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Excerpt from Bulletin of the Mount Weather Observatory, 1911, Vol. 3 Bigelow, Frank H., studies on the general circulation of the atmosphere 151; 229 Bjerknes Prof. V., Computation of solenoids and energy in the gust of Oct. 4. 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.
Excerpt from Bulletin of the Mount Weather Observatory, 1910, Vol. 2 Solar Radiation Research. Upper Air Research. Research Observer. Assistant Research Observer. Assistant Research Observer. Assistant Research Observer. Assistant Research Observer. Assistant Research Observer. 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.
Excerpt from Bulletin of the Mount Weather Observatory, Vol. 1 The meteorological service of the United States Government is com prised of many stations distributed over a broad area, but until the founding of Mount Weather no station was specifically devoted to research work. The position that the Weather Bureau now occupies in the United States and before the world justifies research into the fundamental principles that underlie meteorological science. Such research will give information and direction to the two hundred stations that are taking observations and making forecasts. In the application of known principles to the art of weather fore casting the Weather Service of the United States is doubtless in the forefront; on the other hand, it has not done its full part in the way of discovering new principles; therefore, it was high time that such an institution as Mount Weather be founded so that the scientists of the Weather Bureau might have placed at their disposal facilities for research that will enable them to better understand the influences that control weather conditions. 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.
This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1911 edition. Excerpt: ...systems of temperature, pressure, density, and wind vectors that will conform to the one that is observed to exist in any region. (To be continued.) (VI) RECENT PUBLICATIONS RELATING TO AEROLOGY. C. Fitzhuqh Talman, Librarian, U. S. Weather Bureau. Assmann Richard. Ein hoher Drachenaufstieg in Lindenberg am 4. April, 1910. Wetter, Berlin, April, 1910, 27: 89-91. Gives altitudes of several high kiteflights at Lindenbcrg and Mount Weather. Batavia. Royal magnetic and meteorological observatory. Report on cloud observations at Batavia during the international cloud-year, 1896-1897. Utrecht. 1910. 32 p. f. (Appendix 2 to volume 30 of the observations.) Berson, Arthur. Bericht uber die aerologische Expedition... nach Ostafrika im Jahre 1908, erstattet von ihrem Leiter Arthur Berson. Braunschweig, 1910. 119 p. f. (K. Preussisches aeronaut. Observatorium bei Lindenberg.) Blue Hill meteorological observatory, 1885-1910. Boston, 1910. 3 p. 8. (Reprinted from Tech. Rev., 1910, vol. 2, no. 2.) Boyer, Jaques. Eiffel's recent experiments on the resistance of the air. Scientific American, New York, May 28, 1910, 102: 437-8. Boyer, Jaques. Nouvelles recherches sur la resistance de l'air. Cosmos, Paris, 1910. 59: 685-8. Brockett, Paul. Bibliography of aeronautics. Washington, 1910. xiv, 940 p. 80. (Smithsonian miscellaneous collections, v. 55.) Dines, W. H., & Pring, J. H. Meteorological observations during the passage of the earth through the tail of Halley's comet. Nature, London, June 9, 1910, 83: 427. Upper air observations, including measurements of ozone. Everdingen, E. van. Ist die Luft auf den Bergen kalter als die Atmosphare in gleicher Hohe? Meteorol. Zeitschr., Mai, 1910, 27: 215-17. Gockel, Albert. Luftelektrische...
Excerpt from Bulletin of the Mount Weather Observatory, 1912, Vol. 4 There are five barometric highs on the oceans, as indicated by figure 1, that remain substantially fixed in position throughout the year though of varying intensity. No of these are approximately 35 north of the Equator and three about 32 south of it. Two occur in the Pacific Ocean, one just west of southern California, the other near the coast of Chile; two in the Atlantic Ocean, near Morocco and southern Africa, respectively; and one in the Indian Ocean about half way between southern Africa and Australia. 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.
Excerpt from Bulletin of the Mount Weather Observatory, 1913, Vol. 6 Old lake beaches, glacial moraines, and various other geological records give indisputable evidence of numerous climatic changes. It appears too that these changes were irregular in their times oi occur rence and irregular also in their intensity and duration. Many seem to have been mild and relatively fleeting, while a few were so profound and lasting as even to bring on ice ages and to cover extensive areas of the earth with glacial sheets, or, on the other hand, to melt these sheets away and to establish for long periods warm and genial climates over much the greater portion of the earth. When this series of climatic changes began there is no sure means of knowing, for the records, especially those of glacial origin, grow gradually fainter and more scanty with increase of geological age, and it is probable therefore that the effects of many of the earlier changes have long since been completely obliterated. But, however this may be, it is well nigh certain that from the time of the earliest known of these changes down to the very present the series has been irregularly continuous, and the end, one might reasonably assume. Is not yet. Change after change of climate in an almost endless succession, and even additional ice ages, presumably are still to be experienced, though, except small and fleeting changes to be noted below, when they shall begin, how intense they may be or how long they shall last no one can form the slightest idea. 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.
Excerpt from Bulletin of the Mount Weather Observatory, Vol. 2 I. The region of terrestrial disturbance, extending from the ground to an elevation of roughly meters above its surface, in which the temperature gradient usually is very irregular and often locally reversed. This is also the principal region of cloud formation and of precipitation. 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.
This historic book may have numerous typos and missing text. Purchasers can usually download a free scanned copy of the original book (without typos) from the publisher. Not indexed. Not illustrated. 1911 edition. Excerpt: ...par. 2). It does show a decidedly greater drop in temperature, from the temperature of the lower air strata, in the summer than in the winter months. If, instead of the grouping used in Table IX, the 46 observations be grouped into (1) those made within areas of high pressure and (2) those made within areas of low pressure, the altitude of the surface S is found to be about the same in both groups--somewhat higher in the low-pressure areas than in the high. It is not easy to see why there should be any difference in the altitude of S in these two groups, and the one found may be attributable to the distribution of the observations. Others have used this grouping in the discussion of their observations and have found the surface S higher in high-pressure areas and lower in low. Having accepted this finding as a universal fact, Prof. Humphreys has offered an explanation for it (this bulletin, Vol. II, p. 16, par. 4). But the fact does not seem to be universal, and the grouping is not a characteristic one when applied to the observations that have been made at Indianapolis, Omaha, and Huron. The differences shown in Table IX are apparently too large to be attributed to the distribution of the observations in the groups there compared. THE SURFACE OF MINIMUM TEMPERATURE. The surface of minimum temperature is about 5 kilometers higher up than the surface of maximum change with altitude in vertical temperature gradient, and the number of observations is consequently considerably less. What observations there are seem to show that both surfaces rise and fall with falling and rising air pressure, respectively, at the earth, s surface and with the seasons over rising air pressure. They seem to be farther apart in the summer than in the winter.
Excerpt from Bulletin of the Mount Weather Observatory, Vol. 4 There are five barometric highs on the oceans, as indicated by figure 1, that remain substantially fixed in position throughout the year though of varying intensity. Two of these are approximately 35 north of the Equator and three about 32 south of it. Two occur in the Pacific Ocean, one just west of southern California, the other near the coast of Chile; two in the Atlantic Ocean, near Morocco and southern Africa, respectively; and one in the Indian Ocean about half way between southern Africa and Australia. 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.