The practice of navigation and nautical astronomy. [With] Tables [and] Supplement to the first ed, Nide 261870 |
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Tulokset 1 - 5 kokonaismäärästä 95
Sivu xviii
... .. 237 252 .... ...... 259 260 260 II . BY DIFFERENCE OF ALTITUDE NEAR THE MERIDIAN 267 III . BY EQUAL ALTITUDES ..... IV . RATING THE CHRONOMETER 269 275 CHAP . VII . FINDING THE Longitude VIII . I. xviii CONTENTS .
... .. 237 252 .... ...... 259 260 260 II . BY DIFFERENCE OF ALTITUDE NEAR THE MERIDIAN 267 III . BY EQUAL ALTITUDES ..... IV . RATING THE CHRONOMETER 269 275 CHAP . VII . FINDING THE Longitude VIII . I. xviii CONTENTS .
Sivu xx
... Difference of Longitude and Corresponding De- parture .. 485 .... 486 495 5. Spherical Traverse Table 6. Meridional ... Differences .. 614 TIMES OF CERTAIN PHENOMENA . TABLE PAGE 26. Apparent Time TABLES .
... Difference of Longitude and Corresponding De- parture .. 485 .... 486 495 5. Spherical Traverse Table 6. Meridional ... Differences .. 614 TIMES OF CERTAIN PHENOMENA . TABLE PAGE 26. Apparent Time TABLES .
Sivu 4
... difference between 3 and These become and 14 , the difference 35 35 of which is I 35 2 Ex . 2. Subtract from Ans . 33 I I 55 363 12 II Ex . 3. Subtract from Ans . 83 18 - I 13 65 [ 4. ] Multiplication . 15. To multiply a fraction by a ...
... difference between 3 and These become and 14 , the difference 35 35 of which is I 35 2 Ex . 2. Subtract from Ans . 33 I I 55 363 12 II Ex . 3. Subtract from Ans . 83 18 - I 13 65 [ 4. ] Multiplication . 15. To multiply a fraction by a ...
Sivu 23
... difference of the directions in which they lie : thus A B C , or B , is the angle contained by the two lines B A ... difference between an angle and 90 ° is called its comp le- ment ; the difference to 180 ° is called its supplement . An ...
... difference of the directions in which they lie : thus A B C , or B , is the angle contained by the two lines B A ... difference between an angle and 90 ° is called its comp le- ment ; the difference to 180 ° is called its supplement . An ...
Sivu 41
... difference of BCE and A CE , and is double of A D B , the difference of B D E and A D E. When E falls on AB , as in fig . 2 , ACB is the sum of ACE and BCE , and is double the sum of the angles A DE and BDE , or the angle A D B. 140 ...
... difference of BCE and A CE , and is double of A D B , the difference of B D E and A D E. When E falls on AB , as in fig . 2 , ACB is the sum of ACE and BCE , and is double the sum of the angles A DE and BDE , or the angle A D B. 140 ...
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The Practice Of Navigation And Nautical Astronomy. [with] Tables [and ... Henry Raper Esikatselu ei käytettävissä - 2019 |
The Practice Of Navigation And Nautical Astronomy. [with] Tables [and ... Henry Raper Esikatselu ei käytettävissä - 2022 |
Yleiset termit ja lausekkeet
add the log altitude alts appears azim azimuth bearing called celestial body celestial equator centre chart chronometer circle colat compass Computation corr correction cosec Course and Distance D.Lat decimal decl declination deviation diff difference direction Dist divided employed equal equator error exceeds feet find the Course fraction given gives greater Greenwich Date height of eye Hence horizon interval latitude less logarithms longitude magnetic magnetic bearing measured meridian miles minutes moon moon's multiplied Nautical Almanac nearly observation parallax parallel Parallel Sailing passes Plane Sailing planet pole prime vertical prop quantity radius reckoned reduce refraction result rhumb line right angles Right Ascension sailing Semid sextant shews ship side sine star subtract sum rejecting tens sun's Traverse Table triangle true true alt variation watch
Suositut otteet
Sivu 41 - The angle in a semicircle is a right angle ; the angle in a segment greater than a semicircle is less than a right angle; and the angle in a segment less than a semicircle is greater than a right angle.
Sivu 147 - Since the apparent altitude is too great on account of refraction, and too small on account of parallax, the diff. between these quantities is the diff. between the true and apparent altitudes. This difference, or the combined effect of parallax and refraction, is called the Correction of Altitude. The moon's Corr. of Alt. is given in Table 39; that of a star is merely its refraction. 439. The SEMI-DIAMETER of a celestial body is half the angle subtended by the diameter of the visible disc. Thus...
Sivu 38 - A parallelogram is a four.sided figure, of which the opposite sides are parallel; and the diameter is the straight line joining two of its opposite angles.
Sivu 19 - The characteristic of a number less than 1 is found by subtracting from 9 the number of ciphers between the decimal point and the first significant digit, and writing — 10 after the result.
Sivu 43 - ... section shall be parallel to the remaining side of the triangle. Let DE be drawn parallel to BC, one of the sides of the triangle ABC: then BD shall be to DA, as CE to EA. Join BE, CD; then the triangle BDE is equal...
Sivu 105 - The distance between two points on the surface of a sphere is the length of the minor arc of a great circle between them.
Sivu 186 - A line drawn from Polaris perpendicular to the line of the Pointers, and on the opposite side to the Great Bear, passes, at 48° distance, through CAPELLA, one of the brightest stars. In this same line, about the same distance on the opposite side of the pole, is a.
Sivu 145 - ... of Altitude are circles parallel to the horizon. 431. ZENITH DISTANCE is the arc included between the zenith and the celestial body, or the angular distance of a body from the zenith of which that arc is the measure. The zenith distance is, therefore, the complement of the altitude to 90°, as Z A.
Sivu 4 - RULE. Multiply all the numerators together for a new numerator, and all the denominators for a new denominator: then reduce the new fraction to its lowest terms.
Sivu 358 - Frigate La Venus, 1836-9, vol. iii. p. 419) paid particular attention to this indication, and remarks that the observations generally shew a lowering of the thermometer on approaching land, but they disprove that the water on a bank is always colder.* 1039. The temperature of the sea has been observed to change several degrees, in intervals of time varying from a few hours to a day and a half previous to a change of wind, the water becoming gradually warmer when the wind was about to blow from a...