Equator

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World location map (equirectangular 180).svg
Equator in the map of Earth
Countries and territories that touch the Equator (red) or the prime meridian (blue) Equator and Prime Meridian.svg
Countries and territories that touch the Equator (red) or the prime meridian (blue)

Earth's Equator (spelled with capital E) is a specific case of a planetary equator. It is about 40,075 km (24,901 mi) long, of which 78.8% lies across water and 21.3% over land.[ citation needed ]

Contents

In spatial (3D) geometry, as applied in astronomy, the equator of a rotating spheroid (such as a planet) is the parallel (circle of latitude) at which latitude is defined to be 0°. It is the imaginary line on the spheroid, equidistant from its poles, dividing it into northern and southern hemispheres. In other words, it is the intersection of the spheroid with the plane perpendicular to its axis of rotation and midway between its geographical poles.

When the Sun is directly above the Earth's Equator (on the equinoxes of approximately March 20 and September 23), sunlight shines perpendicular to the Earth's axis of rotation, and all latitudes have a 12-hour day and 12-hour night. On and near the Equator sunlight comes from almost directly above every day year-round, and thus the Equator has a rather stable daytime temperature the whole year.

Etymology

The name is derived from medieval Latin word aequator, in the phrase circulus aequator diei et noctis, meaning 'circle equalizing day and night', from the Latin word aequare meaning 'make equal'. [1]

Overview

Equator monument.jpg
Equator sign kenya.jpg
Left: A monument marking the equator near the city of Pontianak, Indonesia
Right: Road sign marking the equator near Nanyuki, Kenya

The latitude of the Earth's equator is, by definition, 0° (zero degrees) of arc. The equator is one of the five notable circles of latitude on Earth; the other four are both polar circles (the Arctic Circle and the Antarctic Circle) and both tropical circles (the Tropic of Cancer and the Tropic of Capricorn). The equator is the only line of latitude which is also a great circle—that is, one whose plane passes through the center of the globe. The plane of Earth's equator, when projected outwards to the celestial sphere, defines the celestial equator.

In the cycle of Earth's seasons, the equatorial plane runs through the Sun twice per year: on the equinoxes in March and September. To a person on Earth, the Sun appears to travel above the equator (or along the celestial equator) at these times. Light rays from the Sun's center are perpendicular to Earth's surface at the point of solar noon on the equator.

The equator marked as it crosses Ilheu das Rolas, in Sao Tome and Principe Equator Sao Tome.jpg
The equator marked as it crosses Ilhéu das Rolas, in São Tomé and Príncipe
The Marco Zero monument marking the equator in Macapa, Brazil Equator Line Monument, Macapa city, Brazil.jpg
The Marco Zero monument marking the equator in Macapá, Brazil

Locations on the equator experience the shortest sunrises and sunsets because the Sun's daily path is nearly perpendicular to the horizon for most of the year. The length of daylight (sunrise to sunset) is almost constant throughout the year; it is about 14 minutes longer than nighttime due to atmospheric refraction and the fact that sunrise begins (or sunset ends) as the upper limb, not the center, of the Sun's disk contacts the horizon.

Earth bulges slightly at the equator; the "average" diameter of Earth is 12,750 km (7,922 mi), but the diameter at the equator is about 43 km (27 mi) greater than at the poles. [2]

Sites near the equator, such as the Guiana Space Centre in Kourou, French Guiana, are good locations for spaceports as they have a fastest rotational speed of any latitude, 460 m (1,509 ft)/sec. The added velocity reduces the fuel needed to launch spacecraft eastward (in the direction of Earth's rotation) to orbit, while simultaneously avoiding costly maneuvers to flatten inclination during missions such as the Apollo moon landings. [3]

Geodesy

Precise location

The precise location of the equator is not truly fixed; the true equatorial plane is perpendicular to the Earth's rotation axis, which drifts about 9 metres (30 ft) during a year. This effect must be accounted for in detailed geophysical measurements.[ citation needed ]

Geological samples show the equator significantly changed positions between 12 and 48 million years ago, as sediment deposited by ocean thermal currents at the equator have shifted. The deposits by thermal currents are determined by the axis of the earth, which determines solar coverage of the Earth's surface. Changes in Earth axis can also be observed in the geographic layout of volcanic island chains, which are created by shifting hot spots under the Earth's crust as the axis and crust move. [4] This correlates with Indian plate crashing into Asia and Himalayan uplift.

Exact length

The International Association of Geodesy (IAG) and the International Astronomical Union (IAU) have chosen to use an equatorial radius of 6,378.1366 km (3,963.1903 mi) (codified as the IAU 2009 value). [5] This equatorial radius is also in the 2003 and 2010 IERS Conventions. [6] It is also the equatorial radius used for the IERS 2003 ellipsoid. If it were really circular, the length of the equator would then be exactly 2π times the radius, namely 40,075.0142 km (24,901.4594 mi). The GRS 80 (Geodetic Reference System 1980) as approved and adopted by the IUGG at its Canberra, Australia meeting of 1979 has an equatorial radius of 6,378.137 km (3,963.191 mi). The WGS 84 (World Geodetic System 1984) which is a standard for use in cartography, geodesy, and satellite navigation including GPS, also has an equatorial radius of 6,378.137 km (3,963.191 mi). For both GRS 80 and WGS 84, this results in a length for the equator of 40,075.0167 km (24,901.4609 mi).

The geographical mile is defined as one arc-minute of the equator, so it has different values depending on which radius is assumed. For example, by WSG-84, the distance is 1,855.3248 metres (6,087.024 ft), while by IAU-2000, it is 1,855.3257 metres (6,087.027 ft). This is a difference of less than one millimetre (0.039 in) over the total distance (approximately 1.86 kilometres or 1.16 miles).

The earth is commonly modeled as a sphere flattened 0.336% along its axis. This makes the equator 0.16% longer than a meridian (a great circle passing through the two poles). The IUGG standard meridian is, to the nearest millimetre, 40,007.862917 kilometres (24,859.733480 mi), one arc-minute of which is 1,852.216 metres (6,076.82 ft), explaining the SI standardization of the nautical mile as 1,852 metres (6,076 ft), more than 3 metres (9.8 ft) less than the geographical mile.

The sea-level surface of the Earth (the geoid) is irregular, so the actual length of the equator is not so easy to determine. Aviation Week and Space Technology on 9 October 1961 reported that measurements using the Transit IV-A satellite had shown the equatorial diameter from longitude 11° West to 169° East to be 1,000 feet (305 m) greater than its diameter ninety degrees away.[ citation needed ]

Equatorial countries and territories

Map all coordinates using: OpenStreetMap  
Download coordinates as: KML  ·  GPX
GPS reading taken on the equator close to the Quitsato Sundial, in Cayambe, Ecuador ECSundialGPS.jpg
GPS reading taken on the equator close to the Quitsato Sundial, in Cayambe, Ecuador

The equator passes through the land of 11 countries. Indonesia is the country straddling the greatest length of the equatorial line across both land and sea. Starting at the Prime Meridian and heading eastwards, the equator passes through:

Co-ordinatesCountry, territory or seaNotes
0°N0°E / 0°N 0°E / 0; 0 (Prime Meridian) Atlantic Ocean Gulf of Guinea, "Null Island"
0°0′N6°31′E / 0.000°N 6.517°E / 0.000; 6.517 (São Tomé and Príncipe) Flag of Sao Tome and Principe.svg  São Tomé and Príncipe Passing through Pestana Equador resort on the Ilhéu das Rolas
0°0′N9°21′E / 0.000°N 9.350°E / 0.000; 9.350 (Gabon) Flag of Gabon.svg  Gabon Passing 8.9 km (5.5 mi) south of Ayem, 10.6 km (6.6 mi) north of Mayene, Booue
0°0′N13°56′E / 0.000°N 13.933°E / 0.000; 13.933 (Republic of the Congo) Flag of the Republic of the Congo.svg  Republic of the Congo Passing through the town of Makoua.
0°0′N17°46′E / 0.000°N 17.767°E / 0.000; 17.767 (Democratic Republic of the Congo) Flag of the Democratic Republic of the Congo.svg  Democratic Republic of the Congo Passing 9 km (5.6 mi) south of central Butembo
0°0′N29°43′E / 0.000°N 29.717°E / 0.000; 29.717 (Uganda) Flag of Uganda.svg  Uganda Passing 32 km (20 mi) south of central Kampala
0°0′N32°22′E / 0.000°N 32.367°E / 0.000; 32.367 (Lake Victoria) Lake Victoria Passing through some islands of Flag of Uganda.svg  Uganda in Mukono District and Namayingo District
0°0′N34°0′E / 0.000°N 34.000°E / 0.000; 34.000 (Kenya) Flag of Kenya.svg  Kenya Passing 6 km (3.7 mi) north of central Kisumu
0°0′N41°0′E / 0.000°N 41.000°E / 0.000; 41.000 (Somalia) Flag of Somalia.svg  Somalia Passing south of Jamame
0°0′N42°53′E / 0.000°N 42.883°E / 0.000; 42.883 (Indian Ocean) Indian Ocean Passing between Huvadhu Atoll and Fuvahmulah of the Flag of Maldives.svg  Maldives
0°0′N98°12′E / 0.000°N 98.200°E / 0.000; 98.200 (Indonesia) Flag of Indonesia.svg  Indonesia North Sumatra (including the Batu Islands) and Lingga Regency, Riau Islands
0°0′N104°34′E / 0.000°N 104.567°E / 0.000; 104.567 (Karimata Strait) Karimata Strait
0°0′N109°9′E / 0.000°N 109.150°E / 0.000; 109.150 (Indonesia) Flag of Indonesia.svg  Indonesia Bornean provinces of West Kalimantan (passing through province capital Pontianak), Central Kalimantan, and East Kalimantan
0°0′N117°30′E / 0.000°N 117.500°E / 0.000; 117.500 (Makassar Strait) Makassar Strait
0°0′N119°40′E / 0.000°N 119.667°E / 0.000; 119.667 (Indonesia) Flag of Indonesia.svg  Indonesia Donggala & Parigi Moutong Regency, Central Sulawesi (Celebes)
0°0′N120°5′E / 0.000°N 120.083°E / 0.000; 120.083 (Gulf of Tomini) Gulf of Tomini
0°0′N124°0′E / 0.000°N 124.000°E / 0.000; 124.000 (Molucca Sea) Molucca Sea
0°0′N127°24′E / 0.000°N 127.400°E / 0.000; 127.400 (Indonesia) Flag of Indonesia.svg  Indonesia Kayoa and Halmahera islands, North Maluku
0°0′N127°53′E / 0.000°N 127.883°E / 0.000; 127.883 (Halmahera Sea) Halmahera Sea
0°0′N129°20′E / 0.000°N 129.333°E / 0.000; 129.333 (Indonesia) Flag of Indonesia.svg  Indonesia Gebe and Kawe islands, West Papua
0°0′N129°21′E / 0.000°N 129.350°E / 0.000; 129.350 (Pacific Ocean) Pacific Ocean Passing between Aranuka and Nonouti atolls, Flag of Kiribati.svg  Kiribati (at 0°0′N173°40′E / 0.000°N 173.667°E / 0.000; 173.667 )

Passing just south of Baker Island, and just north of Jarvis Island, Flag of the United States.svg  United States Minor Outlying Islands

0°0′N80°6′W / 0.000°N 80.100°W / 0.000; -80.100 (Ecuador) Flag of Ecuador.svg  Ecuador Passing 24 km (15 mi) north of central Quito, near Mitad del Mundo, and precisely at the location of Catequilla, a pre-Columbian ruin. Also, Isabela Island in the Galápagos Islands
0°0′N75°32′W / 0.000°N 75.533°W / 0.000; -75.533 (Colombia) Flag of Colombia.svg  Colombia Passing 4.3 km (2.7 mi) north of the border with Peru
0°0′N70°3′W / 0.000°N 70.050°W / 0.000; -70.050 (Brazil) Flag of Brazil.svg  Brazil Amazonas, Roraima, Pará, Amapá (passing slightly south of the city center of the state capital Macapá, and precisely at the Marco Zero monument and the Avenue Equatorial)
0°0′N49°21′W / 0.000°N 49.350°W / 0.000; -49.350 (Atlantic Ocean) Atlantic Ocean At the Perigoso Canal (sv) on the mouth of the Amazon River

Despite its name, no part of Equatorial Guinea lies on the equator. However, its island of Annobón is 155 km (96 mi) south of the equator, and the rest of the country lies to the north.

Equatorial seasons and climate

Diagram of the seasons, depicting the situation at the December solstice. Regardless of the time of day (i.e. the Earth's rotation on its axis), the North Pole will be dark, and the South Pole will be illuminated; see also arctic winter. In addition to the density of incident light, the dissipation of light in the atmosphere is greater when it falls at a shallow angle. Seasons.svg

Diagram of the seasons, depicting the situation at the December solstice. Regardless of the time of day (i.e. the Earth's rotation on its axis), the North Pole will be dark, and the South Pole will be illuminated; see also arctic winter. In addition to the density of incident light, the dissipation of light in the atmosphere is greater when it falls at a shallow angle.

Seasons result from the tilt of the Earth's axis compared to the plane of its revolution around the Sun. Throughout the year, the northern and southern hemispheres are alternately turned either toward or away from the sun depending on Earth's position in its orbit. The hemisphere turned toward the sun receives more sunlight and is in summer, while the other hemisphere receives less sun and is in winter (see solstice).

At the equinoxes, the Earth's axis is perpendicular to the sun rather than tilted toward or away, meaning that day and night are both about 12 hours long across the whole of the Earth.

Near the equator, this means the variation in strength of solar radiation is different relative to the time of year than it is at higher latitudes: Maximum solar radiation is received during the equinoxes, when a place at the equator is under the subsolar point at high noon, and the intermediate seasons of spring and autumn occur at higher latitudes, and the minimum occurs during both solstices, when either pole is tilted towards or away from the sun, resulting in either summer or winter in both hemispheres. This also results in a corresponding movement of the equator away from the subsolar point, which is then situated over or near the relevant tropic circle. Nevertheless, temperatures are high year round due to the earth's axial tilt of 23.5° not being enough to create a low minimum midday declination to sufficiently weaken the sun's rays even during the solstices.

Near the equator, there is little temperature change throughout the year, though there may be dramatic differences in rainfall and humidity. The terms summer, autumn, winter and spring do not generally apply. Lowlands around the equator generally have a tropical rainforest climate, also known as an equatorial climate, though cold ocean currents cause some regions to have tropical monsoon climates with a dry season in the middle of the year, and the Somali Current generated by the Asian monsoon due to continental heating via the high Tibetan Plateau causes Greater Somalia to have an arid climate despite its equatorial location.

Average annual temperatures in equatorial lowlands are around 31 °C (88 °F) during the afternoon and 23 °C (73 °F) around sunrise. Rainfall is very high away from cold ocean current upwelling zones, from 2,500 to 3,500 mm (100 to 140 in) per year. There are about 200 rainy days per year and average annual sunshine hours are around 2,000. Despite high year-round sea level temperatures, some higher altitudes such as the Andes and Mount Kilimanjaro have glaciers. The highest point on the equator is at the elevation of 4,690 metres (15,387 ft), at 0°0′0″N77°59′31″W / 0.00000°N 77.99194°W / 0.00000; -77.99194 (highest point on the equator) , found on the southern slopes of Volcán Cayambe [summit 5,790 metres (18,996 ft)] in Ecuador. This is slightly above the snow line and is the only place on the equator where snow lies on the ground. At the equator, the snow line is around 1,000 metres (3,300 ft)lower than on Mount Everest and as much as 2,000 metres (6,600 ft) lower than the highest snow line in the world, near the Tropic of Capricorn on Llullaillaco.

Climate data for Macapá, Brazil in South America
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Average high °C (°F)29.7
(85.5)
29.2
(84.6)
29.3
(84.7)
29.5
(85.1)
30.0
(86.0)
30.3
(86.5)
30.6
(87.1)
31.5
(88.7)
32.1
(89.8)
32.6
(90.7)
32.3
(90.1)
31.4
(88.5)
30.71
(87.28)
Daily mean °C (°F)26.5
(79.7)
26.2
(79.2)
26.3
(79.3)
26.4
(79.5)
26.8
(80.2)
26.8
(80.2)
26.8
(80.2)
27.4
(81.3)
27.8
(82.0)
28.1
(82.6)
27.9
(82.2)
27.4
(81.3)
27.03
(80.65)
Average low °C (°F)23.0
(73.4)
23.1
(73.6)
23.2
(73.8)
23.5
(74.3)
23.5
(74.3)
23.2
(73.8)
22.9
(73.2)
23.3
(73.9)
23.4
(74.1)
23.5
(74.3)
23.5
(74.3)
23.4
(74.1)
23.29
(73.92)
Average rainfall mm (inches)299.6
(11.80)
347.0
(13.66)
407.2
(16.03)
384.3
(15.13)
351.5
(13.84)
220.1
(8.67)
184.8
(7.28)
98.0
(3.86)
42.6
(1.68)
35.5
(1.40)
58.4
(2.30)
142.5
(5.61)
2,571.5
(101.26)
Average rainy days (≥ 0.1 mm)232224242522191365614203
Mean monthly sunshine hours 148.8113.1108.5114.0151.9189.0226.3272.8273.0282.1252.0204.62,336.1
Source: World Meteorological Organization (UN), [8] Hong Kong Observatory [9]
Climate data for Pontianak, Indonesia in Asia
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Average high °C (°F)32.4
(90.3)
32.7
(90.9)
32.9
(91.2)
33.2
(91.8)
33.0
(91.4)
33.2
(91.8)
32.9
(91.2)
33.4
(92.1)
32.6
(90.7)
32.6
(90.7)
32.2
(90.0)
32.0
(89.6)
32.7
(90.9)
Daily mean °C (°F)27.6
(81.7)
27.7
(81.9)
28.0
(82.4)
28.2
(82.8)
28.2
(82.8)
28.2
(82.8)
27.7
(81.9)
27.9
(82.2)
27.6
(81.7)
27.7
(81.9)
27.4
(81.3)
27.2
(81.0)
27.7
(81.9)
Average low °C (°F)22.7
(72.9)
22.6
(72.7)
23.0
(73.4)
23.2
(73.8)
23.4
(74.1)
23.1
(73.6)
22.5
(72.5)
22.3
(72.1)
22.6
(72.7)
22.8
(73.0)
22.6
(72.7)
22.4
(72.3)
22.7
(72.9)
Average rainfall mm (inches)260
(10.2)
215
(8.5)
254
(10.0)
292
(11.5)
256
(10.1)
212
(8.3)
201
(7.9)
180
(7.1)
295
(11.6)
329
(13.0)
400
(15.7)
302
(11.9)
3,196
(125.8)
Average rainy days (≥ 0.1 mm)151321222018162514272522238
Source: World Meteorological Organization (UN) [10]
Climate data for Libreville, Gabon in Africa
MonthJanFebMarAprMayJunJulAugSepOctNovDecYear
Average high °C (°F)29.5
(85.1)
30.0
(86.0)
30.2
(86.4)
30.1
(86.2)
29.4
(84.9)
27.6
(81.7)
26.4
(79.5)
26.8
(80.2)
27.5
(81.5)
28.0
(82.4)
28.4
(83.1)
29.0
(84.2)
28.58
(83.44)
Daily mean °C (°F)26.8
(80.2)
27.0
(80.6)
27.1
(80.8)
26.6
(79.9)
26.7
(80.1)
25.4
(77.7)
24.3
(75.7)
24.3
(75.7)
25.4
(77.7)
25.7
(78.3)
25.9
(78.6)
26.2
(79.2)
25.95
(78.71)
Average low °C (°F)24.1
(75.4)
24.0
(75.2)
23.9
(75.0)
23.1
(73.6)
24.0
(75.2)
23.2
(73.8)
22.1
(71.8)
21.8
(71.2)
23.2
(73.8)
23.4
(74.1)
23.4
(74.1)
23.4
(74.1)
23.30
(73.94)
Average rainfall mm (inches)250.3
(9.85)
243.1
(9.57)
363.2
(14.30)
339.0
(13.35)
247.3
(9.74)
54.1
(2.13)
6.6
(0.26)
13.7
(0.54)
104.0
(4.09)
427.2
(16.82)
490.0
(19.29)
303.2
(11.94)
2,841.7
(111.88)
Average rainy days (≥ 0.1 mm)17.914.819.519.216.03.701.704.9014.525.022.617.6177.4
Mean monthly sunshine hours 176.7182.7176.7177.0158.1132.0117.889.9096.00111.6135.0167.41,720.9
Source: World Meteorological Organization (UN), [11] Hong Kong Observatory [12]

Line crossing ceremonies

There is a widespread maritime tradition of holding ceremonies to mark a sailor's first crossing of the equator. In the past, these ceremonies have been notorious for their brutality, especially in naval practice. [ citation needed ] Milder line-crossing ceremonies, typically featuring King Neptune, are also held for passengers' entertainment on some civilian ocean liners and cruise ships.[ citation needed ]

See also

Related Research Articles

Declination Astronomical coordinate analogous to latitude

In astronomy, declination is one of the two angles that locate a point on the celestial sphere in the equatorial coordinate system, the other being hour angle. Declination's angle is measured north or south of the celestial equator, along the hour circle passing through the point in question.

Ecliptic Apparent path of the Sun on the celestial sphere

The ecliptic is the plane of Earth's orbit around the Sun. From the perspective of an observer on Earth, the Sun's movement around the celestial sphere over the course of a year traces out a path along the ecliptic against the background of stars. The ecliptic is an important reference plane and is the basis of the ecliptic coordinate system.

Equinox semi-annual astronomical event where the Sun is directly above the Earths equator

An equinox is commonly regarded as the instant of time when the plane of Earth's equator passes through the geometric center of the Sun's disk. This occurs twice each year, around 20 March and 23 September. In other words, it is the moment at which the center of the visible Sun is directly above the equator.

Latitude geographic coordinate specifying north–south position

In geography, latitude is a geographic coordinate that specifies the north–south position of a point on the Earth's surface. Latitude is an angle which ranges from 0° at the Equator to 90° at the poles. Lines of constant latitude, or parallels, run east–west as circles parallel to the equator. Latitude is used together with longitude to specify the precise location of features on the surface of the Earth. On its own, the term latitude should be taken to be the geodetic latitude as defined below. Briefly, geodetic latitude at a point is the angle formed by the vector perpendicular to the ellipsoidal surface from that point, and the equatorial plane. Also defined are six auxiliary latitudes that are used in special applications.

Northern Hemisphere Half of Earth that is north of the equator

The Northern Hemisphere is the top half of Earth that is north of the Equator. For other planets in the Solar System, north is defined as being in the same celestial hemisphere relative to the invariable plane of the solar system as Earth's North Pole.

A solstice is an event that occurs when the Sun appears to reach its most northerly or southerly excursion relative to the celestial equator on the celestial sphere. Two solstices occur annually, around June 21 and December 21. In many countries, the seasons of the year are determined by reference to the solstices and the equinoxes.

Equatorial coordinate system celestial coordinate system used to specify the positions of celestial objects

The equatorial coordinate system is a celestial coordinate system widely used to specify the positions of celestial objects. It may be implemented in spherical or rectangular coordinates, both defined by an origin at the centre of Earth, a fundamental plane consisting of the projection of Earth's equator onto the celestial sphere, a primary direction towards the vernal equinox, and a right-handed convention.

Ecliptic coordinate system

The ecliptic coordinate system is a celestial coordinate system commonly used for representing the apparent positions and orbits of Solar System objects. Because most planets and many small Solar System bodies have orbits with only slight inclinations to the ecliptic, using it as the fundamental plane is convenient. The system's origin can be the center of either the Sun or Earth, its primary direction is towards the vernal (March) equinox, and it has a right-hand convention. It may be implemented in spherical or rectangular coordinates.

Orbital inclination Angle between a reference plane and the plane of an orbit

Orbital inclination measures the tilt of an object's orbit around a celestial body. It is expressed as the angle between a reference plane and the orbital plane or axis of direction of the orbiting object.

Tropic of Cancer Line of northernmost latitude at which the sun can be directly overhead

The Tropic of Cancer, which is also referred to as the Northern Tropic, is the most northerly circle of latitude on Earth at which the Sun can be directly overhead. This occurs on the June solstice, when the Northern Hemisphere is tilted toward the Sun to its maximum extent. It also reaches 90 degrees below the horizon at solar midnight on the December Solstice. Using a continuously updated formula, the circle is currently 23°26′11.6″ (or 23.43655°) north of the Equator.

Circle of latitude Geographic notion

A circle of latitude on Earth is an abstract east–west circle connecting all locations around Earth at a given latitude.

Earth radius Distance from the center of Earth to a point on its surface

Earth radius is the distance from the center of Earth to a point on its surface. Its value ranges from a near maximum 6,378 km (3,963 mi) at the equator to a near minimum 6,357 km (3,950 mi) at either pole. A nominal Earth radius is sometimes used as a unit of measurement in astronomy and geophysics, denoted in astronomy by the symbol R. In other contexts, it is denoted or sometimes . The early definition of the metre such that the distance from equator to pole along the circumference is 10,000 km gives a radius roughly 6,367 km which is close to halfway between the minimum and maximum. However a better “average” is usually considered to be 6,371 km with a 0.3% variability for the following reasons.

Earths orbit Trajectory of Earth around the Sun

Earth orbits the Sun at an average distance of 149.60 million km, and one complete orbit takes 365.256 days, during which time Earth has traveled 940 million km. Ignoring the influence of other solar system bodies, Earth's orbit is an ellipse with the Earth-Sun barycenter as one focus and a current eccentricity of 0.0167; since this value is close to zero, the center of the orbit is close, relative to the size of the orbit, to the center of the Sun.

A lunar standstill is the gradually varying range between the northern and the southern limits of the Moon's declination, or the lunistices, over the course of one-half a sidereal month, or 13.66 days. One major, or one minor, lunar standstill occurs every 18.6 years due to the precessional cycle of the lunar nodes at that rate.

Orbit of the Moon Orbit

The Moon orbits Earth in the prograde direction and completes one revolution relative to the Vernal Equinox and the stars in about 27.32 days and one revolution relative to the Sun in about 29.53 days. Earth and the Moon orbit about their barycentre, which lies about 4,600 km (2,900 mi) from Earth's center. On average, the distance to the Moon is about 385,000 km (239,000 mi) from Earth's center, which corresponds to about 60 Earth radii or 1.282 light-seconds.

Daytime Period of a day in which a location experiences natural illumination

On Earth, daytime is the period of the day during which a given location experiences natural illumination from direct sunlight. Daytime occurs when the Sun appears above the local horizon, that is, anywhere on the globe's hemisphere facing the Sun. In direct sunlight the movement of the sun can be recorded and observed using a sundial that casts a shadow that slowly moves during the day. Other planets and natural satellites that rotate relative to a luminous primary body, such as a local star, also experience daytime, but this article primarily discusses daytime on Earth.

The poles of astronomical bodies are determined based on their axis of rotation in relation to the celestial poles of the celestial sphere. Astronomical bodies include stars, planets, dwarf planets and small Solar System bodies such as comets and minor planets, as well as natural satellites and minor-planet moons.

Sun path

Sun path, sometimes also called day arc, refers to the daily and seasonal arc-like path that the Sun appears to follow across the sky as the Earth rotates and orbits the Sun. The Sun's path affects the length of daytime experienced and amount of daylight received along a certain latitude during a given season.

Earth-centered inertial

Earth-centered inertial (ECI) coordinate frames have their origins at the center of mass of Earth and are fixed with respect to the stars. "I" in "ECI" stands for inertial, in contrast to the "Earth-centered - Earth-fixed" (ECEF) frames, which rotate with respect to stars.

The start and end dates of a season on any planet of the Solar System depends on same factors valid on Earth, but which have different values on different planets:

References

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Sources