By Robert G. Fleagle and Joost A. Businger (Eds.)

This publication is addressed to those that desire to comprehend the connection among atmospheric phenomena and the character of subject as expressed within the ideas of physics. The attention-grabbing atmospheric phenomena are greater than purposes of gravitation, of thermodynamics, of hydrodynamics, or of electrodynamics; and mastery of the result of managed scan and of the similar idea by myself doesn't suggest an knowing of atmospheric phenomena. This contrast arises as the volume and the complexity of the ambience allow results and interactions which are fullyyt negligible within the laboratory or are intentionally excluded from it. the target of laboratory physics is, through separating the proper variables, to bare the elemental houses of subject; while the target of atmospheric physics, or of any observational technology, is to appreciate these phenomena which are attribute of the full procedure. For those purposes the exposition of atmospheric physics calls for huge extensions of classical physics. It additionally calls for that realizing be in line with a coherent "way of seeing" the ensemble of atmospheric phenomena. merely then is knowing prone to stimulate nonetheless extra normal insights.

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5. Find the angle between g* and g at the surface of the earth as a function of latitude. What is its maximum numerical value, and at what latitude does it occur? 6. 80 N kg- 1 at latitude 30". 7. Find the periods of revolution for satellites in circular orbits at heights of 200 and 600 km above the earth. What are the apparent periods as seen from a point on the earth if the satellites move from west to east around the equator? 8. 3 days at a distance of 384,400 km from the earth. Compare the result with Problem 6.

And v y . THE VELOCITY DISTRIBUTION OF MOLECULES 37 The molecular distribution function [Eq. 13)] for the two velocity components obtained there results 1 ¢'(v x ) ~ ¢'(v y) -~~ Vx ¢(v x ) vy ¢(v y) where the prime denotes the derivative. The left-hand side of this equation is independent of v y and the right-hand side is independent of VX" This is only possible when each side is equal to the same constant, say - A. 14c) The constant of integration is found by substituting Eqs. 14) into 38 II. 13), which yields A = ¢(O) The value of ¢(O) is found by substituting one of Eqs.

Ocean tidal currents and the height of the tide are influenced strongly 21 LIST OF SYMBOLS by the boundaries of the ocean basins, and there are therefore large local differences in the ocean tide. The tide generating force acting on the elastic body of the earth produces earth tides of which we are not usually aware, but which can be detected by sensitive instruments. To detect the atmospheric tide, records of sea level atmospheric pressure must be averaged over long periods in order to eliminate the large pressure changes associated with weather and to separate the lunar and solar effects.

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