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Elements Of Astronomy $17.39 Purchase of this book includes free trial access to www.million-books.com where you can read more than a million books for free.This is an OCR edition with typos.Excerpt from book:CHAP. IV. On Refraction and Twilight. 46. AS connected with the earth, we may here consider its atmosphere, and how it affects the apparent places of the heavenly bodies. We know, from the science of pneumatics, that the air surrounding the earth is an elastic fluid, the density of which is nearly proportional to the compressing force, or the weight of the incumbent air. Whence it follows that the density continually decreases, and at a few miles high becomes very small. Now a ray of light passing out of a rarer medium into a denser, is always bent out of its course toward the perpendicular to the surface, on which the ray is incident. It follows therefore that a ray of light must be continually bent in its course through the atmosphere, and describe a curve, the tangent to which curve, at the surface of the earth, is the direction in which the celestial object appears. Consequently the apparent altitude if always greater than the true. 47. The refraction or deviation is greater, the greater the angle of incidence, and therefore greatest when the object is in the horizon, The horizontal refraction is about 32'. At 45 altitude, in its mean quantity it is 57i". 48. The refraction is affected by the variation of the quantity or weight of the superincumbent atmosphere at a given place, and also by its temperature. In computing the quantity of refraction, the height of the barometer and thermometer must be noted. The quantity of refraction at the same zenith distance varies nearly as the height of the barometer, the temperature remaining constant. The effect of a variation of temperature is to diminish the quantity of refraction about T'5 part for every increase of one degree in the height of the thermometer. Therefore, in all accurate observations of altitude or zenith d |
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Elements Of Astronomy $26.85 Purchase of this book includes free trial access to www.million-books.com where you can read more than a million books for free.This is an OCR edition with typos.Excerpt from book:CHAP. IV. On Refraction and Twilight. 46. AS connected with the earth, we may here consider its atmosphere, and how it affects the apparent places of the heavenly bodies. We know, from the science of pneumatics, that the air surrounding the earth is an elastic fluid, the density of which is nearly proportional to the compressing force, or the weight of the incumbent air. Whence it follows that the density continually decreases, and at a few miles high becomes very small. Now a ray of light passing out of a rarer medium into a denser, is always bent out of its course toward the perpendicular to the surface, on which the ray is incident. It follows therefore that a ray of light must be continually bent in its course through the atmosphere, and describe a curve, the tangent to which curve, at the surface of the earth, is the direction in which the celestial object appears. Consequently the apparent altitude if always greater than the true. 47. The refraction or deviation is greater, the greater the angle of incidence, and therefore greatest when the object is in the horizon, The horizontal refraction is about 32'. At 45 altitude, in its mean quantity it is 57i". 48. The refraction is affected by the variation of the quantity or weight of the superincumbent atmosphere at a given place, and also by its temperature. In computing the quantity of refraction, the height of the barometer and thermometer must be noted. The quantity of refraction at the same zenith distance varies nearly as the height of the barometer, the temperature remaining constant. The effect of a variation of temperature is to diminish the quantity of refraction about T'5 part for every increase of one degree in the height of the thermometer. Therefore, in all accurate observations of altitude or zenith d |
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Elements Of Astronomy $20.75 Purchase of this book includes free trial access to www.million-books.com where you can read more than a million books for free.This is an OCR edition with typos.Excerpt from book:CHAP. IV. On Refraction and Twilight. 46. AS connected with the earth, we may here consider its atmosphere, and how it affects the apparent places of the heavenly bodies. We know, from the science of pneumatics, that the air surrounding the earth is an elastic fluid, the density of which is nearly proportional to the compressing force, or the weight of the incumbent air. Whence it follows that the density continually decreases, and at a few miles high becomes very small. Now a ray of light passing out of a rarer medium into a denser, is always bent out of its course toward the perpendicular to the surface, on which the ray is incident. It follows therefore that a ray of light must be continually bent in its course through the atmosphere, and describe a curve, the tangent to which curve, at the surface of the earth, is the direction in which the celestial object appears. Consequently the apparent altitude if always greater than the true. 47. The refraction or deviation is greater, the greater the angle of incidence, and therefore greatest when the object is in the horizon, The horizontal refraction is about 32'. At 45 altitude, in its mean quantity it is 57i". 48. The refraction is affected by the variation of the quantity or weight of the superincumbent atmosphere at a given place, and also by its temperature. In computing the quantity of refraction, the height of the barometer and thermometer must be noted. The quantity of refraction at the same zenith distance varies nearly as the height of the barometer, the temperature remaining constant. The effect of a variation of temperature is to diminish the quantity of refraction about T'5 part for every increase of one degree in the height of the thermometer. Therefore, in all accurate observations of altitude or zenith d |
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Old Ballads (V. 2) $17.39 Purchase of this book includes free trial access to www.million-books.com where you can read more than a million books for free.This is an OCR edition with typos.Excerpt from book:VII. THE BRAVE MEN OF KENT. This Ballad is of a later date, but being upon the same sub- ject, we have introduced it here. It is the production of Tom Durfey, and was written the beginning of this century Vyh E N Harold was invaded, And falling lost his crown ; And Norman William waded Thro" gore to pull him down ; When countries round with fear profound, To mend their sad condition, And lands to save, base homage gave; Bold Kent made no submission. Cho. Sing, sing in praise of men of Kent, So loyal, brave and free; 'Mongst Britons' race, if one surpass, A man of Kent is he, The hardy stout free-holders, That knew the tyrant near, In girdles, and on shoulders, A grove of oaks did bear : Whom when he saw in battle draw, And thought how he might need 'em ; He turn'd his arms, allow'd their terms, Compleat with noble freedom : And when by barons wrangling, Hot faction did increase, And vile intestine jangling Had banish'd England's peace, The men of Kent to battle went, They fear'd no wild confusion ; But join'd with York, soon did the work, And made a blest conclusion : At hunting, or the race too, They sprightly vigour shew; And at a female chase too, None like a Kentish beau ; All blest with health; and as for wealth, By fortune's kind embraces, A yeoman gray shall oft out-weigh A knight in other places : The generous, brave and hearty, All o'er the shire we find; And for the low-church party, They're of the brightest kind : For king and laws, they prop the cause, Which high-church has confounded ; They love with height the moderate right, But hate the crop-ear'd round-head: The promis'd land of blessing, For our forefathers meant, Is now in right possessing, For Canaan sure wa... |
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