Longitude

Longitude is a way to describe a place's position on Earth from east to west. It is like a line that goes from the North Pole to the South Pole. All places along that line share the same longitude. These lines are called meridians.

The most important meridian is called the prime meridian. It passes near a place called the Royal Observatory in Greenwich, in Great Britain.

Longitude helps us understand time because the Earth rotates. For every 15 degrees of longitude you move east or west, the time changes by one hour. This means if you know the time somewhere and you know its longitude, you can figure out the time at another place by comparing their longitudes.

Knowing longitude is very important for navigation, mapping, and many scientific studies. It helps us pinpoint exactly where we are on the whole wide Earth.

History

Main article: History of longitude

The idea of longitude started with ancient Greek astronomers. Hipparchus, who lived in the 2nd century BC, was the first to use degrees to describe places on Earth. He also suggested using lunar eclipses to figure out longitude by comparing times at different places.

Later, Claudius Ptolemy improved mapping methods and collected data from many places. During the Middle Ages, interest in geography grew with more travel and new ideas from other cultures. Explorers like Christopher Columbus tried to use lunar eclipses to find their position, but often made mistakes.

Important inventions like the telescope and the pendulum clock helped improve these measurements. Over time, new tools such as the chronometers invented by John Harrison and later, radio signals and GPS, made figuring out longitude much easier and more accurate, especially for sailors at sea.

Determination

There are several ways people have figured out longitude, which tells us how far east or west a place is. Most of these methods rely on comparing time at two different places. Since the Earth turns, time differences can help us find longitude.

One old method used the Moon's movement in the sky. By measuring the angle between the Moon and stars, sailors could find the time at a faraway place, like Greenwich. Another method watched the moons of Jupiter through telescopes. Clocks carried on ships, called chronometers, also helped by comparing local time to the time at the starting point. Later, telegraph lines let people send time signals across long distances, improving maps and navigation.

Values

Longitude is a way to describe a place’s position from east to west on Earth. It is measured in degrees, with 0° at the Prime Meridian. Longitude can range from −180° to +180°. We use the Greek letter λ (lambda) to show a place’s longitude.

Each degree is divided into 60 minutes, and each minute into 60 seconds. For example, a longitude might be written as 23° 27′ 30″ E. Sometimes, we use decimal numbers to make it easier, like 23.45833° E. For math, we can change degrees into radians.

Length of a degree of longitude

See also: Length of a degree of latitude

The distance between two points that are 1 degree apart in longitude changes depending on where you are on Earth. Near the equator, a degree of longitude is longest. It gets shorter as you move closer to the poles. This happens because the circles of latitude — the imaginary lines running around Earth — get smaller as you move away from the equator toward the poles.

At the equator, one degree of longitude is about 111 kilometers or 69 miles long. This distance becomes smaller as you move toward the poles. This is different from latitude, where the distance between degrees stays almost the same everywhere.