Read Rainfall of the United States: With Annual, Seasonal, and Other Charts (Classic Reprint)

Rainfall of the United States: With Annual, Seasonal, and Other Charts (Classic Reprint)

Alfred Judson Henry

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Description:Excerpt from Rainfall of the United States: With Annual, Seasonal, and Other Charts It is quite probable that rain falls in the United States at one point or another every day of the year. On very rare occasions the observers of the Weather Bureau report no precipitation at a given hour, but it should be remembered that their range of vision can cover at the utmost less than one-hundredth part of the whole area. The theories of rainfall given in the books of twenty or thirty years ago are not now wholly accepted. There is one very simple principle, however, upon which no disagreement exists, viz, that in order to produce abundant rain the temperature of air must he suddenly cooled below the dew-point. When the air is thus cooled, a portion of the water vapor which is always present within it is changed to the liquid state, and that which formerly existed as a gas or vapor now becomes visible in the form of minute particles of fog or mist. The particles thus formed may oat away with the wind or they may increase in size, coalesce, and fall to the ground of their own weight. Whether the condensation of vapor thus outlined results simply in cloud, or whether rain falls, depends on the magnitude of the temperature changes that take place in the air mass whose vapor is being condensed. A rise in temperature is inimical to further condensation; a fall is favorable to precipitation. The precise manner in which air is cooled sufficiently to produce rain, whether by contact or by mixing, is not clearly apprehended. Cooling by expansion as air ascends is one of the most effective causes of rainfall. The ascensional movement of air is brought about in several ways, chief of which are: (1) The air may be forced up the side of a mountain into a region of dimin ished pressure and lower temperature, as happens whenever a mountain range runs in a direction at right angles to the prevailing winds; (2) in the warm season, the lower layers of the atmosphere under the effect of solar radiation, and probably other causes, frequently reach a state of unstable equilibrium, thus inducing ascensional currents - summer thunderstorms are largely a result of this process; (3) last, and doubtless most important of all, is the circulation of air in cyclonic storms, viz, a radial in ow from all sides and an ascensional movement in the center. A very large percentage of the rain of the United States is precipitated in connection with the passage of storms of the latter class. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works."We have made it easy for you to find a PDF Ebooks without any digging. And by having access to our ebooks online or by storing it on your computer, you have convenient answers with Rainfall of the United States: With Annual, Seasonal, and Other Charts (Classic Reprint). To get started finding Rainfall of the United States: With Annual, Seasonal, and Other Charts (Classic Reprint), you are right to find our website which has a comprehensive collection of manuals listed.
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ISBN: 1333171013

Description: Excerpt from Rainfall of the United States: With Annual, Seasonal, and Other Charts It is quite probable that rain falls in the United States at one point or another every day of the year. On very rare occasions the observers of the Weather Bureau report no precipitation at a given hour, but it should be remembered that their range of vision can cover at the utmost less than one-hundredth part of the whole area. The theories of rainfall given in the books of twenty or thirty years ago are not now wholly accepted. There is one very simple principle, however, upon which no disagreement exists, viz, that in order to produce abundant rain the temperature of air must he suddenly cooled below the dew-point. When the air is thus cooled, a portion of the water vapor which is always present within it is changed to the liquid state, and that which formerly existed as a gas or vapor now becomes visible in the form of minute particles of fog or mist. The particles thus formed may oat away with the wind or they may increase in size, coalesce, and fall to the ground of their own weight. Whether the condensation of vapor thus outlined results simply in cloud, or whether rain falls, depends on the magnitude of the temperature changes that take place in the air mass whose vapor is being condensed. A rise in temperature is inimical to further condensation; a fall is favorable to precipitation. The precise manner in which air is cooled sufficiently to produce rain, whether by contact or by mixing, is not clearly apprehended. Cooling by expansion as air ascends is one of the most effective causes of rainfall. The ascensional movement of air is brought about in several ways, chief of which are: (1) The air may be forced up the side of a mountain into a region of dimin ished pressure and lower temperature, as happens whenever a mountain range runs in a direction at right angles to the prevailing winds; (2) in the warm season, the lower layers of the atmosphere under the effect of solar radiation, and probably other causes, frequently reach a state of unstable equilibrium, thus inducing ascensional currents - summer thunderstorms are largely a result of this process; (3) last, and doubtless most important of all, is the circulation of air in cyclonic storms, viz, a radial in ow from all sides and an ascensional movement in the center. A very large percentage of the rain of the United States is precipitated in connection with the passage of storms of the latter class. About the Publisher Forgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.com This book is a reproduction of an important historical work. Forgotten Books uses state-of-the-art technology to digitally reconstruct the work, preserving the original format whilst repairing imperfections present in the aged copy. In rare cases, an imperfection in the original, such as a blemish or missing page, may be replicated in our edition. We do, however, repair the vast majority of imperfections successfully; any imperfections that remain are intentionally left to preserve the state of such historical works."We have made it easy for you to find a PDF Ebooks without any digging. And by having access to our ebooks online or by storing it on your computer, you have convenient answers with Rainfall of the United States: With Annual, Seasonal, and Other Charts (Classic Reprint). To get started finding Rainfall of the United States: With Annual, Seasonal, and Other Charts (Classic Reprint), you are right to find our website which has a comprehensive collection of manuals listed.
Our library is the biggest of these that have literally hundreds of thousands of different products represented.

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Rainfall of the United States: With Annual, Seasonal, and Other Charts (Classic Reprint)

Rainfall of the United States: With Annual, Seasonal, and Other Charts (Classic Reprint)

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