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Livros sobre o tema "Topographic flow"

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Autor: Grafiati

Publicado: 25 de maio de 2024

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1

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

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2

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

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3

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

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4

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

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5

Carl, Freeman D., e Intermountain Research Station (Ogden, Utah), eds. Influence of topography on cumulative pollen flow of fourwing saltbush. Ogden, UT (324 25th St., Ogden 84401): 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. Monterey, California: Naval Postgraduate School, 1988.

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7

Skupniewicz, C. E. Vandenberg Boundary Layer Survey (VBLS): Final report - results. Monterey, Calif: 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. Greenbelt, Md: Goddard Space Flight Center, 1987.

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9

P, Castro I., Rockliff N. J e 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. Oxford: Clarendon Press, 1994.

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10

Batchelor, G. K., Peter G. Baines, L. B. Freud, S. Leibovich e 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 classical baroclinic instability is given, and its relation to Rossby waves is explained. Modifications of quasi-geostrophic dynamics in the presence of coastal, topographic, and equatorial wave-guides are analysed. Emission of mountain Rossby waves by a flow over topography is demonstrated. The phenomena of Kelvin wave breaking, and of soliton formation by long equatorial and topographic Rossby waves due to nonlinear effects are explained.

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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 raw input data to a final conclusion but seems instead to send information both backward and forward so sensory input and learned information work together for a consensus analysis. Relative to body size, a bigger brain is a better brain. The most common cell types are variants of pyramidal cells with pronounced lateral interconnections.

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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, e 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. London: Royal Society, 1987.

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19

Blatt, Ari J., e 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 with space in France has taken shape across a range of media, from recent cinema, documentary filmmaking and photographic projects through to television drama and contemporary fiction, and examines what it reveals about the state of the nation in a post-colonial and post-industrial age. The impact of global flows of capital, trade and migration can be mapped through attention to the specificities of place and topography. Investigation of liminal locations, from seaboard cities and abandoned industrial sites to refugee camps and peasant smallholdings, interrogates the assertion of a national territory (and thereby, a national identity) through the figure of the hexagon, and highlights the fluidities, instabilities and lines of flight which render it increasingly unsettled.

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20

Michel, Christoph M., e Bin He. EEG Mapping and Source Imaging. Editado por Donald L. Schomer e 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 reconstruction has increased the precision of EEG source localization. Algorithms of functional connectivity applied to the source space allow determination of communication between large-scale brain networks in certain frequencies and identification of the directionality of this information flow and detection of crucial drivers in these networks. These methods have boosted the use of EEG as a functional neuroimaging method in experimental and clinical applications.

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21

Luca, Ioana, Yih-Chin Tai e 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 saturation of such instabilities exhibits typical secondary meso-vortex structures, and leads to intensification of the vortex. Special attention is paid to instabilities in laboratory flows in rotating cylindrical channels. Classification of these instabilities is given, and their nature, in terms of resonances between different wave modes, is established. Rigid-lid and free-surface configuration with topography are considered and compared with experiments.

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23

Fieberling Guyot moored array data: Office of Naval Research, Accelerated Research Initiative on Flow Over Abrupt Topography. Seattle, Wash: 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 e 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

Collings, David G., Kamel Mellahi e 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 the context of talent management, talent and performance, talent, teams and networks, managing talent flows, and contemporary issues in talent management. Each chapter is written by a leading international scholar in the area, and thus the volume represents the authoritative reference for anyone working in the area of talent management.

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27

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 major source of pollution aerosol emissions, but also a major receptor of large quantities of natural dust aerosols transported from the deserts of West Asia and the Middle East during the premonsoon and early monsoon season (April–June). The dust aerosols, combined with local emissions of light-absorbing aerosols, that is, black carbon (BC), organic carbon (OC), and mineral dust, can (a) provide additional powerful heating to the atmosphere and (b) allow more sunlight to penetrate the snow layer by darkening the snow surface. Both effects will lead to accelerated melting of snowpack and glaciers in the HKHG region, amplifying the greenhouse warming effect. In addition, these light-absorbing aerosols can interact with monsoon winds and precipitation, affecting extreme precipitation events in the HKHG, as well as weather variability and climate change over the TP and the greater Asian monsoon region.

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28

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 in the ancient highlands. In fact, the planet has been volcanically active for nearly all of its 4.5 Gyr history, and crater counts in the Northern Lowlands suggest that may have extended to within the last tens of millions of years. Our knowledge of the composition of the igneous rocks on Mars is informed by over 100 Martian meteorites and the results from landers and orbiters. These show dominantly tholeiitic basaltic compositions derived by melting of a relatively K, Fe-rich mantle compared to that of the Earth. However, recent meteorite and lander results reveal considerable diversity, including more silica-rich and alkaline igneous activity. These show the importance of a range of processes including crystal fractionation, partial melting, and possibly mantle metasomatism and crustal contamination of magmas. The figures and plots of compositional data from meteorites and landers show the range of compositions with comparisons to other planetary basalts (Earth, Moon, Venus). A notable feature of Martian igneous rocks is the apparent absence of amphibole. This is one of the clues that the Martian mantle had a very low water content when compared to that of Earth.The Martian crust, however, has undergone hydrothermal alteration, with impact as an important heat source. This is shown by SNC analyses of secondary minerals and Near Infra-Red analyses from orbit. The associated water may be endogenous.Our view of the Martian crust has changed since Viking landers touched down on the planet in 1976: from one almost entirely dominated by basaltic flows to one where much of the ancient highlands, particularly in ancient craters, is covered by km deep sedimentary deposits that record changing environmental conditions from ancient to recent Mars. The composition of these sediments—including, notably, the MSL Curiosity Rover results—reveal an ancient Mars where physical weathering of basaltic and fractionated igneous source material has dominated over extensive chemical weathering.

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