Relevant bibliographies by topics / Baroclinic

Academic literature on the topic 'Baroclinic'

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Published: 4 June 2021
Last updated: 1 February 2022

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Journal articles on the topic "Baroclinic"

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Donohoe, Aaron, and David S. Battisti. "Causes of Reduced North Atlantic Storm Activity in a CAM3 Simulation of the Last Glacial Maximum." Journal of Climate 22, no. 18 (September 15, 2009): 4793–808. http://dx.doi.org/10.1175/2009jcli2776.1.

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Abstract The aim of this paper is to determine how an atmosphere with enhanced mean-state baroclinity can support weaker baroclinic wave activity than an atmosphere with weak mean-state baroclinity. As a case study, a Last Glacial Maximum (LGM) model simulation previously documented to have reduced baroclinic storm activity, relative to the modern-day climate (simulated by the same model), despite having an enhanced midlatitude temperature gradient, is considered. Several candidate mechanisms are evaluated to explain this apparent paradox. A linear stability analysis is first performed on the jet in the modern-day and the LGM simulation; the latter has relatively strong barotropic velocity shear. It was found that the LGM mean state is more unstable to baroclinic disturbances than the modern-day mean state, although the three-dimensional jet structure does stabilize the LGM jet relative to the Eady growth rate. Next, feature tracking was used to assess the storm track seeding and temporal growth of disturbances. It was found that the reduction in LGM eddy activity, relative to the modern-day eddy activity, is due to the smaller magnitude of the upper-level storms entering the North Atlantic domain in the LGM. Although the LGM storms do grow more rapidly in the North Atlantic than their modern-day counterparts, the storminess in the LGM is reduced because storms seeding the region of enhanced baroclinity are weaker.
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Pierrehumbert, R. T., and K. L. Swanson. "Baroclinic Instability." Annual Review of Fluid Mechanics 27, no. 1 (January 1995): 419–67. http://dx.doi.org/10.1146/annurev.fl.27.010195.002223.

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Kantha, Lakshmi H., and Craig C. Tierney. "Global baroclinic tides." Progress in Oceanography 40, no. 1-4 (January 1997): 163–78. http://dx.doi.org/10.1016/s0079-6611(97)00028-1.

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REZNIK, GREGORY M., and GEORGI G. SUTYRIN. "Baroclinic topographic modons." Journal of Fluid Mechanics 437 (June 22, 2001): 121–42. http://dx.doi.org/10.1017/s0022112001004062.

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The theory of solitary topographic Rossby waves (modons) in a uniformly rotating two-layer ocean over a constant slope is developed. The modon is described by an exact, form-preserving, uniformly translating, horizontally localized, nonlinear solution to the inviscid quasi-geostrophic equations. Baroclinic topographic modons are found to translate steadily along contours of constant depth in both directions: either with negative speed (within the range of the phase velocities of linear topographic waves) or with positive speed (outside the range of the phase velocities of linear topographic waves). The lack of resonant wave radiation in the first case is due to the orthogonality of the flow field in the modon exterior to the linear topographic wave field propagating with the modon translation speed, that is impossible for barotropic modons. Another important property of a baroclinic topographic modon is that its integral angular momentum must be zero only in the bottom layer; the total angular momentum can be non-zero unlike for the beta-plane modons over flat bottom. This feature allows modon solutions superimposed by intense monopolar vortices in the surface layer to exist. Explicit analytical solutions for the baroclinic topographic modons with piecewise linear dependence of the potential vorticity on the streamfunction are presented and analysed.
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Cehelsky, Priscilla, and Ka Kit Tung. "Nonlinear Baroclinic Adjustment." Journal of the Atmospheric Sciences 48, no. 17 (September 1991): 1930–47. http://dx.doi.org/10.1175/1520-0469(1991)048<1930:nba>2.0.co;2.

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Fleming, Rex J. "Explosive Baroclinic Instability." Journal of the Atmospheric Sciences 71, no. 6 (May 30, 2014): 2155–68. http://dx.doi.org/10.1175/jas-d-13-0323.1.

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Abstract A low-order general circulation model contains all the elements of baroclinic instability, including differential heating to drive the mean zonal shear flow against dissipation. Simulations exhibit vacillation ending in fixed-point solutions and chaotic solutions with significant amplifications of the baroclinic cycles compared to those of vacillation. The chaos sensitivity to initial conditions, covering a broad landscape of initial values, demands analysis of why the chaos occurs and its impact on subsequent storm intensity. Three attractors found in the dynamic system are important. One attractor is the stable fixed-point solution—the ultimate destination of a vacillation trajectory. A second attractor represents an unstable zonal solution. Though this dynamic system is bound, some trajectories get extremely close to the unstable, but strongly attracting, zonal solution. It is while traversing such a trajectory that the buildup of available potential energy is such to allow subsequent explosive baroclinic instability to develop. The roots of the characteristic matrix of the dynamic system are examined at every time step. A single critical value of one of the roots is found to be the cause of the chaos for a given value of the differential heating H. The system becomes more stable with increased values of H; vacillation is stronger and more prominent, and the critical value for chaos increases with H. When chaos does occur, it is stronger and more explosive.
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Zhang, Zheen, Xueen Chen, and Thomas Pohlmann. "The Impact of Fortnightly Stratification Variability on the Generation of Baroclinic Tides in the Luzon Strait." Journal of Marine Science and Engineering 9, no. 7 (June 26, 2021): 703. http://dx.doi.org/10.3390/jmse9070703.

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The impact of fortnightly stratification variability induced by tide–topography interaction on the generation of baroclinic tides in the Luzon Strait is numerically investigated using the MIT general circulation model. The simulation shows that advection of buoyancy by baroclinic flows results in daily oscillations and a fortnightly variability in the stratification at the main generation site of internal tides. As the stratification for the whole Luzon Strait is periodically redistributed by these flows, the energy analysis indicates that the fortnightly stratification variability can significantly affect the energy transfer between barotropic and baroclinic tides. Due to this effect on stratification variability by the baroclinic flows, the phases of baroclinic potential energy variability do not match the phase of barotropic forcing in the fortnight time scale. This phenomenon leads to the fact that the maximum baroclinic tides may not be generated during the maximum barotropic forcing. Therefore, a significant impact of stratification variability on the generation of baroclinic tides is demonstrated by our modeling study, which suggests a lead–lag relation between barotropic tidal forcing and maximum baroclinic response in the Luzon Strait within the fortnightly tidal cycle.
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Ji, Xuan, J. David Neelin, and C. Roberto Mechoso. "Baroclinic-to-Barotropic Pathway in El Niño–Southern Oscillation Teleconnections from the Viewpoint of a Barotropic Rossby Wave Source." Journal of the Atmospheric Sciences 73, no. 12 (November 29, 2016): 4989–5002. http://dx.doi.org/10.1175/jas-d-16-0053.1.

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Abstract The baroclinic-to-barotropic pathway in ENSO teleconnections is examined from the viewpoint of a barotropic Rossby wave source that results from decomposition into barotropic and baroclinic components. Diagnoses using the NCEP–NCAR reanalysis are supplemented by analysis of the response of a tropical atmospheric model of intermediate complexity to the NCEP–NCAR barotropic Rossby wave source. Among the three barotropic Rossby wave source contributions (shear advection, vertical advection, and surface drag), the leading contribution is from shear advection and, more specifically, the mean baroclinic zonal wind advecting the anomalous baroclinic zonal wind. Vertical advection is the smallest term, while surface drag tends to cancel and reinforce the shear advection in different regions through damping on the baroclinic mode, which spins up a barotropic response. There are also nontrivial impacts of transients in the barotropic wind response to ENSO. Both tropical and subtropical baroclinic vorticity advection contribute to the barotropic component of the Pacific subtropical jet near the coast of North America, where the resulting barotropic wind contribution approximately doubles the zonal jet anomaly at upper levels, relative to the baroclinic anomalies alone. In this view, the barotropic Rossby wave source in the subtropics simply arises from the basic-state baroclinic flow acting on the well-known baroclinic ENSO flow pattern that spreads from the deep tropics into the subtropics over a scale of equatorial radius of deformation. This is inseparably connected to the leading deep tropical Rossby wave source that arises from eastern Pacific climatological baroclinic winds advecting the tropical portion of the same ENSO flow pattern.
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Canals, Miguel, Geno Pawlak, and Parker MacCready. "Tilted Baroclinic Tidal Vortices." Journal of Physical Oceanography 39, no. 2 (February 1, 2009): 333–50. http://dx.doi.org/10.1175/2008jpo3954.1.

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Abstract The structure of baroclinic vortices generated by horizontal flow separation past a sloping headland in deep, stably stratified waters is investigated. The most distinctive feature of these eddies is that their cores are strongly tilted with respect to the stratification, yet their velocity field remains quasi-horizontal. Field observations and numerical simulations are used to explore the consequences of the strong tilt on the eddy baroclinic structure. It is found that the background density field is altered in such a way as to maintain a pressure minimum in the tilted vortex cores. This adjustment results in a fundamental asymmetry of the density field. Isopycnals are deflected upward on the shoreward side and downward on the opposite side of the eddy center. The resulting pattern closely resembles the asymmetries of azimuthal wavenumber one that develop when tropical cyclones become tilted by an environmental shear. The authors provide a simple analytical model that suggests this structure is obtained via a balance between the centrifugal force and the horizontal pressure gradient. As the eddies release from the boundary, adjust, and decay, their tilt as well as the associated density perturbation decrease and lose coherence. It is suggested that this may lead to a conversion of potential energy into kinetic energy.
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TIPPETT, MICHAEL K. "Transient moist baroclinic instability." Tellus A 51, no. 2 (March 1999): 273–88. http://dx.doi.org/10.1034/j.1600-0870.1999.t01-2-00008.x.

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Dissertations / Theses on the topic "Baroclinic"

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Früh, Wolf-Gerrit. "Bifurcations to baroclinic chaos." Thesis, University of Oxford, 1993. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.358616.

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Pita, A. A. C. "Synchronization in baroclinic systems." Thesis, University of Oxford, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.489417.

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In recent years, the study of synchronization phenomena in nonlinear systems has made a number of significant advances in various areas of physics, engineering and the life sciences. Ideas of chaos synchronization have been used recently in some atmospheric phenomena as an attempt to better understand certain kinds of cyclic behaviour and teleconnection patterns, and at least some have shown promising results.
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Foreman, S. J. "Baroclinic instability and blocking." Thesis, University of Reading, 1985. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.354071.

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Cenedese, Claudia. "Baroclinic eddies over topography." Thesis, University of Cambridge, 1999. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.624104.

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Castrejón-Pita, Alfonso Arturo. "Synchronisation in baroclinic systems." Thesis, University of Oxford, 2008. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.670072.

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Thompson, Andrew F. "Eddy fluxes in baroclinic turbulence." Connect to a 24 p. preview or request complete full text in PDF format. Access restricted to UC campuses, 2006. http://wwwlib.umi.com/cr/ucsd/fullcit?p3225998.

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Thesis (Ph. D.)--University of California, San Diego, 2006.
Title from first page of PDF file (viewed October 10, 2006). Available via ProQuest Digital Dissertations. Vita. Includes bibliographical references (p. 173-182).
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Stephen, Adam Vercingetorix. "POD methods in baroclinic flows." Thesis, University of Oxford, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.302401.

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Elliott, Simon S. "Numerical studies of baroclinic instability." Thesis, University of Oxford, 1995. http://ora.ox.ac.uk/objects/uuid:eb0c26fe-b0f0-4f2b-aa3b-00428cdd2a57.

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This thesis describes two studies of baroclinic instability in a rotating fluid annulus subject to differential heating. The first part is concerned with the development of a time dependent axisymmetric numerical model. The model was formulated using the control volume finite element method and was designed to be as flexible as possible both in terms of the range of problems to be studied and the techniques used to study them. Details of these techniques are presented together with a discussion of their limitations and possible refinements and extensions which could be made. The second part of this thesis describes a numerical study of unstable normal mode perturbations which can develop on a prescribed mean state. The growth rate and structure of these modes are examined for various background states and the relevance of these results to laboratory measurements is discussed. Evidence is presented to suggest the possible presence of hitherto unobserved baroclinic weak waves in an internally heated annulus system.
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Methven, John. "Tracer behaviour in baroclinic waves." Thesis, University of Reading, 1996. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.296636.

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James, Paul Martin. "Interannual variability in a baroclinic atmosphere." Thesis, University of Reading, 1991. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.290299.

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Books on the topic "Baroclinic"

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

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

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

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

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

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

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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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Book chapters on the topic "Baroclinic"

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Lackmann, Gary. "Baroclinic Instability." In Midlatitude Synoptic Meteorology, 167–91. Boston, MA: American Meteorological Society, 2011. http://dx.doi.org/10.1007/978-1-878220-56-1_7.

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Hopfinger, E. J. "Baroclinic Turbulence." In Rotating Fluids in Geophysical and Industrial Applications, 359–69. Vienna: Springer Vienna, 1992. http://dx.doi.org/10.1007/978-3-7091-2602-8_16.

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Carton, Xavier J., and Stéphanie M. Corréard. "Baroclinic Tripolar Geostrophic Vortices." In Fluid Mechanics and Its Applications, 181–90. Dordrecht: Springer Netherlands, 1999. http://dx.doi.org/10.1007/978-94-011-4601-2_16.

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Linden, P. F. "Barotropic and Baroclinic Instabilities." In Rotating Fluids in Geophysical and Industrial Applications, 85–98. Vienna: Springer Vienna, 1992. http://dx.doi.org/10.1007/978-3-7091-2602-8_5.

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Dymnikov, Valentin P., and Aleksander N. Filatov. "Two-Layer Baroclinic Model." In Mathematics of Climate Modeling, 189–209. Boston, MA: Birkhäuser Boston, 1997. http://dx.doi.org/10.1007/978-1-4612-4148-5_6.

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Ghil, M., and S. Childress. "Effects of Stratification: Baroclinic Instability." In Topics in Geophysical Fluid Dynamics: Atmospheric Dynamics, Dynamo Theory, and Climate Dynamics, 44–72. New York, NY: Springer New York, 1987. http://dx.doi.org/10.1007/978-1-4612-1052-8_4.

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Früh, Wolf-Gerrit. "Amplitude Vacillation in Baroclinic Flows." In Modeling Atmospheric and Oceanic Flows, 61–81. Hoboken, NJ: John Wiley & Sons, Inc, 2014. http://dx.doi.org/10.1002/9781118856024.ch3.

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Pedlosky, Joseph. "Baroclinic Instability: The Charney Paradigm*." In The Atmosphere — A Challenge, 159–76. Boston, MA: American Meteorological Society, 1990. http://dx.doi.org/10.1007/978-1-944970-35-2_10.

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Zhang, L., and C. Sun. "Baroclinic Structure of Oceanic Rings." In New Trends in Fluid Mechanics Research, 412. Berlin, Heidelberg: Springer Berlin Heidelberg, 2007. http://dx.doi.org/10.1007/978-3-540-75995-9_133.

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Baines, Peter G. "Internal tides, internal waves and near-inertial motions." In Baroclinic Processes on Continental Shelves, 19–31. Washington, D. C.: American Geophysical Union, 1986. http://dx.doi.org/10.1029/co003p0019.

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Conference papers on the topic "Baroclinic"

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Men'shov, Igor, and Yoshiaki Nakamura. "Instability Modes Acoustically Excited in Baroclinic Vortices." In 3rd Theoretical Fluid Mechanics Meeting. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2002. http://dx.doi.org/10.2514/6.2002-2986.

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GS, Sidharth, Graham V. Candler, and Paul Dimotakis. "Baroclinic Torque and Implications for Subgrid-Scale Modeling." In 7th AIAA Theoretical Fluid Mechanics Conference. Reston, Virginia: American Institute of Aeronautics and Astronautics, 2014. http://dx.doi.org/10.2514/6.2014-3214.

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Zheng, Y., J. Mo, and Basil Antar. "A numerical analysis of strongly nonlinear baroclinic instability." In 33rd Aerospace Sciences Meeting and Exhibit. Reston, Virigina: American Institute of Aeronautics and Astronautics, 1995. http://dx.doi.org/10.2514/6.1995-197.

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Callies, Jörn. "Video: Baroclinic instability in the presence of forced convection." In 68th Annual Meeting of the APS Division of Fluid Dynamics. American Physical Society, 2015. http://dx.doi.org/10.1103/aps.dfd.2015.gfm.v0020.

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Zou, Xin, Xin Yuan, and W. N. Dawes. "The Role of Density Gradient in Species Migration and Secondary Flow Structures in Axial Flow Turbines." In ASME Turbo Expo 2013: Turbine Technical Conference and Exposition. American Society of Mechanical Engineers, 2013. http://dx.doi.org/10.1115/gt2013-94235.

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Physical quantities at combustor exit, hence turbine inlet, are highly non-uniform not just due to spatially varying combustion but also due to the dilution air and film-cooling air used in the combustor design. The effects of inlet total pressure and temperature (“hot streak”) non-uniformity on the unsteady flow and heat transfer of turbine stages have been widely studied. However, few studies have considered the effects of inlet density non-uniformity derived from spatially varying species concentration (“species streak”). This “species streak” results in density gradients which, if not aligned with pressure gradients, will lead to the generation of baroclinic torque which will influence the generation, migration and evolution of vorticity within the turbine passages and hence the secondary flow structure and mixing within the blade row. This paper examines the “species streak” effects on the unsteady flow and heat transfer within a high-pressure axial flow turbine stage focusing on the flow through the rotor. First, a validation study was carried out to check the capability of the selected CFD in modeling unsteady turbine stage flows. Time-accurate solutions were achieved and the results agreed well with the available experimental measurements. Based on the validation, two expanded case studies were carried out to investigate the “species streak” effects on the secondary flow and heat transfer in turbine rotor passages. It was found that the “species streak” could generate “hot streak enhancement structure” as well as “baroclinic torque structure” in rotor passages, which would work with the inherent secondary flow structures in rotor to determine its heat transfer. It was also found that the contributions of the baroclinic torque source term could have magnitudes comparable to other effects, such as vortex stretching, in creating secondary flows. In some circumstances, however, the overall effects of the baroclinic torque could be partially reduced by opposite vortex stretching effects generated by the same density gradients.
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Ogino, Yousuke, Masami Tate, and Naofumi Ohnishi. "Shock Control with Baroclinic Vortex Induced by a Pulse Energy Deposition." In 47th AIAA Aerospace Sciences Meeting including The New Horizons Forum and Aerospace Exposition. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2009. http://dx.doi.org/10.2514/6.2009-1225.

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Mahloul, M., A. Mahamdia, N. Merabet, and E. Adnane. "EXPERIMENTAL INVESTIGATION OF SYMMETRICAL BAROCLINIC INSTABILITY BETWEEN TWO CONCENTRIC ROTATING SPHERES." In Topical Problems of Fluid Mechanics 2018. Institute of Thermomechanics, AS CR, v.v.i., 2018. http://dx.doi.org/10.14311/tpfm.2018.026.

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Hirosawa, Takuya, Hiroshi Kusakawa, Hironori Yamada, Wataru Takizawa, Yuma Mano, Takuo Kuwahara, and Mitsuaki Tanabe. "Roles of Baroclinic Torque by Acoustic Oscillation on Structure of Premixed Flame." In 50th AIAA Aerospace Sciences Meeting including the New Horizons Forum and Aerospace Exposition. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2012. http://dx.doi.org/10.2514/6.2012-341.

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Romagnosi, L., Antonella Ingenito, Donato Cecere, Giacomazzi Eugenio, and Claudio Bruno. "The role of the baroclinic term in supersonic fuel/air mixing enhancement." In 49th AIAA Aerospace Sciences Meeting including the New Horizons Forum and Aerospace Exposition. Reston, Virigina: American Institute of Aeronautics and Astronautics, 2011. http://dx.doi.org/10.2514/6.2011-401.

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Dresback, K. M., E. M. Tromble, D. G. Reid, R. L. Kolar, T. C. G. Kibbey, C. A. Blain, R. A. Luettich, Jr., and C. M. Szpilka. "Evaluation of Baroclinic ADCIRC Using a Process-Oriented Test along a Slope." In International Conference on Estuarine and Coastal Modeling 2012. Reston, VA: American Society of Civil Engineers, 2012. http://dx.doi.org/10.1061/9780784412411.00005.

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Reports on the topic "Baroclinic"

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Kolar, R. L., J. Antonio, S. Dhall, and S. Lakshmivarahan. A Parallel, 3D Baroclinic Shallow Water Model. Fort Belvoir, VA: Defense Technical Information Center, September 2003. http://dx.doi.org/10.21236/ada620404.

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Nechaev, Dmitri, Henry Perkins, Gregg Jacobs, Pavel Pistek, William Teague, and Alex Ostrovsky. Baroclinic Data Assimilation in Korea/Tsushima Strait. Fort Belvoir, VA: Defense Technical Information Center, September 2001. http://dx.doi.org/10.21236/ada625251.

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Lindzen, Richard S. Dynamic heat and moisture transport and baroclinic adjustment. Office of Scientific and Technical Information (OSTI), April 2002. http://dx.doi.org/10.2172/771316.

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Skyllingstad, Eric D., and Roger M. Samelson. Large-Eddy Simulations of Baroclinic Instability and Turbulent Mixing. Fort Belvoir, VA: Defense Technical Information Center, September 2010. http://dx.doi.org/10.21236/ada542829.

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Skyllingstad, Eric D., and Roger M. Samuelson. Large-Eddy Simulations of Baroclinic Instability and Turbulent Mixing. Fort Belvoir, VA: Defense Technical Information Center, September 2013. http://dx.doi.org/10.21236/ada602484.

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Skyllingstad, Eric D., and Roger M. Samelson. Large-Eddy Simulations of Baroclinic Instability and Turbulent Mixing. Fort Belvoir, VA: Defense Technical Information Center, September 2012. http://dx.doi.org/10.21236/ada590579.

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Drake, John B. A Vertical Grid Module for Baroclinic Models of the Atmosphere. Office of Scientific and Technical Information (OSTI), April 2008. http://dx.doi.org/10.2172/969953.

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Alford, Matthew. Dynamics and Structure of Baroclinic Tides in Mamala Bay, Oahu, Hawaii. Fort Belvoir, VA: Defense Technical Information Center, September 2003. http://dx.doi.org/10.21236/ada629118.

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9

Farrell, B. F. Role of baroclinic wave amplitude and transport variation in climate change. Final report. Office of Scientific and Technical Information (OSTI), April 1998. http://dx.doi.org/10.2172/582181.

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Scott, A., and S. Mitran. Barotropic to Baroclinic Energy Conversion Across Topographyically Rough Straits With Application to the Luzon Strait. Fort Belvoir, VA: Defense Technical Information Center, September 2009. http://dx.doi.org/10.21236/ada531806.

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