## Navigation and Nautical Astronomy, Part 1Longman, Brown, Green, and Longmans, 1858 |

### From inside the book

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**mean**solar year To find the length of the sidereal year · Page 51 • 60 60 61 The sidereal day , the apparent solar day , and the**mean**solar day . 61 To find the daily motion of the**mean**...**time**at**Greenwich**corresponding iv CONTENTS . Page v

H. W. Jeans. Page XV . To find the

H. W. Jeans. Page XV . To find the

**time**at**Greenwich**corresponding to a given lunar distance To take out a planet's right ascension and declination . XVI . Given**mean**solar**time**and the equation of**time**to find apparent solar**time**, and ... Page vi

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**Greenwich mean**time at some instant • XLIII . To find error of chronometer on mean time at the ship by a single altitude of the sun 161 166 168 • 170 XLIV . To find the error of chronometer on mean time at Greenwich by a single altitude ... Page 71

... mean time is known . Rule VI . To the time shown by chronometer , apply its error on

... mean time is known . Rule VI . To the time shown by chronometer , apply its error on

**Greenwich mean**time ; adding if error is slow , and ... Greenwich date by chronometer . Greenwich date approximately . July IN NAUTICAL ASTRONOMY . 71. Page 72

... Greenwich date is July 10th , 10h 39m 533 . EXAMPLE 2 . Aug. 3rd , 1853 , at 5h 42m P.M. mean time nearly , in long . by account 150 ° 30 ′ W. , a chronometer showed 3h 23m 15s , and its error on

... Greenwich date is July 10th , 10h 39m 533 . EXAMPLE 2 . Aug. 3rd , 1853 , at 5h 42m P.M. mean time nearly , in long . by account 150 ° 30 ′ W. , a chronometer showed 3h 23m 15s , and its error on

**Greenwich mean**time was 10m 10s - 4 slow ...### Other editions - View all

### Common terms and phrases

24 hours altitude for index apparent distance April 27 ascension mean sun ascension of mean auxiliary angle celestial concave celestial equator chro colatitude compass bearing correction in altitude cosec decl diff east of meridian Elements from Nautical EXAMPLES find the latitude Greenwich date Greenwich mean haversines heavenly body height of eye horizontal parallax hour angle Index cor index correction June longitude by chronometer mean time nearly moon moon's declination Moon's right Moon's semi moon's semidiameter Nautical Almanac observed altitude observed meridian altitude P.M. mean pass the meridian point of Aries polar distance pole proportional logarithm refraction required the latitude required the longitude required the true Right asc Right ascension mean sea 20 feet ship mean sidereal star subtract Sun's declination sun's L. L. sun's lower limb true altitude true bearing true distance true zenith distance vers versines zenith dist

### Popular passages

Page 12 - Fig. 3) loaded on the circular side with lead sufficient to make it swim upright in the water: to this is fastened a line about 150 fathoms long, called the Log-line, which is divided into certain spaces called knots, and is wound on a reel (see Plate VI.

Page 54 - ... consequence of the whirling motion of the earth about its axis, the parts near the equator, which have the greatest velocity, acquire thereby a greater distance from the centre than the parts near the poles.

Page 60 - The hour angle of a heavenly body, is the angle at the pole between the celestial meridian and the circle of declination passing through the place of the body ; thus, zpx is the hour angle of x.

Page 59 - The right ascension of a heavenly body is the arc of the equator, intercepted between the first point of Aries and the circle of declination, passing through the place of the...

Page 61 - The apparent solar day is the interval between two successive transits of the sun's centre over the same meridian.

Page 63 - Mean Solar Day is the interval between two successive transits of the mean sun over the same meridian ; it begins when the mean sun is on the meridian.

Page 13 - ... ascertained at sea by observing the magnetic bearing of- the sun when in the horizon, or at a given altitude abo-ve it. From this observation the true bearing is found by rules given in nautical astronomy. The difference between the true bearing and the observed bearing by compass determines this correction.

Page 258 - W., and at the same time the observed altitude of the sun's lower limb was 21° 40' 45", the index correction was — 2' 18", and the height of the eye above the sea was 14 feet : required the variation.

Page 199 - To the hour angle thus found, add the star's right ascension; and from the sum, increased if necessary by 24 hours, subtract the right ascension of the mean sun ; the remainder is mean time at the place at the instant of observation.

Page 54 - ... path of the sun as seen from the Earth, and is called the Ecliptic. The plane of the Earth's equator, extended till it meets the concave surface of the heavens, forms what is called the Celestial Equator, or the Equinoctial. The ecliptic and the equinoctial form an angle of 23° 28', and this angle is called the Obliquity of the Ecliptic. The axis of the Earth, therefore, instead of being perpendicular to the plane of its orbit, is inclined to it at an angle of (90° — 23° 28') 66° 32'.