The Story of the Earth's AtmosphereD. Appleton, 1898 |
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Página 29
... poles it vanishes altogether . Between the tropics , the irregular changes of pressure introduced by the passage of storms are so small and infrequent that the diurnal variation is noticeable above all other changes , and is so regular ...
... poles it vanishes altogether . Between the tropics , the irregular changes of pressure introduced by the passage of storms are so small and infrequent that the diurnal variation is noticeable above all other changes , and is so regular ...
Página 34
... Pole than on any other part of the earth . The temperature of the Pole does not of course at once respond to this 34 THE STORY OF THE EARTH'S ATMOSPHERE .
... Pole than on any other part of the earth . The temperature of the Pole does not of course at once respond to this 34 THE STORY OF THE EARTH'S ATMOSPHERE .
Página 35
Douglas Archibald. Pole does not of course at once respond to this heating , since the average temperature effect lags about one month behind the solar radiation , and near the Pole the heat is mainly employed in melt- ing the Arctic ice ...
Douglas Archibald. Pole does not of course at once respond to this heating , since the average temperature effect lags about one month behind the solar radiation , and near the Pole the heat is mainly employed in melt- ing the Arctic ice ...
Página 38
... Pole , where one long day and night occurs in the year , the coldest month is delayed to Feb- ruary or March , in the northern hemisphere . When the sun's rays fall upon water , or where the locality is naturally moist , the heat is ...
... Pole , where one long day and night occurs in the year , the coldest month is delayed to Feb- ruary or March , in the northern hemisphere . When the sun's rays fall upon water , or where the locality is naturally moist , the heat is ...
Página 42
... pole is about o degree F. and at the equator between 80 and 90 degrees F. , we can similarly alter our tem- perature degree F. by travelling north or south . about 70 to 80 English miles . As an illustration of a combination of these ...
... pole is about o degree F. and at the equator between 80 and 90 degrees F. , we can similarly alter our tem- perature degree F. by travelling north or south . about 70 to 80 English miles . As an illustration of a combination of these ...
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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.