Gotowe bibliografie tematyczne / Quasigeostrophic

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Gotowa bibliografia na temat „Quasigeostrophic”

Autor: Grafiati

Data publikacji: 4 czerwca 2021

Data aktualizacji: 19 lutego 2022

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Artykuły w czasopismach na temat "Quasigeostrophic"

Egger, Joseph. "Mountain torques in quasigeostrophic theory." Meteorologische Zeitschrift 12, no. 6 (December 1, 2003): 301–4. http://dx.doi.org/10.1127/0941-2948/2003/0012-0301.

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Miyazaki, Takeshi, Koki Ueno, and Tomoyuki Shimonishi. "Quasigeostrophic, Tilted Spheroidal Vortices." Journal of the Physical Society of Japan 68, no. 8 (August 15, 1999): 2592–601. http://dx.doi.org/10.1143/jpsj.68.2592.

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Miyazaki, Takeshi, Masahiro Shimada, and Naoya Takahashi. "Quasigeostrophic Wire-Vortex Model." Journal of the Physical Society of Japan 69, no. 10 (October 15, 2000): 3233–43. http://dx.doi.org/10.1143/jpsj.69.3233.

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Miyazaki, Takeshi, Takahiro Fujiwara, and Masahiro Yamamoto. "Quasigeostrophic Confocal Spheroidal Vortices." Journal of the Physical Society of Japan 72, no. 11 (November 15, 2003): 2786–803. http://dx.doi.org/10.1143/jpsj.72.2786.

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Miyazaki, Takeshi, Yu Furuichi, and Naoya Takahashi. "Quasigeostrophic Ellipsoidal Vortex Model." Journal of the Physical Society of Japan 70, no. 7 (July 15, 2001): 1942–53. http://dx.doi.org/10.1143/jpsj.70.1942.

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Duan, Jinqiao, and Beniamin Goldys. "Ergodicity of stochastically forced large scale geophysical flows." International Journal of Mathematics and Mathematical Sciences 28, no. 6 (2001): 313–20. http://dx.doi.org/10.1155/s0161171201012443.

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We investigate the ergodicity of 2D large scale quasigeostrophic flows under random wind forcing. We show that the quasigeostrophic flows are ergodic under suitable conditions on the random forcing and on the fluid domain, and under no restrictions on viscosity, Ekman constant or Coriolis parameter. When these conditions are satisfied, then for any observable of the quasigeostrophic flows, its time average approximates the statistical ensemble average, as long as the time interval is sufficiently long.

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Delsole, Timothy. "Stochastic Models of Quasigeostrophic Turbulence." Surveys in Geophysics 25, no. 2 (March 2004): 107–49. http://dx.doi.org/10.1023/b:geop.0000028164.58516.b2.

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Juckes, Martin. "Quasigeostrophic Dynamics of the Tropopause." Journal of the Atmospheric Sciences 51, no. 19 (October 1994): 2756–68. http://dx.doi.org/10.1175/1520-0469(1994)051<2756:qdott>2.0.co;2.

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Carton, Xavier. "Instability of Surface Quasigeostrophic Vortices." Journal of the Atmospheric Sciences 66, no. 4 (April 1, 2009): 1051–62. http://dx.doi.org/10.1175/2008jas2872.1.

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Abstract The instability of circular vortices is studied numerically in the surface quasigeostrophic (SQG) model, and their evolutions are compared with those of barotropically unstable 2D vortices. The growth rates in the SQG model evidence similarity with their barotropic counterparts for moderate radial gradients of temperature (or of vorticity in the 2D model). For stronger gradients, SQG vortices are more unstable than 2D vortices. The nonlinear, finite-amplitude evolutions of perturbed vortices provide evidence that moderately unstable, elliptically perturbed vortices form tripoles. When

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Zhmur, V. V., and K. K. Pankratov. "Dynamics of desingularized quasigeostrophic vortices." Physics of Fluids A: Fluid Dynamics 3, no. 5 (May 1991): 1464. http://dx.doi.org/10.1063/1.857998.

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Rozprawy doktorskie na temat "Quasigeostrophic"

Nadeau, Louis-Philippe. "Dynamics of a quasigeostrophic antarctic circumpolar current." Thesis, McGill University, 2011. http://digitool.Library.McGill.CA:80/R/?func=dbin-jump-full&object_id=96911.

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The idea that basin-like dynamics may influence or control the Antarctic Circumpolar Current (ACC) is investigated with idealized analytic and numerical models. A simple 2-layer analytic model is developed to predict the transport evolution with the wind stress amplitude. At very low forcing, a non-zero minimum is predicted. This is followed by two distinct dynamical regimes for stronger forcing: a linearly increasing Stommel regime and a saturation regime in which the transport ceases to increase. The vertical distribution of the flow obtained using the geometry of the geostrophic contours (o

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Vallgren, Andreas. "Statistical characteristics of two-dimensional and quasigeostrophic turbulence." Licentiate thesis, KTH, Linné Flow Center, FLOW, 2010. http://urn.kb.se/resolve?urn=urn:nbn:se:kth:diva-13128.

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<p>Two codes have been developed and implemented for use on massively parallelsuper computers to simulate two-dimensional and quasigeostrophic turbulence.The codes have been found to scale well with increasing resolution and width ofthe simulations. This has allowed for the highest resolution simulations of two-dimensional and quasigeostrophic turbulence so far reported in the literature.The direct numerical simulations have focused on the statistical characteristicsof turbulent cascades of energy and enstrophy, the role of coherent vorticesand departures from universal scaling laws, theoretiz

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Wells, David Reese. "A Two-Level Method For The Steady-State Quasigeostrophic Equation." Thesis, Virginia Tech, 2013. http://hdl.handle.net/10919/23090.

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The quasi-geostrophic equations (QGE) are a model of large-scale ocean flows. We consider a pure stream function formulation and cite results for optimal error estimates for finding approximate solutions with the finite element method. We examine both the time dependent and steady-state versions of the equations. Numerical experiments verify the error estimates.<br />We examine the Argyris finite element and derive the transformation matrix necessary to perform calculations on the reference triangle. We use the Argyris element because it is a high-order, conforming finite element for fourth or

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Zidikheri, Meelis Juma, and m. zidikheri@bom gov au. "Dynamical Subgrid-scale Parameterizations for Quasigeostrophic Flows using Direct Numerical Simulations." The Australian National University. Research School of Physical Sciences and Engineering, 2008. http://thesis.anu.edu.au./public/adt-ANU20090108.112027.

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In this thesis, parameterizations of non-linear interactions in quasigeostrophic (QG) flows for severely truncated models (STM) and Large Eddy Simulations (LES) are studied. Firstly, using Direct Numerical Simulations (DNS), atmospheric barotropic flows over topography are examined, and it is established that such flows exhibit multiple equilibrium states for a wide range of parameters. A STM is then constructed, consisting of the large scale zonal flow and a topographic mode. It is shown that, qualitatively, this system behaves similarly to the DNS as far as the interaction between the zonal

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Zidikheri, Meelis Juma. "Dynamical subgrid-scale parameterizations for quasigeostrophic flows using direct numerical simulations /." View thesis entry in Australian Digital Theses, 2007. http://thesis.anu.edu.au/public/adt-ANU20090108.112027/index.html.

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Johnson, John Edward. "An assessment of data requirements for quasigeostrophic nowcasts and hindcasts of a mesoscale eddy field in the California Current System with application to fall transition." Diss., Monterey, California : Naval Postgraduate School, 1990. http://handle.dtic.mil/100.2/ADA231394.

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Dissertation (Doctor of Philosophy)--Naval Postgraduate School, March 1990.<br>Dissertation Supervisor(s): Mooers, Christopher N.K. Description based on signature page August 25, 2009. DTIC Descriptor(s): Accuracy, California, Cyclones, Data Storage Systems, Density, Digital Simulation, Dynamics, Environments, Functions (Mathematics), Height, Images, Mathematical Models, Mean, North (Direction), Ocean Currents, Ocean Surface, Oceans, Predictions, Pressure Gradients, Requirements, Satellite Photography, Sea Water, Sensitivity, Surface Temperature, Surfaces, Topography, Transitions, Upwelling,

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Blackbourn, Luke A. K. "An analytical, phenomenological and numerical study of geophysical and magnetohydrodynamic turbulence in two dimensions." Thesis, University of St Andrews, 2013. http://hdl.handle.net/10023/4291.

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In this thesis I study a variety of two-dimensional turbulent systems using a mixed analytical, phenomenological and numerical approach. The systems under consideration are governed by the two-dimensional Navier-Stokes (2DNS), surface quasigeostrophic (SQG), alpha-turbulence and magnetohydrodynamic (MHD) equations. The main analytical focus is on the number of degrees of freedom of a given system, defined as the least value $N$ such that all $n$-dimensional ($n$ ≥ $N$) volume elements along a given trajectory contract during the course of evolution. By equating $N$ with the number of active Fo

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Kiss, Andrew Elek, and Andrew Kiss@anu edu au. "Dynamics of laboratory models of the wind-driven ocean circulation." The Australian National University. Research School of Earth Sciences, 2001. http://thesis.anu.edu.au./public/adt-ANU20011018.115707.

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This thesis presents a numerical exploration of the dynamics governing rotating flow driven by a surface stress in the " sliced cylinder " model of Pedlosky & Greenspan (1967) and Beardsley (1969), and its close relative, the " sliced cone " model introduced by Griffiths & Veronis (1997). The sliced cylinder model simulates the barotropic wind-driven circulation in a circular basin with vertical sidewalls, using a depth gradient to mimic the effects of a gradient in Coriolis parameter. In the sliced cone the vertical sidewalls are replaced by an azimuthally uniform slope around the

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Książki na temat "Quasigeostrophic"

R, Holland William, Malanotte-Rizzoli Paola 1946-, and United States. National Aeronautics and Space Administration., eds. Assimilation of altimeter data into a quasigeostrophic model of the Gulf Stream system. [Washington, DC: National Aeronautics and Space Administration, 1995.

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1946-, Malanotte-Rizzoli Paola, Holland William R, and United States. National Aeronautics and Space Administration., eds. Assimilation of altimeter data into a quasigeostrophic model of the Gulf Stream system. [Washington, DC: National Aeronautics and Space Administration, 1995.

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Quasigeostrophic Theory Of Oceans And Atmosphere Topics In The Dynamics And Thermodynamics Of The Fluid Earth. Springer, 2012.

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United States. National Aeronautics and Space Administration., ed. Assimilation Of Altimeter Data Into A Quasigeostrophic Model Of The Gulf Stream System... NASA-CR-205501... Oct. 31, 1997. [S.l: s.n., 1998.

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Chemin, Jean-Yves, Benoit Desjardins, Isabelle Gallagher, and Emmanuel Grenier. Mathematical Geophysics. Oxford University Press, 2006. http://dx.doi.org/10.1093/oso/9780198571339.001.0001.

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Aimed at graduate students, researchers and academics in mathematics, engineering, oceanography, meteorology, and mechanics, this text provides a detailed introduction to the physical theory of rotating fluids, a significant part of geophysical fluid dynamics. The text is divided into four parts, with the first part providing the physical background of the geophysical models to be analyzed. Part two is devoted to a self contained proof of the existence of weak (or strong) solutions to the imcompressible Navier-Stokes equations. Part three deals with the rapidly rotating Navier-Stokes equations

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Części książek na temat "Quasigeostrophic"

Lackmann, Gary. "Quasigeostrophic Theory." In Midlatitude Synoptic Meteorology, 35–66. Boston, MA: American Meteorological Society, 2011. http://dx.doi.org/10.1007/978-1-878220-56-1_2.

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Özsoy, Emin. "Quasigeostrophic Theory." In Geophysical Fluid Dynamics I, 183–92. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-16973-2_7.

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Holland, William R. "Quasigeostrophic Modelling of Eddy-Resolved Ocean Circulation." In Advanced Physical Oceanographic Numerical Modelling, 203–31. Dordrecht: Springer Netherlands, 1986. http://dx.doi.org/10.1007/978-94-017-0627-8_14.

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Bartello, Peter. "Quasigeostrophic and stratified turbulence in the atmosphere." In IUTAM Symposium on Turbulence in the Atmosphere and Oceans, 117–30. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-94-007-0360-5_10.

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Pedlosky, Joseph. "Quasigeostrophic Motion of a Stratified Fluid on a Sphere." In Geophysical Fluid Dynamics, 336–489. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-4650-3_6.

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Duan, Jinqiao, Peter E. Kloeden, and Björn Schmalfuss. "Exponential stability of the quasigeostrophic equation under random perturbations." In Stochastic Climate Models, 241–56. Basel: Birkhäuser Basel, 2001. http://dx.doi.org/10.1007/978-3-0348-8287-3_10.

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Nielsen-Gammon, John W., and David A. Gold. "Dynamical Diagnosis: A Comparison of Quasigeostrophy and Ertel Potential Vorticity." In Synoptic—Dynamic Meteorology and Weather Analysis and Forecasting, 183–202. Boston, MA: American Meteorological Society, 2008. http://dx.doi.org/10.1007/978-0-933876-68-2_9.

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Davies, H. C., and H. Wernli. "DYNAMICAL METEOROLOGY | Quasigeostrophic Theory." In Encyclopedia of Atmospheric Sciences, 393–403. Elsevier, 2015. http://dx.doi.org/10.1016/b978-0-12-382225-3.00326-1.

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Salmon, Rick. "Geostrophic Turbulence." In Lectures on Geophysical Fluid Dynamics. Oxford University Press, 1998. http://dx.doi.org/10.1093/oso/9780195108088.003.0009.

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Strongly nonlinear, rapidly rotating, stably stratified flow is called geostrophic turbulence. This subject, which blends ideas from chapters 2,4, and 5, is relevant to the large-scale flow in the Earth’s oceans and atmosphere. The quasigeostrophic equations form the basis of the study of geostrophic turbulence. We view the quasigeostrophic equations as a generalization of the vorticity equation for two-dimensional turbulence to include the important effects of stratification, bottom topography, and varying Coriolis parameter. Thus the theory of geostrophic turbulence represents an extension of the theory of two dimensional turbulence. However, its richer physics and greater applicability to real geophysical flows make geostrophic turbulence a much more interesting and important subject. This chapter offers a very brief introduction to the theory of geostrophic turbulence. We illustrate the principal ideas by separately considering the effects of bottom topography, varying Coriolis parameter, and density stratification on highly nonlinear, quasigeostrophic flow. We make no attempt at a comprehensive review. In every case, the theory of geostrophic turbulence relies almost solely on two now-familiar components: a conservation principle that energy and potential vorticity are (nearly) conserved and an irreversibility principle in the form of an appealing assumption that breaks the time-reversal symmetry of the exact (inviscid) dynamics. This irreversibility assumption takes a great many superficially dissimilar forms, fostering the misleading impression of a great many competing explanations for the same phenomena. However, broadminded analysis inevitably reveals that these competing explanations are virtually equivalent. We begin by considering the quasigeostrophic flow of a single layer of homogeneous fluid over a bumpy bottom. No case better illustrates how diverse forms of the irreversibility principle lead to the same conclusions.

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Carton, X. J., and J. C. Mcwilliams. "Barotropic and Baroclinic Instabilities of Axisymmetric Vortices in a Quasigeostrophic Model." In Mesoscale/Synoptic Coherent structures in Geophysical Turbulence, 225–44. Elsevier, 1989. http://dx.doi.org/10.1016/s0422-9894(08)70188-0.

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Streszczenia konferencji na temat "Quasigeostrophic"

Miglietta, Victoria M., and Manhar R. Dhanak. "Current Turbine Array Placement in Quasigeostrophic Flows Over Bottom Topography." In OCEANS 2019 MTS/IEEE SEATTLE. IEEE, 2019. http://dx.doi.org/10.23919/oceans40490.2019.8962717.

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