The practice of navigation and nautical astronomy. [With] Tables [and] Supplement to the first ed, Volume 261870 |
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Page vi
... bearing , and by its altitude observed above the sea - horizon . The seaman will find every necessary information on the subject of local magnetic deviation . The highly useful problem of determining the latitude at sea , by the ...
... bearing , and by its altitude observed above the sea - horizon . The seaman will find every necessary information on the subject of local magnetic deviation . The highly useful problem of determining the latitude at sea , by the ...
Page xvii
... BEARING AND DISTANCE 114 II . DETERMINATION OF DISTANCE III . METHODS BY THE CHART .... 114 120 V. CHARTS 122 I. USE OF MERCATOR'S CHART II . CONSTRUCTION OF MERCATOR'S CHART . III . PROPERTIES OF CERTAIN PROJECTIONS 123 .... 127 127 VI ...
... BEARING AND DISTANCE 114 II . DETERMINATION OF DISTANCE III . METHODS BY THE CHART .... 114 120 V. CHARTS 122 I. USE OF MERCATOR'S CHART II . CONSTRUCTION OF MERCATOR'S CHART . III . PROPERTIES OF CERTAIN PROJECTIONS 123 .... 127 127 VI ...
Page xix
... BEARINGS IX . THE TIDES .. I. PHENOMENA of the TIDES PAGE 279 279 283 301 304 307 ..... ... 308 308 310 313 317 317 II . RULES FOR finding the TIME OF HIGH Water .. 323 III . TIDE OBSERVATIONS 326 NAVIGATING THE SHIP . I. SHAPING THE ...
... BEARINGS IX . THE TIDES .. I. PHENOMENA of the TIDES PAGE 279 279 283 301 304 307 ..... ... 308 308 310 313 317 317 II . RULES FOR finding the TIME OF HIGH Water .. 323 III . TIDE OBSERVATIONS 326 NAVIGATING THE SHIP . I. SHAPING THE ...
Page xx
... Bearings and the Distance run between them 500 8. True Depression or Distance of the Sea Horizon 501 9. Number of Feet subtending an Angle of l ' at Different Distances ... 10. Maritime Positions .. .. 501 502 11. Approximate Variation ...
... Bearings and the Distance run between them 500 8. True Depression or Distance of the Sea Horizon 501 9. Number of Feet subtending an Angle of l ' at Different Distances ... 10. Maritime Positions .. .. 501 502 11. Approximate Variation ...
Page 52
... bearing . 2. Degree of Dependance . 170. The result of every computation is , as above remarked , No. 168 , more or less uncertain . If we knew the error in one of the elements , we could easily find the effect it would produce on the ...
... bearing . 2. Degree of Dependance . 170. The result of every computation is , as above remarked , No. 168 , more or less uncertain . If we knew the error in one of the elements , we could easily find the effect it would produce on the ...
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The Practice Of Navigation And Nautical Astronomy. [with] Tables [and ... Henry Raper No preview available - 2019 |
The Practice Of Navigation And Nautical Astronomy. [with] Tables [and ... Henry Raper No preview available - 2022 |
Common terms and phrases
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
Popular passages
Page 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.
Page 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...
Page 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.
Page 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.
Page 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...
Page 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.
Page 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.
Page 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.
Page 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.
Page 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...