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Books on the topic 'Physical boundary conditions'

Author: Grafiati

Published: 24 July 2022

Last updated: 8 August 2022

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1

Syed, Hasnain H. Electromagnetic scattering by coated convex surfaces and wedges simulated by approximate boundary conditions. Ann Arbor, Mich: University of Michigan, Radiation Laboratory, Dept. of Electrical Engineering and Computer Science, 1992.

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2

The scaling limit of the correlation of holes on the triangular lattice with periodic boundary conditions. Providence, R.I: American Mathematical Society, 2009.

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3

Peter, Schloerb F., University of Massachusetts at Amherst. Dept. of Physics and Astronomy., and United States. National Aeronautics and Space Administration., eds. Boundary conditions for the paleoenvironment: Chemical and physical processes in the pre-solar nebula. [Amherst, Mass.]: Dept. of Physics and Astronomy, University of Massachusetts, 1985.

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4

Peter, Schloerb F., and United States. National Aeronautics and Space Administration., eds. Boundary conditions for the paleoenvironment: Chemical and physical processes in the pre-solar nebula : semi-annual status report no. 21, February 16, 1993 - August 15, 1993. Amherst, MA: Five College Radio Astronomy and Observatory, University of Massachusetts, 1993.

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5

Peter, Schoerb F., and United States. National Aeronautics and Space Administration, eds. Boundary conditions for the paleoenvironment: Chemical and physical processes in the pre-solar nebula : semi-annual status report no. 7, February 16, 1986 - August 15, 1986. [Amherst, Mass.]: Dept. of Physics and Astronomy, University of Massachusetts, 1986.

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6

Dervishi, Sokol. Sky Radiance and Luminance Models: The Boundary Conditions. Nova Science Publishers, Incorporated, 2019.

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7

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, first in the whole space, where dispersion effects are considered. The case where the domain has periodic boundary conditions is then analyzed, and finally rotating Navier-Stokes equations between two plates are studied, both in the case of periodic horizontal coordinated and those in R2. In Part IV, the stability of Ekman boundary layers and boundary layer effects in magnetohydrodynamics and quasigeostrophic equations are discussed. The boundary layers which appear near vertical walls are presented and formally linked with the classical Prandlt equations. Finally spherical layers are introduced, whose study is completely open.

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8

J, Luebbers Raymond, Kunz Karl S, and United States. National Aeronautics and Space Administration., eds. Wideband finite difference time domain implementation of surface impedance boundary conditions for good conductors. [Washington, DC: National Aeronautics and Space Administration, 1991.

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9

Whence the boundary conditions in modern continuum physics?: Convegno internazionale, (Roma, 14-16 ottobre 2002). Roma: Accademia Nazionale dei Lincei, 2004.

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10

Guenther, B. D. Modern Optics Simplified. Oxford University Press, 2019. http://dx.doi.org/10.1093/oso/9780198842859.001.0001.

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This textbook is designed for use in a standard physics course on optics at the sophomore level. The book is an attempt to reduce the complexity of coverage found in Modem Optics to allow a student with only elementary calculus to learn the principles of optics and the modern Fourier theory of diffraction and imaging. Examples based on real optics engineering problems are contained in each chapter. Topics covered include aberrations with experimental examples, correction of chromatic aberration, explanation of coherence and the use of interference theory to design an antireflection coating, Fourier transform optics and its application to diffraction and imaging, use of gaussian wave theory, and fiber optics will make the text of interest as a textbook in Electrical and bioengineering as well as Physics. Students who take this course should have completed an introductory physics course and math courses through calculus Need for experience with differential equations is avoided and extensive use of vector theory is avoided by using a one dimensional theory of optics as often as possible. Maxwell’s equations are introduced to determine the properties of a light wave and the boundary conditions are introduced to characterize reflection and refraction. Most discussion is limited to reflection. The book provides an introduction to Fourier transforms. Many pictures, figures, diagrams are used to provide readers a good physical insight of Optics. There are some more difficult topics that could be skipped and they are indicated by boundaries in the text.

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11

Triana, María del Carmen, Tiffany M. Trzebiatowski, and Seo-Young Byun. Individual Outcomes of Discrimination in Workplaces. Edited by Adrienne J. Colella and Eden B. King. Oxford University Press, 2015. http://dx.doi.org/10.1093/oxfordhb/9780199363643.013.23.

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This chapter reviews the recent literature on the outcomes of workplace discrimination against individuals. The chapter describes how discrimination affects individuals by reviewing theories related to outcomes of discrimination (e.g., social categorization, attributional ambiguity, and minority stress theories). From there, the review covers meta-analyses, empirical studies conducted between 2012 and 2014, and outcomes of discrimination (e.g., job attitudes, psychological outcomes, physical outcomes, and work-related outcomes). There is consistent support for an overall negative effect of discrimination on various individual-level outcomes. Recent studies are advancing our knowledge of individual-level consequences of discrimination by incorporating underrepresented samples, examining discrimination types other than race and sex, considering the nuances of boundary conditions, and connecting research streams from multiple areas (e.g., turnover, incivility). The chapter concludes with suggestions for future research directions on individual outcomes of workplace discrimination.

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12

Mann, Peter. Wave Mechanics & Elements of Mathematical Physics. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198822370.003.0005.

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This chapter presents an in-depth look at classical wave mechanics and mathematical physics, containing key examples directly relevant to molecular physics. The separation of variables is used to construct the Helmholtz equation from the one-dimensional wave equation before considering the three-dimensional wave equation. From this, equations for the temporal, radial, azimuth and angular components are developed and solutions using the Bessel equations and Legendre polynomials are found. Boundary conditions are explained and the Rayleigh plane wave expansion as the general solution to the Helmholtz equation is reconstructed. Both the Hermite equation and the Legendre equation are derived using the series solution method, and the Laplace equation is discussed.

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13

Mann, Peter. Vector Calculus. Oxford University Press, 2018. http://dx.doi.org/10.1093/oso/9780198822370.003.0034.

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This chapter gives a non-technical overview of differential equations from across mathematical physics, with particular attention to those used in the book. It is a common trend in physics and nature, or perhaps just the way numbers and calculus come together, that, to describe the evolution of things, most theories use a differential equation of low order. This chapter is useful for those with no prior knowledge of the differential equations and explains the concepts required for a basic exposition of classical mechanics. It discusses separable differential equations, boundary conditions and initial value problems, as well as particular solutions, complete solutions, series solutions and general solutions. It also discusses the Cauchy–Lipschitz theorem, flow and the Fourier method, as well as first integrals, complete integrals and integral curves.

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14

North, Jill. Time in Thermodynamics. Edited by Craig Callender. Oxford University Press, 2011. http://dx.doi.org/10.1093/oxfordhb/9780199298204.003.0011.

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It is often claimed, or hoped, that some temporal asymmetries are explained by the thermodynamic asymmetry in time. Thermodynamics, the macroscopic physics of pressure, temperature, volume, and so on, describes many temporally asymmetric processes. Heat flows spontaneously from hot objects to cold objects (in closed systems), never the reverse. More generally, systems spontaneously move from non-equilibrium states to equilibrium states, never the reverse. Delving into the foundations of statistical mechanics, this chapter reviews the many open questions in that field as they relate to temporal asymmetry. Taking a stand on many of them, it tackles questions about the nature of probabilities, the role of boundary conditions, and even the nature and scope of statistical mechanics.

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15

Douglas, Darling, Radhakrishnan Krishnan, and United States. National Aeronautics and Space Administration., eds. Review of combustion-acoustic instabilities. [Washington, D.C.]: National Aeronautics and Space Administration, 1995.

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16

Douglas, Darling, Radhakrishnan Krishnan, and United States. National Aeronautics and Space Administration., eds. Review of combustion-acoustic instabilities. [Washington, D.C.]: National Aeronautics and Space Administration, 1995.

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17

Douglas, Darling, Radhakrishnan Krishnan, and United States. National Aeronautics and Space Administration., eds. Review of combustion-acoustic instabilities. [Washington, D.C.]: National Aeronautics and Space Administration, 1995.

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18

Douglas, Darling, Radhakrishnan Krishnan, and United States. National Aeronautics and Space Administration., eds. Review of combustion-acoustic instabilities. [Washington, D.C.]: National Aeronautics and Space Administration, 1995.

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19

Wang, Bin. Intraseasonal Modulation of the Indian Summer Monsoon. Oxford University Press, 2018. http://dx.doi.org/10.1093/acrefore/9780190228620.013.616.

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The strongest Indian summer monsoon (ISM) on the planet features prolonged clustered spells of wet and dry conditions often lasting for two to three weeks, known as active and break monsoons. The active and break monsoons are attributed to a quasi-periodic intraseasonal oscillation (ISO), which is an extremely important form of the ISM variability bridging weather and climate variation. The ISO over India is part of the ISO in global tropics. The latter is one of the most important meteorological phenomena discovered during the 20th century (Madden & Julian, 1971, 1972). The extreme dry and wet events are regulated by the boreal summer ISO (BSISO). The BSISO over Indian monsoon region consists of northward propagating 30–60 day and westward propagating 10–20 day modes. The “clustering” of synoptic activity was separately modulated by both the 30–60 day and 10–20 day BSISO modes in approximately equal amounts. The clustering is particularly strong when the enhancement effect from both modes acts in concert. The northward propagation of BSISO is primarily originated from the easterly vertical shear (increasing easterly winds with height) of the monsoon flows, which by interacting with the BSISO convective system can generate boundary layer convergence to the north of the convective system that promotes its northward movement. The BSISO-ocean interaction through wind-evaporation feedback and cloud-radiation feedback can also contribute to the northward propagation of BSISO from the equator. The 10–20 day oscillation is primarily produced by convectively coupled Rossby waves modified by the monsoon mean flows. Using coupled general circulation models (GCMs) for ISO prediction is an important advance in subseasonal forecasts. The major modes of ISO over Indian monsoon region are potentially predictable up to 40–45 days as estimated by multiple GCM ensemble hindcast experiments. The current dynamical models’ prediction skills for the large initial amplitude cases are approximately 20–25 days, but the prediction of developing BSISO disturbance is much more difficult than the prediction of the mature BSISO disturbances. This article provides a synthesis of our current knowledge on the observed spatial and temporal structure of the ISO over India and the important physical processes through which the BSISO regulates the ISM active-break cycles and severe weather events. Our present capability and shortcomings in simulating and predicting the monsoon ISO and outstanding issues are also discussed.

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