Terrestrial equator

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In red the equatorial line on the globe.
World map with the equatorial line.

The terrestrial equator, also called the line of the equator or parallel 0°, is the great perpendicular circle to the axis of rotation of the planet Earth. Like any great circle, it defines a plane that passes through the center. It divides the planet into the northern and southern hemispheres and is located at the same distance from the geographic poles. By definition, the latitude of the Earth's equator is 0°. The equatorial radius is 6,378.1 km and the corresponding circumference is 40,075 km.

Astronomy and geodesy

The Sun, in its apparent movement, passes through the equatorial plane twice a year (on the March and September equinoxes), moments in which the sun's rays are perpendicular to the Earth's surface on the equator, that is, the Sun is located at the zenith of the observer.

In the regions located on the Earth's equatorial line, the duration of sunrise and sunset is shorter than in the rest of the planet, due to the fact that, throughout the year, the Sun "appears" and "hides" almost vertically. The duration of the day on the equator is practically constant throughout the year: approximately 14 minutes longer than the night, caused by atmospheric refraction and because the sunrise and sunset are not determined by the passage of the center of the Sun above the horizon, but by passing the edge of the solar disk. Therefore, the moment of sunrise precedes the passage of the center of the sun over the horizon, and sunset is after the passage of the center of the Sun over the horizon line.

At the equator, the Earth widens slightly. The average diameter of the planet is 12,750 kilometers. The equatorial radius is 43 kilometers greater than the result of measuring it passing through the poles.

Places close to the line are more suitable for the location of spaceports, such as the Guiana Space Center, located in Kourou (French Guiana) France, because its movement due to the Earth's rotation is faster compared to other latitudes, since this addition of speed requires less fuel to launch spacecraft. To take advantage of this fact, casts should be directed to the east, southeast, or northeast.

The latitude of the equator is by definition 0° (zero degrees). It is the only one of the five notable circles at Earth's latitude that is strictly a circle, as is the imaginary line that results from its projection on the celestial sphere. The other four notable "circles" are the two polar circles and the two tropical circles (Tropic of Cancer in the Northern Hemisphere and Tropic of Capricorn in the Southern Hemisphere).

Magnetic field

Earth's outer core produces Earth's magnetic field that extends into the magnetosphere. On the earth's surface, this field guides the compass needles. The field strength at the surface is not constant. It is maximum near the poles and minimum near the Earth's equator, thus defining a magnetic equator that roughly follows the geographic equator. The point where the magnetic equator is furthest from the geographic one is in South America, related to the South Atlantic Anomaly.

Climate

The rainy tropical climate Af (blue) predominates in the land equator.

The seasons of the year in the tropics and on the equator differ significantly from the seasons in the temperate and polar zones. In many tropical regions, only two seasons are identified, one of rain and the other of drought, but most places near the equator are rainy throughout the year. However, the seasons can vary depending on a variety of factors, including elevation, winds, and proximity to the ocean.

Meteorologists define a place's climate as "equatorial" rather than "tropical" if the difference between the normal temperatures of the warmest and coldest months is less than 2°C and year-round abundant and constant rains.

Climate Equators

Map of climate equator: in red the thermal equator, in blue the belt of tropical rains, in yellow the zone of equatorial calms and in green the weather equator.

The terrestrial equator has climatic characteristics that imply high temperatures, abundant rainfall, gentle winds, and low pressure, which are indicators of a rainy equatorial climate. However, the annual maximum longitudinal climatic means of these values have their own trajectory due to climatic differences in both hemispheres of the Earth. The northern hemisphere has the largest surface area of the continents and landmass, so it tends to warm at a greater rate than the southern hemisphere, which is why these equatorial climate indicators are more frequently located in the northern hemisphere; although during the year they actually migrate from one hemisphere to the other.

The following climatic equators have been defined:

Geographic features

Countries where the line (red) and the meridian zero (blue) is located.

The surface of the Earth crossed by the equator line is mostly oceanic. The equator line passes through the following countries:

Monument on the fictitious equatorial line in Cayambe (Ecuador).