Weather Charts and Storm WarningsHenry S. King & Company, 1876 - 158 pagini |
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Pagina 4
... tion is the mean level of the sea , and the reduction is carried out by means of tables . A slight consideration of the foregoing remarks , and of the last - named principle in particular , will show how it comes about that the reading ...
... tion is the mean level of the sea , and the reduction is carried out by means of tables . A slight consideration of the foregoing remarks , and of the last - named principle in particular , will show how it comes about that the reading ...
Pagina 23
... tion , is related to the amount of difference of barome- trical pressure over a given distance , and this is defined as the ' gradient , ' a term which will be explained in Chapter IV . p . 41 , so that this force in no way depends on ...
... tion , is related to the amount of difference of barome- trical pressure over a given distance , and this is defined as the ' gradient , ' a term which will be explained in Chapter IV . p . 41 , so that this force in no way depends on ...
Pagina 24
Robert Henry Scott. tion here that the wind will blow hard from the same point , and for a considerable length of time , over a large district . The study of observations taken at the same hour over an extensive tract of the earth's ...
Robert Henry Scott. tion here that the wind will blow hard from the same point , and for a considerable length of time , over a large district . The study of observations taken at the same hour over an extensive tract of the earth's ...
Pagina 25
... one general principle which has been often brought forward as almost indisputable , and that is the principle known under the name of the ' Law of Gyra- tion , ' propounded by Professor Dove , of Berlin The Wind . 25.
... one general principle which has been often brought forward as almost indisputable , and that is the principle known under the name of the ' Law of Gyra- tion , ' propounded by Professor Dove , of Berlin The Wind . 25.
Pagina 26
Robert Henry Scott. tion , ' propounded by Professor Dove , of Berlin , some forty years ago . This principle is , that the wind changes more frequently ' with the sun , ' that is , from east , through south , to west , in the Northern ...
Robert Henry Scott. tion , ' propounded by Professor Dove , of Berlin , some forty years ago . This principle is , that the wind changes more frequently ' with the sun , ' that is , from east , through south , to west , in the Northern ...
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Aberdeen anticyclonic area of low Atlantic atmosphere barometer Beaufort scale Brest Cape Gris Nez centre changes Cheaper Edition Cloth clouds coast Crown 8vo cyclonic cyclonic area cyclonic disturbances cyclonic systems Daily Weather Report Demy 8vo depression direction Donaghadee east Easterly fact fall Fcap force Frontispiece gradients Henry hoisted Holyhead inch indication instance International Scientific Series Ireland islands isobars LL.D low pressure Meteorological Office motion of storms Noon North-west northern side northward Novel November 29 observations Observatory passing POEMS Portrait Post 8vo price 58 Prof Professor rain region Rochefort scale Scilly Scotland Second Edition SERMONS shown signal Skudesnaes Small crown 8vo Square crown 8vo stations storm warnings Stornoway Sumburgh Head telegraphic temperature thermometer Third Edition tion Translated University of Erlangen Valencia vapour tension veering velocity vols Volume WEATHER CHARTS Westerly ΙΟ ΟΙΟ
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