves." In Middle Atmosphere, 277–89. Basel: Birkhäuser Basel, 1989. http://dx.doi.org/10.1007/978-3-0348-5825-0_10.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.

Тези доповідей конференцій з теми "Rossby waves":

1
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.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2
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.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3
Campbell, L. J. "Nonlinear dynamics of Rossby waves in a western boundary current." In ADVANCES IN FLUID MECHANICS 2006. Southampton, UK: WIT Press, 2006. http://dx.doi.org/10.2495/afm06045.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
4
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.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
5
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.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
6
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.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
7
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.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
Анотація:
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 vortex were measured by means of two pressure transducers fixed at a distance of 2 mm to the opposite walls of the diffuser downstream of its inlet. The analysis of the experimental result of Tsurusaki, Imaichi and Miyake (1987) about the fields of the total and fluctuating velocities of rotating stall in the vaneless diffuser reveals furthermore that the longitudinal spiral vortex is centred on the through flow. The two vortices of the pair stay side by side in touch but without mixing because of their opposite rotational sense. The longitudinal vortices make about 1 1/4 turns from the inlet to the outlet of the diffuser under the guidance of the Rossby waves. The vorticity of the longitudinal vortex is determined from the experimental result. Furthermore, the experimental result reveals that the fronts along the high pressure ridges and the low pressure troughs of the Rossby wave pattern are themselves longitudinal vortices. Then these fronts possess a behaviour of the jet stream, which is associated with the Rossby waves of the atmosphere in the midlatitude. Finally, the origin of the vorticity of the longitudinal vortices along the through flow and the Rossby-wave front is derived based on the experimental results obtained by Hergt and Jaberg (1988), and Hide (1958).
8
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.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
9
Meheut, Heloise, Fabien Casse, Peggy Varniere, and Michel Tagger. "3D numerical simulations of the Rossby wave instability." In VII Microquasar Workshop: Microquasars and Beyond. Trieste, Italy: Sissa Medialab, 2009. http://dx.doi.org/10.22323/1.062.0097.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
10
Da, Chaojiu, and Jian Song. "The numerical simulation of the evolution of the amplitude of nonlinear solitary Rossby waves in a sort of time-dependent zonal flow." In 2012 8th International Conference on Natural Computation (ICNC). IEEE, 2012. http://dx.doi.org/10.1109/icnc.2012.6234578.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.

Звіти організацій з теми "Rossby waves":

1
Peng, Melinda S. Role of Vortex Rossby Waves on Tropical Cyclone Intensity. Fort Belvoir, VA: Defense Technical Information Center, September 2007. http://dx.doi.org/10.21236/ada541436.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
2
Peng, Melinda S. Role of Vortex Rossby Waves on Tropical Cyclone Intensity. Fort Belvoir, VA: Defense Technical Information Center, September 2008. http://dx.doi.org/10.21236/ada532809.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
3
Peng, Melinda S. Role of Vortex Rossby Waves on Tropical Cyclone Intensity. Fort Belvoir, VA: Defense Technical Information Center, September 2006. http://dx.doi.org/10.21236/ada631046.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
4
Montgomery, Michael T., and Lloyd J. Shapiro. Vortex Rossby Waves and Hurricane Evolution in the Presence of Convection and Potential Vorticity and Hurricane Motion. Fort Belvoir, VA: Defense Technical Information Center, September 1997. http://dx.doi.org/10.21236/ada628370.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
5
Miller, Jonah Maxwell. Gravitational Waves. Office of Scientific and Technical Information (OSTI), October 2017. http://dx.doi.org/10.2172/1402567.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
6
Del Pizzo, Rebecca, and Vincent Quevedo. Ocean Waves. Ames: Iowa State University, Digital Repository, November 2015. http://dx.doi.org/10.31274/itaa_proceedings-180814-1278.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
7
Johnston, T. M. Island-Trapped Waves, Internal Waves, and Island Circulation. Fort Belvoir, VA: Defense Technical Information Center, September 2014. http://dx.doi.org/10.21236/ada624487.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
8
Ablowitz, Mark J., James H. Curry, Joe L. Hammack, and Harvey Segur. Nonlinear Ocean Waves. Fort Belvoir, VA: Defense Technical Information Center, September 1994. http://dx.doi.org/10.21236/ada285331.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
9
Cliver, Edward W. Making Waves (Postprint). Fort Belvoir, VA: Defense Technical Information Center, October 2013. http://dx.doi.org/10.21236/ada599244.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.
10
He, Zhiguo, and Péter Kondor. Inefficient Investment Waves. Cambridge, MA: National Bureau of Economic Research, July 2012. http://dx.doi.org/10.3386/w18217.
Повний текст джерела
Стилі APA, Harvard, Vancouver, ISO та ін.

До бібліографії

Будь ласка, вимкніть ваш блокувальник реклами

Adblock logo Adblock logo Adblock logo

"Grafiati" – це незалежний сервіс, що забезпечує унікальну якість оформлення бібліографічних посилань. Ви можете користуватися нашим сайтом безоплатно, дозволивши показ реклами, або оформити передплату.

Передплатити