11 edition of An Introduction to Dynamic Meteorology, Volume 88, Fourth Edition (International Geophysics) found in the catalog.
March 31, 2004 by Academic Press .
Written in English
|The Physical Object|
|Number of Pages||535|
Extensive numerical and qualitative exercises help students apply basic physical principles to atmospheric problems. Buettner, D. The lead custodian of the site seems to be C. Time is expressed in terms of the simultaneous occurrence of an arbitrary familiar event, for instance, the rotation of the earth about its axis or the characteristic period of an electromagnetic wave emitted by an atom.
About the Author: James R. These define the position of the event in terms of its distance from an arbitrary reference point; the distance may be measured along mutually perpendicular straight lines Cartesian coordinates or along any of a number of lines associated with other coordinate systems. Includes many satellite-derived products. Parts of the manuscript have profited from the critical comments of Professors E. It also should be of useful interest to students of other branches of geophysics and to students of physics who want to extend their horizons beyond the laboratory.
The paper and updated data tables can be found here. Mason, H. The final two chapters on energy transfer and signal phenomena have been rewritten and extended, and other chapters have been revised in accordance with insights provided by recent research. Gordon Little, and George A.
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About the Author: James R. Some race series have restricted data logging to decrease the teama's running budgets. Read: Atmospheric Science by John M.
This revised edition features updated treatments on climate dynamics, tropical meteorology, middle atmosphere dynamics, and numerical prediction.
It is an example of the inverse square relation which makes its appearance over and over in fundamental principles and applications. Deeper understanding of this problem requires consideration of complex energy transformations which will be discussed at a later stage; we shall then have occasion to refer to this problem of the vertical distribution of density in the atmosphere.
There are also biographical footnotes summarizing the work of key scientists, along with a student companion website that hosts climate data; answers to quantitative exercises; full solutions to selected exercises; skew-T log p chart; related links, appendices; and more.
Kim, J. We are indebted for numerous suggestions to our colleagues who have taken their turns at teaching the introductory courses in Atmospheric Physics: Professors F. This book is recommended for senior and graduate students in meteorology and atmospheric science, as well as atmospheric scientists desiring a broad overview of dynamical meteorology.
Atmospheric motions, which are part of atmospheric physics and which logically follow discussion of physical properties, have not been included because they require more advanced mathematical methods than those used here.
Whether measuring the performance of a Formula One racecar or that of a road-legal street car on the local drag strip the dynamics of vehicles and their drivers remain the same. For in one published work Newton stated both the law of universal gravitation and the laws of motion; together these laws provided the base for all later developments in mechanics until the twentieth century.
The objective of laboratory physics is, by isolating the relevant variables, to reveal the fundamental properties of matter; whereas the objective of atmospheric physics, or of any observational science, is to understand those phenomena that are characteristic of the whole system. The paper and updated data tables can be found here.
For these reasons, we have with some reluctance omitted ionospheric and magnetospheric physics from this revised edition. Compromise has been necessary in a few cases, particularly in Chapter VII, where full development would have required extended discussion of advanced and specialized material.
It is also a good place to look for ice core and marine sediment core data. Viewed from a fixed point in space at a distance of several earth radii, our planet appears as a smooth spheroid strongly illuminated by a very distant sun.
The picture is formed by computer from 13 successive passes of the satellite at the times indicated along the equator by courtesy of National Environmental Satellite Service, National Oceanic and Atmospheric Administration.
Therefore, for applications in which mass is the relevant factor, the atmosphere properly is considered a thin shell; for other applications the shell concept is inadequate. Read more. These acclaimed applets, designed by Tom Whittaker and co-author Steven Ackerman, are divided into two types, "Observational Learning" applets deal with interpreting satellite imagery and "Atmospheric Explorations" extend the book's treatment of key topics, such as weather map analysis and numerical weather models.
Notice that the forces referred to in discussing the second law and the law of universal gravitation are forces acting on the body under consideration. Holton, Conway B. McDonald, B.This revised text presents a cogent explanation of the fundamentals of meteorology, and explains storm dynamics for weather-oriented meteorologists.
It discusses climate dynamics and the implications posed for global change. The Fourth Edition features a CD-ROM with MATLABR exercises and updated treatments of several key topics.
In this volume James R. Holton () An Introduction to Dynamic Meteorology, Academic Press, International Geophysics Series Volume 88, Fourth Edition, p., ISBN Preface.
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Holton. May 05, · Atmospheric Science, Second Edition: An Introductory Survey (International Geophysics) An Introduction to Dynamic Meteorology, Fourth Edition (The International Geophysics Series, Vol 88) Global Physical Climatology, Volume 56 (International Geophysics) A Climate Modelling Primer Planetary Atmospheres Introduction to Atmospheric Chemistry.