An Introduction to Dynamic Meteorology, Fifth Edition by James R. Holton PDF

By James R. Holton

ISBN-10: 0123848660

ISBN-13: 9780123848666

During the previous decade, the technology of dynamic meteorology has persisted its speedy enhance. The scope of dynamic meteorology has broadened significantly. a lot of the fabric relies on a two-term path for seniors majoring in atmospheric sciences.

This publication offers a cogent clarification of the basics of meteorology and explains typhoon dynamics for weather-oriented meteorologists. It discusses weather dynamics and the consequences posed for worldwide swap. the recent version has further a better half web site with MATLAB workouts and up to date remedies of a number of key topics.

  • Provides transparent actual reasons of key dynamical principles
  • Contains a wealth of illustrations to explain textual content and equations, plus end-of-chapter problems
  • Holton is among the major specialists in modern meteorology, and renowned for his transparent writing style
  • Instructor's handbook to be had to adopters

NEW during this EDITION

  • A significant other site with MATLAB® routines and demonstrations
  • Updated remedies on weather dynamics, tropical meteorology, heart surroundings dynamics, and numerical prediction
  • Show description

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Additional resources for An Introduction to Dynamic Meteorology, Fifth Edition

Example text

24) Thus, an object displaced horizontally from its equilibrium position on the surface of Earth under the influence of the force of gravity will oscillate about its equilibrium position with a period that depends on latitude and is equal to one sidereal day at 30° latitude and 1/2 sidereal day at the pole. Constant angular momentum oscillations (often referred to as “inertial oscillations”) are commonly observed in the oceans, but are apparently not of importance in the atmosphere. 4 Structure of the Static Atmosphere The thermodynamic state of the atmosphere at any point is determined by the values of pressure, temperature, and density (or specific volume) at that point.

Gravity, g, is the vector sum of g* and the centrifugal force and is perpendicular to the level surface of Earth, which approximates an oblate spheroid. Viewed from a frame of reference rotating with Earth, however, a geopotential surface is everywhere normal to the sum of the true force of gravity, g*, and the centrifugal force Ω2R (which is just the reaction force of the centripetal acceleration). A geopotential surface is thus experienced as a level surface by an object at rest on rotating Earth.

By varying the run time, see if you can determine how long it takes for the particle to make a full circuit in each case, and compare this to the time given in Eq. 24) for ϕ = 60°. 2. 1, compare the magnitudes of the lateral deflection for ballistic missiles fired eastward and westward at 43° latitude. Each missile is launched at a velocity of 1000 ms−1 and travels 1000km. Explain your results. Can the curvature term be neglected in these cases? 3. This exercise examines the strange behavior of constant angular momentum trajectories near the equator.

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An Introduction to Dynamic Meteorology, Fifth Edition by James R. Holton


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