 | Jean Baptiste J.D. Boussingault - 1845 - 752 стор.
...the agent which most directly influences the temperature of our atmosphere. The length of the day, the number of hours during which the sun is above the horizon, coupled with the height to which he ascends, such is the cause with which the temperature of each particular... | |
 | Jean Baptiste Boussingault - 1845 - 724 стор.
...the agent which most directly influences the temperature of our atmosphere. The length of the day, the number of hours during which the sun is above the horizon, coupled with the height to which he ascends, such is the cause with which the temperature of each particular... | |
 | Jean Baptiste Boussingault - 1850 - 528 стор.
...the agent which most directly influences the temperature of our atmosphere. The length of the day, the number of hours during which the sun is above the horizon, coupled with the height to which he ascends, such is the cause with which the temperature of each particular... | |
 | Jean Baptiste Boussingault - 1854 - 528 стор.
...as the agent which most directly influences the temperature of our atmosphere The length of the day, the number of hours during which the sun is above the horizon, coupled with the height to which he ascends, such is the cause with which the temperature of each particular... | |
 | Jean Baptiste Boussingault - 1865 - 526 стор.
...the agent which most directly influences the temperature of our atmosphere. The length of the day, the number of hours during which the sun is above the horizon, coupled with the height to which he ascends, such is the cause with which the temperature of each particular... | |
 | Elias Loomis - 1868 - 326 стор.
...of maximum or minimum temperature depends not simply upon the sun's altitude at noon, but also upon the number of hours during which the sun is above the horizon ; that is, upon the relative length of the days and nights. The minimum occurs later in high than in... | |
 | William Henry Brewer, David M. Warren - 1890 - 154 стор.
...there are during the year but one day, of six months' duration, and one night, of the same length. (c) The number of hours during which the sun is above...the hours of daylight are differently distributed. (d) During the summer solstice the days are longest ; during the winter solstice the nights are longest.... | |
 | 1890 - 760 стор.
...Quarters of the Year. Table B. — Showing for each Degree of Latitude, from 49° N. to 53° N. the Total Number of Hours during which the Sun is above the Horizon, in each Week of the Year. Summaries of Kainfall and Mean Temperature, for the First, Second, Third, and... | |
 | 1907 - 528 стор.
...sky, and the prevalence of rain, are some of those which might be dealt with did space permit. Total number of hours during which the sun is above the horizon in each month, and for the whole year ; for each 2° of Latitude from 50° to 6O°. LATITUDE. 50° 52°... | |
 | Robert Stawell Ball - 1908 - 528 стор.
...advances. The amount of heat received from the sun at any place on the surface of the earth depends upon the number of hours during which the sun is above the horizon and its zenith distance at noon. At a place situated in latitude <f> the interval from sunrise to 243... | |
| |
... and more equable climate, gradually died out and disappeared.* In the state of stability to which the surface of the globe appears actually to have attained, the sun must be considered as the agent which most directly influences the temperature of... 
