And now we may proceed to explain the subject of this chapter.
Up to the year 1846, when Leverrier made his great discovery, it was believed that Ura.n.u.s was the most distant planet revolving around the sun. Ura.n.u.s itself was discovered by Sir John Herschel in England in the year 1781. As this planet takes eighty-four years to go round the sun, its complete revolution had not yet been observed in 1846; in spite of this, however, the course of Ura.n.u.s was calculated and known very precisely, because the attractive force of the sun was known; and all the disturbances that might influence the planet were taken into account.
But notwithstanding all nicety of calculations, the real course of Ura.n.u.s would not at all agree with the one computed. At that time already, long before Leverrier"s discovery, the idea arose that beyond Ura.n.u.s, in a region where the human eye could, in spite of all telescopes, discover nothing, there must probably exist a planet which changed the course of Ura.n.u.s. Bessel, a great astronomer, who unfortunately for science died too soon, was already on the point of finding out by computation the unknown disturber. But he died, shortly before Leverrier"s discovery. As early even as 1840, Maedler, in the city of Dorpat, in Russia, wrote a fine article on this as yet unseen disturber.
Leverrier, however, began the task and finished it. He computed with an acuteness that was admired by all men of science. He investigated whereabout in the heavens that intruder must be situated, so as to be able to trouble Ura.n.u.s to such an extent; how fast this disturber itself must move in its...o...b..t, and how large must be its ma.s.s.
We live to see the triumph of Leverrier"s being able to discover with his _mental_ eye, by means of computation only, a planet at a distance of millions of miles from him.
Therefore let us say: Honor science! Honor the men that cultivate it!
And all honor to the human intellect which sees farther than the human eye!
PART VI.
METEOROLOGY
CHAPTER I.
SOMETHING ABOUT THE WEATHER.
We presume that in a state of unusual bad weather there are many persons, who find occasion to reflect on the nature of weather in general.
A few years ago, we had "green Christmas and white Easter," and spring was of course far behind when Pentecost arrived. We had still cold and rainy days, while the nights were frosty; and, if one might judge from appearances, it seemed that nature had made a mistake, and had not known of our being then in the month of June, which, with us, is usually a delightful month.
The sun alone was right. He rose on the 9th of June of that year precisely at 4 o"clock 30 minutes, as was prescribed to him by the calendar; and set at 7 o"clock 30 minutes, precisely according to orders. At that time the sun was hastening towards summer, he lengthened the days and shortened the nights; but he alone is not capable of governing the weather, and our friends the astronomers, although they are able to calculate the sun"s course with more precision than the engineer can the locomotive"s, are themselves greatly embarra.s.sed when asked, "What kind of weather shall we have the day after to-morrow?"
It is unpardonable that some of our almanacs, especially those for the farmer, contain prophecies about the weather. We cannot be too indignant against the foolish superst.i.tion which this abuse tends to foster. And what is worse, really shameful, is, that those who print such things do not believe in them themselves, but consider them a necessity sanctioned by age and custom, and offer it as such to the credulity of the public.
The subject of this article on the knowledge of weather, is a science, a great branch of the natural sciences; but it is a branch just developing, and therefore has, up to the present time, not yet brought forth any fruit.
It is very likely that at some future day we shall be able to indicate in advance the weather of any given place. But for the present this is impossible; and if from time to time men arise and announce that they can calculate and determine in advance the state of the weather in any given place--pretending to consult the planets, etc.--we take it for granted that they are as unreliable as the weather-prophets of the almanacs.
We said above that the weather might possibly be determined a few days ahead; science is at present almost far enough advanced for it. But there are needed for that purpose grand inst.i.tutions, which must first be called into life.
If for the proper observation of the weather, stations were erected throughout the extent of our country, at a distance of about seventy miles from each other, and if these stations were connected by a telegraph-wire, managed by a scientific reliable observer; then we might, in the middle portion of our country, be able to determine in advance the state of the weather, though for a short time only.
For the changeableness of the weather depends on the nature and motion of the air, and on the amount of moisture, and the direction of the winds. It is mostly occasioned by currents of air which pa.s.s over the earth, producing, wherever they meet, here cold, there heat--here rain, there hail or snow.
Along a part of the coast of the United States electric telegraphs have been established. Vessels receive, at a considerable distance, the news of a storm approaching, together with its velocity and direction. The electric telegraph being quicker than the wind, the vessels receive the news in time to take their directions. Before the storm reaches them, they have been enabled to take precautionary measures for its reception.
This is a great step forward in our new science. But not before the time when such stations shall be established everywhere throughout the land, will meteorology manifest its real importance. For it has, like every other science, firmly established rules, which can easily be calculated and verified; while, on the other hand, allowances must be made for changeable conditions which tend to disturb the rules.
We will now endeavor to introduce to our readers these established rules, and explain the changeable conditions to which we refer.
CHAPTER II.
OF THE WEATHER IN SUMMER AND WINTER.
As we have stated above, there exist fixed rules about the weather; these rules are simple and easy to compute. But our computations are often disturbed by a great many circ.u.mstances beyond our reach, so much that we are governed more by exceptions than rules.
These latter are based on the position of our earth with regard to the sun. They are, therefore, easy to determine, for astronomy is a science resting on firm pillars; and although nothing in the universe is so far from us as the stars, yet there is nothing in the world so certain as our knowledge of the courses of the constellations and their distances.
Many of our readers may be surprised, perhaps, to hear that we know more accurately the distance from the earth to the sun than the distance from New York to Cincinnati. Indeed, astronomical knowledge is the most reliable in the world. No merchant is able to measure a piece of cloth without being mistaken, to say the least, as much as 1/300 part; while the uncertainty with respect to distances of bodies in the solar system amounts to a great deal less than 1/300 part.
Our earth turns on its axis once in every twenty-four hours, and goes also round the sun once a year. But the earth"s axis is inclined towards the earth"s...o...b..t--orbit is the circle which a celestial body describes in its revolution around another--in such a manner as to cause the earth, in its...o...b..t round the sun, to be illuminated for six months on one side, and for six months on the other side of the earth. Hence it happens, that at the north pole there is continual day during six months in the year, after which follows uninterrupted winter for the next six months; in the same way the day on the south pole lasts six months, and the night following the same length of time. In the middle between both poles, however, in the regions around the equator, the day has throughout the year twelve hours; the night, of course, the same; while in the countries between the equator and the poles, the length of day and night is, through the whole year, constantly varying.
We, in the United States, inhabit the northern hemisphere; when, therefore, the time comes that the north pole has day for six months, we in North America, being situated about half-way between the equator and north pole, enjoy long days and short nights. The inhabitants of those countries, however, situated on the southern hemisphere, have at that time short days and long nights. But when the time comes that there is six months" night on the north pole and six months" day on the south pole, then will the inhabitants of the southern hemisphere have long days, and we long nights.
Intimately connected with the length of day and night are our seasons, especially summer and winter; for together with the sun"s light heat is also called forth. During our long days, therefore, it is very warm with us, for the sun"s rays heat the soil. During our short days we experience cold, because the warming light of the sun does not reach our earth directly. For this reason the northern hemisphere enjoys summer while the southern has winter; and _vice versa_, when we have mid-winter, people in the other hemisphere are in the midst of summer.
When we are snowed up at Christmas, and seek joy and elevation by the cheerful fireside in the brightly-lighted room, we may, perhaps, think of our friends and relatives who have emigrated to Australia, and the question may occur to us, how things may be with them this cold weather, and how they are enjoying the holidays?
Now, would not the uninformed be surprised, if a letter were to arrive from Australia, written at Christmas, telling how the writer enjoyed Christmas in his vine-arbor, where he had sought shelter from the terrible heat of the day, and that he had but late at night gone to his room, and he could scarcely sleep then on account of the heat, and the longing for his former home in the United States, where he could always enjoy cool weather at Christmas.
The uninformed will now learn that Australia lies in the southern hemisphere, while we are in the northern, and that there they live in midst of summer, while we are buried in snow. Nor will he now be surprised when he reads, that it snowed in Australia in the month of August, and that his friend or relative there reposed by the fireside, and read the letter from home by the light of the lamp, at the same hour that we here were taking an afternoon walk in the summer shade.
The heat of summer, however, does not altogether depend upon the length of the day; nor does the cold of winter upon its shortness; but princ.i.p.ally on this, that during summer-time the sun at noon stands directly over head; that therefore his vertical rays are enabled to pierce the soil with intense heat; while in winter-time the sun at noon stands nearer to the horizon; his rays fall on the earth obliquely, therefore heating the soil with but feeble power.
We shall presently see that this position of the sun exercises great influence upon the weather.
CHAPTER III.
THE CURRENTS OF AIR AND THE WEATHER.
In order to fully understand the conditions of the atmosphere, one must carefully notice the following:
Though the sun produces summer and winter, and although his beams call forth heat, and the absence of heat causes intense cold on the surface of the globe, yet the sun alone does not make what we call "Weather."
If the sun"s influence alone were prevalent, there would be no change at all during our seasons; once cold or warm, it would invariably continue to be so, according to the time of the year. The sun, however, produces certain movements in the air; currents of air or winds pour from cold countries into warm ones, and _vice versa_ from warm ones into cold ones. It is this that makes our sky be cloudy or clear; that produces rain and sunshine, snow and hail, refreshing coolness in summer and warmth sometimes in midwinter, as also chilly nights in summer and thaw in winter. In other words, it is more properly the motion of the air, the wind, that produces what we call _weather_; that is, that changeableness from heat to cold, from dryness to moisture, all of which may be comprised in one name, weather.
But whence does the wind arise? It is caused by the influence of the sun"s heat upon the air.
The whole earth is enveloped with a misty cover called "air." This air has the peculiar quality of expanding when it becomes heated. If you put a bladder that is filled with air and tied up, into the pipe of a heated stove, the air inside will expand so much as to burst the bladder with a loud report. The warm expanded air is lighter than the cold air, and always ascends in the atmosphere.
Lofty rooms are therefore difficult to heat because the warm air ascends towards the ceiling. In every room it is much cooler near the floor than near the top of the room. This accounts for the singular fact that in winter our feet, though warmly clad in stockings and shoes or boots, feel cold more often than our hands, which are entirely uncovered. If you ascend a ladder in a tolerably cold room, you are surprised at finding it much warmer above than below in the room. The flies take advantage of this in autumn, when they are seen to promenade on the ceiling, because there it is warm as in summer, while near the floor it is cold; owing to the circ.u.mstance that warm air, being lighter than cold, ascends.