British Almanac Containing Astronomical, Official and Other Information Relating to the British Isles, the Dominions Oversea and Foreign Countries, Vol. 3 (Classic Reprint)
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Produktbeschreibung
Excerpt from British Almanac Containing Astronomical, Official and Other Information Relating to the British Isles, the Dominions Oversea and Foreign Countries, Vol. 3 Explanation of the column headed "Thermometrical Register." The Thermometrical Register commences with Nov. 1858, and closes with Oct. 1859, inclusive. These registers have been carefully copied from those made at the Royal Observatory, Greenwich, and which are also deposited with the Royal Society. They show the highest and lowest ranges within each twenty-four hours, from twelve different readings. Each month is placed with its corresponding month, as affording the most ready and advantageous means of comparison, although by this arrangement the register of the last two months of 1858 follows the ten months of 1859, which are all we can give up to the day of publication. Explanation of the columns headed "Length of day," "Day´s increase or decrease," "Day breaks" and "Twilight ends" The column headed "Length of day" contains the number of hours and minutes between sunrise and sunset. The column headed "Day´s increase" expresses the number of hours and minutes which the day has increased since the shortest day; and, where the column is headed "Day´s decrease," it expresses the number of hours and minutes which the day has decreased since the longest day; for example, the length of the longest day in 1860 is put down in the column "Length of day" at 16h. 34m.; and on the 6th of July following we find that the length of the day, or the number of hours and minutes between sunrise and sunset, is set down at 16h. 23m.; hence the day has decreased 11m. since the longest day, and, accordingly, in the column "Day´s decrease," we find opposite July the 6th 0h. 11m. Equation of Time. In this Almanac the calculations are all made for mean time (given by the clock), instead of apparent time (given by the sun-dial), which latter had been used up to the year 1833. It mist be obvious that, for all practical purposes, mean time is the most useful; and to obtain it from apparent time, the columns in the Almanac headed "Equation of Time" should be used. The column "Equation of Time" ought, for example, to be consulted when persons are desirous of setting their clock by a sun-dial. When clock after sun is written above the number of minutes and seconds opposite to the day, then the clock ought to be set so much slower than the sun-dial, and the contrary. Moonlight. The Moon´s age is set down in days and the nearest tenths of days from the time of change. Thus it is New Moon on the 23rd of January at 0h. 17m. morning, and therefore at noon she is 11h. 43m. old, which is set down as five-tenths. The fraction of the day of course continues the same throughout the lunation. List Of The Correspondence Of Eras With The Year 1860. [In those Eras which begin with the Christian year, the year alone is stated; in those which begin at a different season, the month in which the 1st of January, 1860, occurs is also given.] 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 intention
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