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Msf dating does mean

Msf dating does mean

History of longitude Amerigo Vespucci's means of determining longitude The measurement of longitude is important both to cartography and for ocean navigation. Mariners and explorers for most of history struggled to determine longitude. Finding a method of determining longitude took centuries, resulting in the history of longitude recording the effort of some of the greatest scientific minds. Latitude was calculated by observing with quadrant or astrolabe the altitude of the sun or of charted stars above the horizon, but longitude is harder.

Amerigo Vespucci was perhaps the first European to proffer a solution, after devoting a great deal of time and energy studying the problem during his sojourns in the New World: As to longitude, I declare that I found so much difficulty in determining it that I was put to great pains to ascertain the east-west distance I had covered. The final result of my labours was that I found nothing better to do than to watch for and take observations at night of the conjunction of one planet with another, and especially of the conjunction of the moon with the other planets, because the moon is swifter in her course than any other planet.

I compared my observations with an almanac. After I had made experiments many nights, one night, the twenty-third of August , there was a conjunction of the moon with Mars, which according to the almanac was to occur at midnight or a half hour before.

But this method had several limitations: First, it required the occurrence of a specific astronomical event in this case, Mars passing through the same right ascension as the moon , and the observer needed to anticipate this event via an astronomical almanac. One needed also to know the precise time, which was difficult to ascertain in foreign lands.

Finally, it required a stable viewing platform, rendering the technique useless on the rolling deck of a ship at sea. See Lunar distance navigation. In Galileo Galilei demonstrated that with sufficiently accurate knowledge of the orbits of the moons of Jupiter one could use their positions as a universal clock and this would make possible the determination of longitude, but the method he devised was impracticable for navigators on ships because of their instability.

These rewards motivated many to search for a solution. Drawing of Earth with longitudes but without latitudes. John Harrison , a self-educated English clockmaker , invented the marine chronometer , the key piece in solving the problem of accurately establishing longitude at sea, thus revolutionising and extending the possibility of safe long distance sea travel.

Finally, the combination of the availability of marine chronometers and wireless telegraph time signals put an end to the use of lunars in the 20th century. Unlike latitude, which has the equator as a natural starting position, there is no natural starting position for longitude. Therefore, a reference meridian had to be chosen. It was a popular practice to use a nation's capital as the starting point, but other locations were also used. In the International Meridian Conference adopted the Greenwich meridian as the universal Prime Meridian or zero point of longitude.

Each degree of longitude is sub-divided into 60 minutes , each of which is divided into 60 seconds. For higher precision, the seconds are specified with a decimal fraction. An alternative representation uses degrees and minutes, where parts of a minute are expressed in decimal notation with a fraction, thus: Degrees may also be expressed as a decimal fraction: Confusingly, the convention of negative for East is also sometimes seen. The preferred convention—that East is positive—is consistent with a right-handed Cartesian coordinate system , with the North Pole up.

A specific longitude may then be combined with a specific latitude usually positive in the northern hemisphere to give a precise position on the Earth's surface.

There is no other physical principle determining longitude directly but with time. Longitude at a point may be determined by calculating the time difference between that at its location and Coordinated Universal Time UTC.

In order to perform this calculation, however, a person needs to have a chronometer watch set to UTC and needs to determine local time by solar or astronomical observation. The details are more complex than described here: Singularity and discontinuity of longitude[ edit ] Note that the longitude is singular at the Poles and calculations that are sufficiently accurate for other positions, may be inaccurate at or near the Poles. An example is a calculation of east displacement by subtracting two longitudes, which gives the wrong answer if the two positions are on either side of this meridian.

To avoid these complexities, consider replacing latitude and longitude with another horizontal position representation in calculation. Plate movement and longitude[ edit ] The Earth's tectonic plates move relative to one another in different directions at speeds on the order of 50 to mm per year. For example, the longitudinal difference between a point on the Equator in Uganda, on the African Plate , and a point on the Equator in Ecuador, on the South American Plate , is increasing by about 0.

These tectonic movements likewise affect latitude. If a global reference frame such as WGS84 , for example is used, the longitude of a place on the surface will change from year to year. To minimize this change, when dealing just with points on a single plate, a different reference frame can be used, whose coordinates are fixed to a particular plate, such as " NAD83 " for North America or " ETRS89 " for Europe.

Length of a degree of longitude[ edit ] The length of a degree of longitude east-west distance depends only on the radius of a circle of latitude.

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Msf dating does mean

History of longitude Amerigo Vespucci's means of determining longitude The measurement of longitude is important both to cartography and for ocean navigation. Mariners and explorers for most of history struggled to determine longitude. Finding a method of determining longitude took centuries, resulting in the history of longitude recording the effort of some of the greatest scientific minds. Latitude was calculated by observing with quadrant or astrolabe the altitude of the sun or of charted stars above the horizon, but longitude is harder.

Amerigo Vespucci was perhaps the first European to proffer a solution, after devoting a great deal of time and energy studying the problem during his sojourns in the New World: As to longitude, I declare that I found so much difficulty in determining it that I was put to great pains to ascertain the east-west distance I had covered.

The final result of my labours was that I found nothing better to do than to watch for and take observations at night of the conjunction of one planet with another, and especially of the conjunction of the moon with the other planets, because the moon is swifter in her course than any other planet. I compared my observations with an almanac. After I had made experiments many nights, one night, the twenty-third of August , there was a conjunction of the moon with Mars, which according to the almanac was to occur at midnight or a half hour before.

But this method had several limitations: First, it required the occurrence of a specific astronomical event in this case, Mars passing through the same right ascension as the moon , and the observer needed to anticipate this event via an astronomical almanac.

One needed also to know the precise time, which was difficult to ascertain in foreign lands. Finally, it required a stable viewing platform, rendering the technique useless on the rolling deck of a ship at sea. See Lunar distance navigation. In Galileo Galilei demonstrated that with sufficiently accurate knowledge of the orbits of the moons of Jupiter one could use their positions as a universal clock and this would make possible the determination of longitude, but the method he devised was impracticable for navigators on ships because of their instability.

These rewards motivated many to search for a solution. Drawing of Earth with longitudes but without latitudes. John Harrison , a self-educated English clockmaker , invented the marine chronometer , the key piece in solving the problem of accurately establishing longitude at sea, thus revolutionising and extending the possibility of safe long distance sea travel.

Finally, the combination of the availability of marine chronometers and wireless telegraph time signals put an end to the use of lunars in the 20th century. Unlike latitude, which has the equator as a natural starting position, there is no natural starting position for longitude.

Therefore, a reference meridian had to be chosen. It was a popular practice to use a nation's capital as the starting point, but other locations were also used. In the International Meridian Conference adopted the Greenwich meridian as the universal Prime Meridian or zero point of longitude.

Each degree of longitude is sub-divided into 60 minutes , each of which is divided into 60 seconds. For higher precision, the seconds are specified with a decimal fraction. An alternative representation uses degrees and minutes, where parts of a minute are expressed in decimal notation with a fraction, thus: Degrees may also be expressed as a decimal fraction: Confusingly, the convention of negative for East is also sometimes seen.

The preferred convention—that East is positive—is consistent with a right-handed Cartesian coordinate system , with the North Pole up. A specific longitude may then be combined with a specific latitude usually positive in the northern hemisphere to give a precise position on the Earth's surface. There is no other physical principle determining longitude directly but with time. Longitude at a point may be determined by calculating the time difference between that at its location and Coordinated Universal Time UTC.

In order to perform this calculation, however, a person needs to have a chronometer watch set to UTC and needs to determine local time by solar or astronomical observation. The details are more complex than described here: Singularity and discontinuity of longitude[ edit ] Note that the longitude is singular at the Poles and calculations that are sufficiently accurate for other positions, may be inaccurate at or near the Poles.

An example is a calculation of east displacement by subtracting two longitudes, which gives the wrong answer if the two positions are on either side of this meridian. To avoid these complexities, consider replacing latitude and longitude with another horizontal position representation in calculation.

Plate movement and longitude[ edit ] The Earth's tectonic plates move relative to one another in different directions at speeds on the order of 50 to mm per year. For example, the longitudinal difference between a point on the Equator in Uganda, on the African Plate , and a point on the Equator in Ecuador, on the South American Plate , is increasing by about 0.

These tectonic movements likewise affect latitude. If a global reference frame such as WGS84 , for example is used, the longitude of a place on the surface will change from year to year. To minimize this change, when dealing just with points on a single plate, a different reference frame can be used, whose coordinates are fixed to a particular plate, such as " NAD83 " for North America or " ETRS89 " for Europe.

Length of a degree of longitude[ edit ] The length of a degree of longitude east-west distance depends only on the radius of a circle of latitude.

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