The Story of the Earth's AtmosphereD. Appleton, 1898 |
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Página 29
... seasonal transfers of air between sea and land and from hemisphere to hemisphere . Others , again , which run through their course in a day , are connected with the daily heating and cooling of the air by the sun , while certain short ...
... seasonal transfers of air between sea and land and from hemisphere to hemisphere . Others , again , which run through their course in a day , are connected with the daily heating and cooling of the air by the sun , while certain short ...
Página 34
... seasonal change in the angle of the sun above the horizon and secure the same general amount of sun radia- tion . We should not , however , be able to secure the same average temperature since the direct ef- fects of the radiation on ...
... seasonal change in the angle of the sun above the horizon and secure the same general amount of sun radia- tion . We should not , however , be able to secure the same average temperature since the direct ef- fects of the radiation on ...
Página 35
... exaggerates the differ- ence caused by the hourly and seasonal changes in the angle of the sun , especially as it approaches the horizon . Direct observations of the sun - heat by means of THE TEMPERATURE OF THE ATMOSPHERE . 35.
... exaggerates the differ- ence caused by the hourly and seasonal changes in the angle of the sun , especially as it approaches the horizon . Direct observations of the sun - heat by means of THE TEMPERATURE OF THE ATMOSPHERE . 35.
Página 44
... seasonal changes vary ac- cording as the locality is continental or maritime , and its soil is dry and rocky or damp and alluvial , and the average itself depends largely on these and other conditions besides mere latitude . The general ...
... seasonal changes vary ac- cording as the locality is continental or maritime , and its soil is dry and rocky or damp and alluvial , and the average itself depends largely on these and other conditions besides mere latitude . The general ...
Página 48
... seasonal and daily changes would be very much less conspicuous than near the surface . By means of thermometers and thermographs the temperature of the atmosphere near the surface is read at certain hours or recorded con- tinuously ...
... seasonal and daily changes would be very much less conspicuous than near the surface . By means of thermometers and thermographs the temperature of the atmosphere near the surface is read at certain hours or recorded con- tinuously ...
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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.