The Story of the Earth's AtmosphereD. Appleton, 1898 |
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Página 33
... Equator ) . E ۲ Sun inclined at 17 de- grees ( as at mid - winter noon in England ) . FIG . 4 . same width of rays is concentrated upon A B in the one case , and spread over A C in the other , consequently the heat received by the earth ...
... Equator ) . E ۲ Sun inclined at 17 de- grees ( as at mid - winter noon in England ) . FIG . 4 . same width of rays is concentrated upon A B in the one case , and spread over A C in the other , consequently the heat received by the earth ...
Página 34
... equator than elsewhere . If we take the six months of the northern summer , more heat falls on latitude 25 degrees north ( the latitude of northern India ) than on the equator . If again we take the three months nearest midsummer , i ...
... equator than elsewhere . If we take the six months of the northern summer , more heat falls on latitude 25 degrees north ( the latitude of northern India ) than on the equator . If again we take the three months nearest midsummer , i ...
Página 42
... equator along which the temperature would range on either side of a certain average throughout the year . These would rise to their highest level over the equator , and their height in any latitude would show us at what elevation we ...
... equator along which the temperature would range on either side of a certain average throughout the year . These would rise to their highest level over the equator , and their height in any latitude would show us at what elevation we ...
Página 46
... Equator . So far as the British Islands are concerned it is equally plain that the northward flow of the gulf - stream of the Atlantic raises the isotherm of 50 ° F. which normally belongs to latitude 40 ° and passes through Nippon ...
... Equator . So far as the British Islands are concerned it is equally plain that the northward flow of the gulf - stream of the Atlantic raises the isotherm of 50 ° F. which normally belongs to latitude 40 ° and passes through Nippon ...
Página 47
... Equator exhibits a generally higher temperature than that which lies over oceans in the same latitude . Since heating and cooling are recipro- cal operations it is easy to see that the reverse applies to the temperature over polar seas ...
... Equator exhibits a generally higher temperature than that which lies over oceans in the same latitude . Since heating and cooling are recipro- cal operations it is easy to see that the reverse applies to the temperature over polar seas ...
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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.