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 91
Sivu ix
... correction has rendered it indispensable to trace its effects on the longitudes of the Eastern Seas . Precision in the Maritime Positions , especially in the longitudes , becomes , as navigation advances to perfection , a matter of ...
... correction has rendered it indispensable to trace its effects on the longitudes of the Eastern Seas . Precision in the Maritime Positions , especially in the longitudes , becomes , as navigation advances to perfection , a matter of ...
Sivu xx
... Correction of the Sun's Declination , at Sea ..... 602 20. Correction of the Equation of Time , at Sea ..... 602 21. For reducing Daily and Twelve - hourly Variations 603 21A . Logarithms for reducing Daily Variations ... 609 22. For ...
... Correction of the Sun's Declination , at Sea ..... 602 20. Correction of the Equation of Time , at Sea ..... 602 21. For reducing Daily and Twelve - hourly Variations 603 21A . Logarithms for reducing Daily Variations ... 609 22. For ...
Sivu xxi
... Correction of the Times in Table 27 .... 619 28. Correction of the Time of the Moon's Meridian Passage ... 29. Hour - angle and Altitude of a Body upon the Prime Vertical 619 620 30. Apparent Dip of the Sea Horizon 625 31. Mean ...
... Correction of the Times in Table 27 .... 619 28. Correction of the Time of the Moon's Meridian Passage ... 29. Hour - angle and Altitude of a Body upon the Prime Vertical 619 620 30. Apparent Dip of the Sea Horizon 625 31. Mean ...
Sivu xxii
... correcting the Lunar Distance for the Sphe- roidal Figure of the Earth ..... 647 LONGITUDE . 56. For computing the Moon's Second Correction of Distance .... 648 57. Correction of the Greenwich Mean Time for the Second Difference of the ...
... correcting the Lunar Distance for the Sphe- roidal Figure of the Earth ..... 647 LONGITUDE . 56. For computing the Moon's Second Correction of Distance .... 648 57. Correction of the Greenwich Mean Time for the Second Difference of the ...
Sivu xxiii
... Correction of the Latitude by Account 851 72. Logarithms for computing the Equation of Equal Altitudes .... 853 73. The Logarithmic Difference ... . 854 74. Proportional Logarithms . 863 APPENDIX . 878 INDEX TO THE MARITIME POSITIONS ...
... Correction of the Latitude by Account 851 72. Logarithms for computing the Equation of Equal Altitudes .... 853 73. The Logarithmic Difference ... . 854 74. Proportional Logarithms . 863 APPENDIX . 878 INDEX TO THE MARITIME POSITIONS ...
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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...