By James R. Holton
During the earlier decade, the technology of dynamic meteorology has endured its speedy enhance. The scope of dynamic meteorology has broadened significantly. a lot of the cloth is predicated on a two-term direction 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 results posed for international swap. the hot variation has additional a spouse site with MATLAB routines and up-to-date remedies of numerous key topics.
- Provides transparent actual factors of key dynamical principles
- Contains a wealth of illustrations to clarify textual content and equations, plus end-of-chapter problems
- Holton is without doubt one of the best gurus in modern meteorology, and renowned for his transparent writing style
- Instructor's guide on hand to adopters
NEW during this EDITION
- A spouse site with MATLAB® routines and demonstrations
- Updated remedies on weather dynamics, tropical meteorology, heart surroundings dynamics, and numerical prediction
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Extra resources for An Introduction to Dynamic Meteorology, Fifth Edition
6. Two balls 4 cm in diameter are placed 100 m apart on a frictionless horizontal plane at 43° N. If the balls are impulsively propelled directly at each other with equal speeds, at what speed must they travel so that they just miss each other? 7. A locomotive of mass 2 × 105kg travels 50 ms−1 along a straight horizontal track at 43° N. What lateral force is exerted on the rails? Compare the magnitudes of the upward reaction force exerted by the rails for cases where the locomotive is traveling eastward and westward, respectively.
Give the solution for the position of the particle as a function of time. 12. Calculate the 1000 to 500hPa thickness for isothermal conditions with temperatures of 273 and 250K, respectively. 13. Isolines of 1000 to 500hPa thickness are drawn on a weather map using a contour interval of 60 m. What is the corresponding layer mean temperature interval? 14. Show that a homogeneous atmosphere (density independent of height) has a finite height that depends only on the temperature at the lower boundary.
1 SI Base Units Property Name Symbol Length Meter (meter) m Mass Kilogram kg Time Second s Temperature Kelvin K A number of important derived units have special names and symbols. 2. 3 lists the symbols frequently used in this book for some of the basic physical quantities. Note that the full three-dimensional velocity vector, U, is related to the horizontal velocity vector, V, by U = (V,w) and U = (V, ω) in height and pressure vertical coordinates, respectively. We shall use the term “zonal” to refer to the East–West direction and “meridional” to refer to the North–South direction.