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- #1The sextant operates on the optical principle of double reflection, where reflecting a ray of light across two mirrors deflects it by twice the angle between the mirrors.
- #2The physical arc of a sextant spans sixty degrees (one-sixth of a circle), enabling observers to measure angular altitudes up to one hundred twenty degrees.
- #3John Hadley and Thomas Godfrey independently designed the precursor octant in 1731, utilizing an arc of forty-five degrees to measure angles up to ninety degrees.
- #4British instrument maker John Bird developed the first marine sextant in 1757 to accommodate wider angular measurements required for lunar distance calculations.
- #5Sighting Polaris provides direct geographic latitude in the Northern Hemisphere because the altitude of the celestial pole matches the observer's terrestrial latitude.
- #6Polaris deviates from the true celestial north pole by less than one degree, necessitating small ephemeris corrections tabulated in nautical tables.
- #7Local apparent noon occurs when the sun reaches its highest daily elevation at the observer's meridian, marking the optimal moment for solar latitude sights.
- #8The meridian altitude calculation subtracts observed solar altitude from ninety degrees to find zenith distance, then adds or subtracts solar declination.
- #9Index error arises from non-parallel alignment between the index mirror and horizon glass when the index arm is positioned precisely at zero degrees.
- #10Dip correction adjusts the measured angle for the height of the observer's eye above the geometric sea horizon due to the curvature of Earth.
- #11Atmospheric refraction bends light rays upward, making celestial bodies appear higher than their true geometric position, especially near the horizon.
- #12Semi-diameter correction adds or subtracts the angular radius of the sun or moon (approximately sixteen arcminutes) to reference the center of the celestial body.
- #13Longitude calculation relies on the Earth's rotational rate of fifteen degrees per hour, converting time difference from a prime meridian into angular distance.
- #14The British Parliament passed the Longitude Act of 1714, offering a twenty-thousand-pound reward to solve the challenge of calculating longitude at sea.
- #15John Harrison constructed the H4 marine chronometer in 1759, providing a clock capable of maintaining accurate Greenwich Mean Time aboard moving ships.
- #16Astronomer Royal Nevil Maskelyne initiated the publication of the Nautical Almanac in 1767 at the Royal Observatory in Greenwich to tabulate lunar distances.
- #17The Davis quadrant, invented by John Davis in 1595, allowed mariners to observe solar altitude with their back to the sun, preventing eye damage.
- #18Cloud cover and hazy ocean horizons represent severe operational impediments, preventing simultaneous observation of celestial targets and the sea boundary.
- #19Artificial horizons consisting of mercury basins or gyroscopic stabilizers permitted terrestrial and modern observers to take sextant sights without an oceanic horizon.
- #20The vernier scale and micrometer drum on modern sextants allow angular measurements to be resolved down to tenths of an arcminute (six arcseconds).
Subject Specialist Commentary
Analytical perspective & practical exam advice from the Master10 academic board
A marine sextant brings the sky down to the water. By bouncing starlight or sunlight off two small mirrors, the instrument lets a mariner see a celestial body and the sea horizon in one view. Measuring that angle reveals how high the star sits above the ocean. Since Polaris marks celestial north, its height directly tells you your latitude north of the equator.
For competitive examinations, never confuse latitude determination with longitude calculation. Latitude requires only an angle measurement from Polaris or a noon sun sight, whereas longitude demands an accurate timekeeper to compare local solar noon against Greenwich time. To master the operational steps and corrections of celestial sights, remember the mnemonic SEXTANT: Sight target, Error index check, X-axis horizon dip, True refraction adjustment, Altitude zenith subtraction, Nautical declination lookup, and Time conversion for longitude.
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