A Complete Course of MeteorologyH. Baillière, 1845 - 598 páginas |
Dentro del libro
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Página xviii
... less powerfully assisted by my friend M. LEON LALANNE , Civil Engineer . He has given a graphic representation of forty - two numerical tables out of a hundred and thirteen , according to the common system of two rectangular co ...
... less powerfully assisted by my friend M. LEON LALANNE , Civil Engineer . He has given a graphic representation of forty - two numerical tables out of a hundred and thirteen , according to the common system of two rectangular co ...
Página 9
... less conducting power does it possess . A crowd of phenomena , falling under our daily observation , depend simply on the difference of conducting powers . On a summer's day expose to the sun a mass of metal and a mass of wood , of the ...
... less conducting power does it possess . A crowd of phenomena , falling under our daily observation , depend simply on the difference of conducting powers . On a summer's day expose to the sun a mass of metal and a mass of wood , of the ...
Página 12
... less elevation of temperature , which renders the existence of a central fire or incandescent nucleus very probable . But the surface of the earth is composed of bodies that are such bad conductors , that this central heat is very ...
... less elevation of temperature , which renders the existence of a central fire or incandescent nucleus very probable . But the surface of the earth is composed of bodies that are such bad conductors , that this central heat is very ...
Página 21
... less than the true mean , in the places where the latter is known , and add or deduct this difference from the mean obtained in the place where the observations are being made . For points situate on the Continent , and in the temperate ...
... less than the true mean , in the places where the latter is known , and add or deduct this difference from the mean obtained in the place where the observations are being made . For points situate on the Continent , and in the temperate ...
Página 24
... less rapidly to the end of July , when it attains its maximum . It falls at first slowly in August , then rapidly in September and Oc- tober , and descends to its minimum in the middle of January . This march is so constant , that the ...
... less rapidly to the end of July , when it attains its maximum . It falls at first slowly in August , then rapidly in September and Oc- tober , and descends to its minimum in the middle of January . This march is so constant , that the ...
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Otras ediciones - Ver todas
A Complete Course of Meteorology Ludwig Friedrich Kämtz,Charles Martins,Léon Lalanne Vista completa - 1845 |
A Complete Course of Meteorology Ludwig Friedrich Kämtz,Charles Martins,Léon Lalanne Vista completa - 1845 |
A Complete Course of Meteorology Ludwig Friedrich Kämtz,Charles Martins,Léon Lalanne Vista de fragmentos - 1845 |
Términos y frases comunes
abscissæ Alps Apenrade ascending current atmosphere attains aurora barometer bodies clouds Col du Géant cold colour column contained corresponding countries crepuscular curves deduced degree diminishes direction distance diurnal diurnal variation earth east winds electricity electrometer elevated equal equator Europe fall Faulhorn globe greater Halle heat height hemisphere horizon hygrometer increases influence instrument interior July kilogramme latitude less light lower maxima and minima maximum mean temperature mercury Meteorology metres millimetres minimum moist month morning mountains myriametres N.E. wind north winds oscillations passes perature phenomena plain pluviometer pole poles of cold pressure quantity of rain quantity of vapour rays regions Rigi rise S.W. winds seasons shews snow south winds southern hemisphere storms strata summer summit surface temperature tension thermometer tion trade-wind tube vapour of water Vide Appendix west winds whilst wind blows winter zenith Zurich