A Manual of the Barometer, Containing An Explanation of the Construction And Method of Using the Mercurial Barometer, With Appropriate Tables for Corrections for Temperature, And Rules for Obtaining the Dew-Point And the Heights of Mountains, to Which Are
The book A Manual of the Barometer, Containing An Explanation of the Construction And Method of Using the Mercurial Barometer, With Appropriate Tables for Corrections for Temperature, And Rules for Obtaining the Dew-Point And the Heights of Mountains, to Which Are was written by author Belville, John Henry Here you can read free online of A Manual of the Barometer, Containing An Explanation of the Construction And Method of Using the Mercurial Barometer, With Appropriate Tables for Corrections for Temperature, And Rules for Obtaining the Dew-Point And the Heights of Mountains, to Which Are book, rate and share your impressions in comments. If you don't know what to write, just answer the question: Why is A Manual of the Barometer, Containing An Explanation of the Construction And Method of Using the Mercurial Barometer, With Appropriate Tables for Corrections for Temperature, And Rules for Obtaining the Dew-Point And the Heights of Mountains, to Which Are a good or bad book?
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...■•■ Mean annual depth ... 24-781 31 From the above synopsis, it appears that the greatest average quantity of rain falls in October and the least in February. The heaviest rains, or those which yield the greatest quantity in the gauge, come down in the summer and early autumnal months. In the summer an inch and a half will sometimes fall in less than an hour in short but impetuous torrents; in the autumathe same quan- tity will occupy many hours in" falling. In winter the number of wet days ...exceeds that of the summer period ; the average fall of a winter's rain is seldom more than yu of ^.n inch an hour. The amount of snow for the thirty-four years is in- cluded in the above Table. Snow yields yu of water to 1 inch fall in depth ; or a fall of snow of 10 inches in depth on the level would be equal to 1 inch of rain. On the Vapour-Point. The dew- or vapour-point is to many a subject in- volved in so much mystery, and hence apparently of so little importance in meteorological investigations, that very little attention has been practically bestowed upon the registration of connected series of observations; when it is viewed as a means of unfolding the state of the atmosphere with regard to its moisture and dryness, and therefore, as a means of assisting not only the flori- culturist in the preservation of his exotics, but also each individual of the community in the protection of himself from the influences of a variable and humid climate, it will assume an interest which will overcome any sup- posed difficulty in its comprehension.
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