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Libros sobre el tema "Topographic flow"

Autor: Grafiati
Publicado: 25 de mayo de 2024
Última modificación: 31 de julio de 2025

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1

Baines, Peter G. Topographic effects in stratified flows. Cambridge University Press, 1995.

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2

Thompson, LuAnne. Flow over finite isolated topography. Woods Hole Oceanographic Institution, 1990.

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3

Rennick, Mary Alice. Air flow over large scale topography. Naval Postgraduate School, 1989.

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4

Luca, Ioana, Yih-Chin Tai, and Chih-Yu Kuo. Shallow Geophysical Mass Flows down Arbitrary Topography. Springer International Publishing, 2016. http://dx.doi.org/10.1007/978-3-319-02627-5.

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5

Carl, Freeman D., and Intermountain Research Station (Ogden, Utah), eds. Influence of topography on cumulative pollen flow of fourwing saltbush. U.S. Dept. of Agriculture, Forest Service, Intermountain Research Station, 1993.

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6

Petroliagis, Thomas I. Studies of barotropic flow over topography using a Galerkin Finite Element model. Naval Postgraduate School, 1988.

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7

Skupniewicz, C. E. Vandenberg Boundary Layer Survey (VBLS): Final report - results. Naval Postgraduate School, 1990.

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8

Rao, Desiraju B. A method of calculating the total flow from a given sea surface topography. Goddard Space Flight Center, 1987.

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9

P, Castro I., Rockliff N. J, and Institute of Mathematics and Its Applications., eds. Stably stratified flows: Flow and dispersion over topography : based on the proceedings of the Fourth Conference on Stably Stratified Flows, organized by the Institute of Mathematics and Its Applications and held at the University of Surrey in September, 1992. Clarendon Press, 1994.

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10

Batchelor, G. K., Peter G. Baines, L. B. Freud, S. Leibovich, and V. Tvergaard. Topographic Effects in Stratified Flows. Cambridge University Press, 1997.

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11

Baines, Peter G. Topographic Effects in Stratified Flows. University of Cambridge ESOL Examinations, 2021.

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12

Baines, Peter G. Topographic Effects in Stratified Flows. University of Cambridge ESOL Examinations, 2021.

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13

Zeitlin, Vladimir. Getting Rid of Fast Waves: Slow Dynamics. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0005.

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After analysis of general properties of horizontal motion in primitive equations and introduction of principal parameters, the key notion of geostrophic equilibrium is introduced. Quasi-geostrophic reductions of one- and two-layer rotating shallow-water models are obtained by a direct filtering of fast inertia–gravity waves through a choice of the time scale of motions of interest, and by asymptotic expansions in Rossby number. Properties of quasi-geostrophic models are established. It is shown that in the beta-plane approximations the models describe Rossby waves. The first idea of the classi
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14

Anderson, James A. Cerebral Cortex. Oxford University Press, 2018. http://dx.doi.org/10.1093/acprof:oso/9780199357789.003.0010.

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Hardware matters. The neural organ largely responsible for cognition is the cerebral cortex of mammals. Cortex is a thin two-dimensional layered structure arranged with on the order of a few hundred interconnected regions that seem to be specialized for particular operations. Regions often show topographic organization. Early vision displays an interestingly distorted topographic map of the retinal input, audition has a topographic map of frequency, and there is a distorted map of the body surface on the somatosensory areas. Information in cortex is not “processed” with an orderly flow from ra
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15

Witter, Donna Lynn. Unstable jet flow along zonal ridge topography. 1995.

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16

Interaction of Large Scale Zonal Flow Anomalies and Topography. Storming Media, 2004.

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17

(Editor), I. P. Castro, and N. J. Rockliff (Editor), eds. Stably Stratified Flows: Flow and Dispersion over Topography (Institute of Mathematics and Its Applications Conference Series New Series). Oxford University Press, USA, 1994.

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18

Stratified rotating flow over and around isolated three-dimensional topography. Royal Society, 1987.

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19

Blatt, Ari J., and Edward Welch, eds. France in Flux. Liverpool University Press, 2019. http://dx.doi.org/10.3828/liverpool/9781786941787.001.0001.

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The look and feel of metropolitan France has been a notable preoccupation of French literary and visual culture since the 1980s. Numerous writers, filmmakers and photographers have been drawn to articulate France’s contrasting spatial qualities, from infrastructural installations such as roads, rail lines and ports, to peri-urban residential developments and isolated rural enclaves. In doing so, they explore how the country’s acute sense of national identity has been both asserted and challenged in topographic terms. This wide-ranging collection of essays explores how the contemporary concern
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20

Michel, Christoph M., and Bin He. EEG Mapping and Source Imaging. Edited by Donald L. Schomer and Fernando H. Lopes da Silva. Oxford University Press, 2017. http://dx.doi.org/10.1093/med/9780190228484.003.0045.

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This chapter describes methods to analyze the scalp electric field recorded with multichannel electroencephalography (EEG). With advances in high-density EEG, systems now allow fast and easy recording from 64 to 256 channels simultaneously. Pattern-recognition algorithms can characterize the topography of scalp electric fields and detect changes in topography over time and between experimental or clinical conditions. Methods for estimating the sources underlying the recorded scalp potential maps have increased the spatial resolution of EEG. The use of anatomical information in EEG source recon
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21

Luca, Ioana, Yih-Chin Tai, and Chih-Yu Kuo. Shallow Geophysical Mass Flows down Arbitrary Topography: Model Equations in Topography-Fitted Coordinates, Numerical Simulation and Back-calculations of Disastrous Events. Springer London, Limited, 2016.

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22

Zeitlin, Vladimir. Instabilities in Cylindrical Geometry: Vortices and Laboratory Flows. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198804338.003.0011.

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Vortex solutions in cyclo-geostrophic equilibrium are described and their geostrophic and ageostrophic barotropic and baroclinic instabilities are studied along the lines of Chapter 10. Special attention is paid to centrifugal instability which, as the inertial instability of jets, is due to modes trapped in the anticyclonic shear in the vortex, and has asymmetric counterparts. Saturation of this instability is shown to exhibit some specific patterns. Instabilities of intense hurricane-like vortices are analysed and shown to be sensitive to fine details of the vortex profile. Nonlinear saturat
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23

Fieberling Guyot moored array data: Office of Naval Research, Accelerated Research Initiative on Flow Over Abrupt Topography. School of Oceanography, University of Washington, 1993.

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24

Luca, Ioana. Shallow Geophysical Mass Flows down Arbitrary Topography: Model Equations in Topography-fitted Coordinates, Numerical Simulation and Back-calculations ... and Environmental Mechanics and Mathematics). Springer, 2018.

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25

Luca, Ioana, Yih-Chin Tai, and Chih-Yu Kuo. Shallow Geophysical Mass Flows down Arbitrary Topography: Model Equations in Topography-fitted Coordinates, Numerical Simulation and Back-calculations ... and Environmental Mechanics and Mathematics). Springer, 2016.

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26

Multiphase Flow Internal Corrosion Direct Assessment (MP-ICDA) Methodology for Pipelines. AMPP, 2022. https://doi.org/10.5006/nace_sp0116-2022.

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Scope This standard practice outlines a methodology to assess pipeline integrity because of the threat internal corrosion in onshore and offshore pipelines and other piping systems that normally carry multiphase fluids (gas, water, and oil) termed multiphase flow internal corrosion direct assessment (MP-ICDA). Liquid separators (drips), compressing stations, vessels, and other equipment not related to pipelines are not included in this standard. This standard applies to pipelines, and piping systems both onshore and offshore, containing carbon dioxide (CO2), hydrogen sulfide (H2S), oxygen (O2)
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27

Collings, David G., Kamel Mellahi, and Wayne F. Cascio, eds. The Oxford Handbook of Talent Management. Oxford University Press, 2017. http://dx.doi.org/10.1093/oxfordhb/9780198758273.001.0001.

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The Oxford Handbook of Talent Management offers a state-of-the-art overview of the key themes, topics, and debates in talent management. The Handbook is designed with a multidisciplinary perspective in mind and it draws upon perspectives from, inter alia, human resource management, psychology, and strategy, to chart the topography of the area of talent management and to establish the base of knowledge in the field. Furthermore, each chapter concludes by identifying key gaps in our understanding of the area of focus. The twenty-eight chapters are structured around five sections. These include t
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28

Lau, William K. M. Impacts of Aerosols on Climate and Weather in the Hindu-Kush-Himalayas-Gangetic Region. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.590.

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Situated at the southern edge of the Tibetan Plateau (TP), the Hindu-Kush-Himalayas-Gangetic (HKHG) region is under the clear and present danger of climate change. Flash-flood, landslide, and debris flow caused by extreme precipitation, as well as rapidly melting glaciers, threaten the water resources and livelihood of more than 1.2 billion people living in the region. Rapid industrialization and increased populations in recent decades have resulted in severe atmospheric and environmental pollution in the region. Because of its unique topography and dense population, the HKHG is not only a maj
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29

Bridges, John C. Evolution of the Martian Crust. Oxford University Press, 2017. http://dx.doi.org/10.1093/acrefore/9780190647926.013.18.

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This is an advance summary of a forthcoming article in the Oxford Encyclopedia of Planetary Science. Please check back later for the full article.Mars, which has a tenth of the mass of Earth, has cooled as a single lithospheric plate. Current topography gravity maps and magnetic maps do not show signs of the plate tectonics processes that have shaped the Earth’s surface. Instead, Mars has been shaped by the effects of meteorite bombardment, igneous activity, and sedimentary—including aqueous—processes. Mars also contains enormous igneous centers—Tharsis and Elysium, with other shield volcanoes
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