The Story of the Earth's AtmosphereD. Appleton, 1898 |
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Página 8
... Storm " " the . 97 Fig . 24 - Diffusive Limits of the Component Gases of the Atmosphere Fig.25 - Cirrus Cloud ( var Tracto Cirrus , 1889 ) · ΙΟΙ · 113 Fig . 4 33 Fig . 26 · . 115 Fig . 5 35 Fig . 27 116 • Fig . 6 43 Fig . 28 - Festooned ...
... Storm " " the . 97 Fig . 24 - Diffusive Limits of the Component Gases of the Atmosphere Fig.25 - Cirrus Cloud ( var Tracto Cirrus , 1889 ) · ΙΟΙ · 113 Fig . 4 33 Fig . 26 · . 115 Fig . 5 35 Fig . 27 116 • Fig . 6 43 Fig . 28 - Festooned ...
Página 9
... storm , to be cer- tain that it is just as material as the solid earth to which it clings . Its past history , unlike that of its more solid partner , is not written in the unmistakable lan- guage of successive rock strata , or fossil ...
... storm , to be cer- tain that it is just as material as the solid earth to which it clings . Its past history , unlike that of its more solid partner , is not written in the unmistakable lan- guage of successive rock strata , or fossil ...
Página 29
... storms are so small and infrequent that the diurnal variation is noticeable above all other changes , and is so regular that the late Mr. Broun , of Trevandrum Observatory in India , used to declare he could tell the time of day by ...
... storms are so small and infrequent that the diurnal variation is noticeable above all other changes , and is so regular that the late Mr. Broun , of Trevandrum Observatory in India , used to declare he could tell the time of day by ...
Página 54
... storms , cloud proportion , etc. , while the late Professor Jevons endeavoured to shew that even commercial panics were brought about periodically through the medium of such indirect . consequences . Though there is much scepticism as ...
... storms , cloud proportion , etc. , while the late Professor Jevons endeavoured to shew that even commercial panics were brought about periodically through the medium of such indirect . consequences . Though there is much scepticism as ...
Página 59
... storm , under different conditions , which will be alluded to later on , but in order that there may be intense local action and a real " courant ascendant , " the air must not be merely gently lifted up and overflow , which is the only ...
... storm , under different conditions , which will be alluded to later on , but in order that there may be intense local action and a real " courant ascendant , " the air must not be merely gently lifted up and overflow , which is the only ...
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Términos y frases comunes
30 inches æther angle anti-cyclones APPLETON ascend atmos atmosphere average balloon barometric pressure Bay of Bengal belt blow carbonic acid cause centre changes Charles's law cirrus cirrus cloud climate cloud cold condensed cool cubic centimetre cumulus cumulus clouds cyclones damp degrees direction dry air earth earth's surface effect electricity equator equatorial fact fall feet Ferrel flying machine globe heat height high pressure increased India isobars kite Krakatoa land latitude layer light lower mass mercury miles an hour motion mountain move northern hemisphere observed occurs ocean oxygen particles perature phere plane poles Prof radiation rain rainfall range rays reached rise rotation round sea-level seasonal shew side solar southern storm Story stratum summer temperature termed theory thunderstorms tion tornado tropical cyclones tropics ture upper upward vapour velocity vertical warm waterspout waves weather wind
Pasajes populares
Página 110 - All the rivers run into the sea; yet the sea is not full; unto the place from whence the rivers come, thither they return again.