Other editions of book Our Weather

This work has been selected by scholars as being culturally important, and is part of the knowledge base of civilization as we know it. This work was reproduced from the original artifact, and remains as true to the original work as possible. Therefore, you will see the original copyright references, library stamps (as most of these works have been housed in our most important libraries around the world), and other notations in the work.This work is in the public domain in the United States of America, and possibly other nations. Within the United States, you may freely copy and distribute this work, as no entity (individual or corporate) has a copyright on the body of the work.As a reproduction of a historical artifact, this work may contain missing or blurred pages, poor pictures, errant marks, etc. Scholars believe, and we concur, that this work is important enough to be preserved, reproduced, and made generally available to the public. We appreciate your support of the preservation process, and thank you for being an important part of keeping this knowledge alive and relevant.

This is a reproduction of a book published before 1923. This book may have occasional imperfections such as missing or blurred pages, poor pictures, errant marks, etc. that were either part of the original artifact, or were introduced by the scanning process. We believe this work is culturally important, and despite the imperfections, have elected to bring it back into print as part of our continuing commitment to the preservation of printed works worldwide. We appreciate your understanding of the imperfections in the preservation process, and hope you enjoy this valuable book.

Excerpt from Our WeatherThe drains of our buildings and of the towns generally are constructed so that they may be able to carry 011 the greatest rainfalls likely to occur, in order that floods may be avoided.About the PublisherForgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.comThis 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.

This book was originally published prior to 1923, and represents a reproduction of an important historical work, maintaining the same format as the original work. While some publishers have opted to apply OCR (optical character recognition) technology to the process, we believe this leads to sub-optimal results (frequent typographical errors, strange characters and confusing formatting) and does not adequately preserve the historical character of the original artifact. We believe this work is culturally important in its original archival form. While we strive to adequately clean and digitally enhance the original work, there are occasionally instances where imperfections such as blurred or missing pages, poor pictures or errant marks may have been introduced due to either the quality of the original work or the scanning process itself. Despite these occasional imperfections, we have brought it back into print as part of our ongoing global book preservation commitment, providing customers with access to the best possible historical reprints. We appreciate your understanding of these occasional imperfections, and sincerely hope you enjoy seeing the book in a format as close as possible to that intended by the original publisher.

Excerpt from Our WeatherThe drains of our buildings and of the towns generally are constructed so that they may be able to carry 011 the greatest rainfalls likely to occur, in order that floods may be avoided.About the PublisherForgotten Books publishes hundreds of thousands of rare and classic books. Find more at www.forgottenbooks.comThis 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.

This historic book may have numerous typos and missing text. Purchasers can download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1912 Excerpt: ...some time. It is also lighter in the woods than in the open plain, and lighter in a gentle than in a strong wind. Naturally also the lower layers having to support the upper become more dense. Indeed, if enough snow accumulates, the lower layers soon approach the consistency of ordinary ice. Though most people consider snow rather a nuisance after its first beauty has disappeared, yet it is often welcomed by the farmers. Snow is a non-conductor of heat, a fact which the dwellers in Arctic regions utilize when they build houses of it. When the earth is coated with snow, it prevents frost from penetrating into the ground and injuring the plants. Moreover, if the snow melts slowly, the greater Fig. 34. Models of hailstones seven inches in circumference. part of the water soaks into the soil and replenishes the underground springs, so making provision for dry weather, whereas when rain falls a considerable portion of the water often runs off into the drains and ditches. Hail.--When rain is frozen, hail is formed. This frequently happens in thunderstorms. The hailstones are usually about the size of a pea, but there are many authentic records of hailstones as large as eggs having fallen in this country. At Richmond in Yorkshire, on July 8, 1893, hailstones six to seven inches in circumference fell. If these large hailstones are cut in halves, it is usually found that they consist of alternate layers or coatings of clear and opaque ice. Fig 34 shows models of five hailstones, seven inches in circumference, which fell at Montereau, France, on August 15, 1888. A penny (l-2 inch diameter) is placed by the side of the upper right-hand model. When large hailstones fall, they are often accompanied by sudden squalls of wind, and so destroy large quantities of glass, and...