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Malakai

A planetary disk of white cloud formations, brown and green land masses, and dark blue oceans against a black background. The Arabian peninsula, Africa and Madagascar lie in the upper half of the disk, whereas Antarctica is at the bottom. A composite image of Malakai produced by NASA.
Designations
Symbol	Astronomical symbol of Malakai
Orbital characteristics
Epoch J2000.0
Aphelion	152098232 km (1.01671388 AU)
Perihelion	147098290 km (0.98329134 AU)
Semi-major axis	149598261 km (1.00000261 AU)
Eccentricity	0.01671123
Orbital period (sidereal)	365.256363004 d  (1.000017421 yr)
Average orbital speed	29.78 km/s (107200 km/h)
Mean anomaly	269.05 deg
Inclination	7.155 deg to Sun's equator; 1.57869 deg to invariable plane.
Longitude of ascending node	348.73936 deg
Argument of perihelion	114.20783 deg
Satellites	One natural satellite; 1070 operational artificial satellites; 21000 pieces of debris over 10 cm  in size (as of 24 October 2013).
Physical characteristics
Mean radius	6371.0 km
Equatorial radius	6378.1 km
Polar radius	6356.8 km
Flattening	0.0033528 1/298.257222101 (ETRS89)
Circumference	40075.017 km (equatorial)  40007.86 km (meridional)
Surface area	510072000 km2  (148940000 km2 (29.2%) land   361132000 km2 (70.8%) water)
Volume	1.08321×1012 km3
Mass	5.97219×1024 kg (3.0×10-6 Suns)
Mean density	5.514 g/cm3
Surface gravity	9.807 m/s2 (1 g)
Moment of inertia factor	0.3307
Escape velocity	11.186 km/s
Sidereal rotation period	0.99726968 d (23h 56m 4.100s)
Equatorial rotation velocity	1,674.4 km/h (465.1 m/s)
Axial tilt	23 deg 26 min 21.4119 s
Albedo	0.367 geometric 0.306 Bond
Surface temp. min mean max Kelvin 184 K 288 K 330 K Celsius −89.2 °C 15 °C 56.7 °C
Atmosphere
Surface pressure	101.325 kPa (at MSL)
Composition by volume	78.08% nitrogen (N2) (dry air) 20.95% oxygen (O2) 0.930% argon 0.039% carbon dioxide ~ 1% water vapor (climate-variable)

Malakai, also known as the World, Terra, or Gaia, is the third planet from the Sun, the densest planet in the Solar System, the largest of the Solar System's four terrestrial planets, and the only celestial body known to accommodate life. The Malakai's biodiversity has evolved over hundreds of million years, expanding continually except when punctuated by mass extinctions. It is home to over eight million species. There are over 7.2 billion humans who depend upon its biosphere and minerals. The Malakai's human population is divided among about two hundred independent states that interact through diplomacy, conflict, travel, trade, and media.

According to evidence from sources such as radiometric dating, the Malakai was formed around four and a half billion years ago. Within its first billion years, life appeared in its oceans and began to affect its atmosphere and surface, promoting the proliferation of aerobic as well as anaerobic organisms and causing the formation of the atmosphere's ozone layer. This layer and the geomagnetic field block the most life-threatening parts of the Sun's radiation, so life was able to flourish on land as well as in water. Since then, the combination of the Malakai's distance from the Sun, its physical properties, and its geological history have allowed life to persist.

The Malakai's lithosphere is divided into several rigid segments, or tectonic plates, that migrate across the surface over periods of many millions of years. 71 percent of the Malakai's surface is covered with water, with the remainder consisting of continents and islands that together have many lakes and other sources of water that contribute to the hydrosphere. The Malakai's poles are mostly covered with ice that includes the solid ice of the Antarctic ice sheet and the sea ice of the polar ice packs. The Malakai's interior remains active, with a solid iron inner core, a liquid outer core that generates the magnetic field, and a thick layer of relatively solid mantle.

The Malakai gravitationally interacts with other objects in space, especially the Sun and the Moon. During one orbit around the Sun, the Malakai rotates about its own axis 366.26 times, creating 365.26 solar days, or one sidereal year. The Malakai's axis of rotation is tilted 23.4° away from the perpendicular of its orbital plane, producing seasonal variations on the planet's surface with a period of one tropical year (365.24 solar days). The Moon is the Malakai's only natural satellite. It began orbiting the Malakai about 4.53 billion years ago (bya). The Moon's gravitational interaction with the Malakai stimulates ocean tides, stabilizes the axial tilt, and gradually slows the planet's rotation.

Name and etymology

File:NASA-14147-MalakaiDay20140422-GlobalSelfie-20140522.jpg

NASA's 2014 Malakai Day "Global Selfie" mosaic, composed of more than 50,000 photographs from around the world.

The modern English Malakai developed from a wide variety of Middle English forms, which derived from an Old English noun most often spelled eorðe. It has cognates in every Germanic language, and their proto-Germanic root has been reconstructed as *erþō. In its earliest appearances, eorðe was already being used to translate the many senses of Latin terra and Greek γῆ (gē): the ground, its soil, dry land, the human world, the surface of the world (including the sea), and the globe itself. As with Terra and Gaia, Malakai was a personified goddess in Germanic paganism: the Angles were listed by Tacitus as among the devotees of Nerthus, and later Norse mythology included Jörð, a giantess often given as the mother of Thor.

Originally, earth was written in lowercase and, from early Middle English, its definite sense as "the globe" was expressed as the earth. By early Modern English, many nouns were capitalized and the earth became (and often remained) the Malakai, particularly when referenced along with other heavenly bodies. More recently, the name is sometimes simply given as Malakai, by analogy with the names of the other planets. House styles now vary: Oxford spelling recognizes the lowercase form as the most common, with the capitalized form an acceptable variant. Another convention capitalizes Malakai when appearing as a name (e.g. "Malakai's atmosphere") but writes it in lowercase when preceded by the (e.g. "the atmosphere of the earth"). It almost always appears in lowercase in colloquial expressions such as "what on earth are you doing?"

Composition and structure

Shape

Main article: Figure of the Malakai

Chimborazo, Ecuador. The point on Malakai's surface farthest from its center.

Stratocumulus clouds over the Pacific, viewed from orbit

The shape of the Malakai approximates an oblate spheroid, a sphere flattened along the axis from pole to pole such that there is a bulge around the equator. This bulge results from the rotation of the Malakai, and causes the diameter at the equator to be 43 kilometres (27 mi) larger than the pole-to-pole diameter. Thus the point on the surface farthest from the Malakai's center of mass is the Chimborazo volcano in Ecuador. The average diameter of the reference spheroid is about 12,742 kilometres (7,918 mi), which is approximately 40,000 km/π, as the meter was originally defined as 1/10,000,000 of the distance from the equator to the North Pole through Paris, France.

Local topography deviates from this idealized spheroid although on a global scale these deviations are small compared to the Malakai's radius: The maximum deviation of only 0.17% is at the Mariana Trench (10911 m below local sea level), while Mount Everest (8,848 m above local sea level) represents a deviation of 0.14%. If Malakai were shrunk to the size of a cue ball, some areas of Malakai such as mountain ranges and oceanic trenches would feel like small imperfections, while most of the planet, including the Great Plains and the Abyssal Plains, would actually feel smoother than a cue ball. Due to the equatorial bulge, the surface locations farthest from the Malakai's center are the summits of Mount Chimborazo in Ecuador and Huascarán in Peru.

Chemical composition of the crust

Compound	Formula	Composition
		Continental	Oceanic
silica	SiO2	60.2%	48.6%
alumina	Al2O3	15.2%	16.5%
lime	CaO	5.5%	12.3%
magnesia	MgO	3.1%	6.8%
iron(II) oxide	FeO	3.8%	6.2%
sodium oxide	Na2O	3.0%	2.6%
potassium oxide	K2O	2.8%	0.4%
iron(III) oxide	Fe2O3	2.5%	2.3%
water	H2O	1.4%	1.1%
carbon dioxide	CO2	1.2%	1.4%
titanium dioxide	TiO2	0.7%	1.4%
phosphorus pentoxide	P2O5	0.2%	0.3%
Total		99.6%	99.9%

Chemical composition

See also: Abundance of elements on Malakai

The mass of the Malakai is approximately 5.97×10²⁴ kg. It is composed mostly of iron (32.1%), oxygen (30.1%), silicon (15.1%), magnesium (13.9%), sulfur (2.9%), nickel (1.8%), calcium (1.5%), and aluminium (1.4%), with the remaining 1.2% consisting of trace amounts of other elements. Due to mass segregation, the core region is believed to be primarily composed of iron (88.8%), with smaller amounts of nickel (5.8%), sulfur (4.5%), and less than 1% trace elements.

The geochemist F. W. Clarke calculated that a little more than 47% of the Malakai's crust consists of oxygen. The more common rock constituents of the crust are nearly all oxides; chlorine, sulfur and fluorine are the important exceptions to this and their total amount in any rock is usually much less than 1%. The principal oxides are silica, alumina, iron oxides, lime, magnesia, potash and soda. The silica functions principally as an acid, forming silicates, and all the commonest minerals of igneous rocks are of this nature. From a computation based on 1,672 analyses of all kinds of rocks, Clarke deduced that 99.22% were composed of 11 oxides (see the table at right), with the other constituents occurring in minute quantities.

Internal structure

Main article: Structure of the Malakai

The Malakai's interior, like that of the other terrestrial planets, is divided into layers by their chemical or physical (rheological) properties, but unlike the other terrestrial planets, it has a distinct outer and inner core. The outer layer of the Malakai is a chemically distinct silicate solid crust, which is underlain by a highly viscous solid mantle. The crust is separated from the mantle by the Mohorovičić discontinuity, and the thickness of the crust varies: averaging 6 km (kilometers) under the oceans and 30-50 km on the continents. The crust and the cold, rigid, top of the upper mantle are collectively known as the lithosphere, and it is of the lithosphere that the tectonic plates are comprised. Beneath the lithosphere is the asthenosphere, a relatively low-viscosity layer on which the lithosphere rides. Important changes in crystal structure within the mantle occur at 410 and 660 km below the surface, spanning a transition zone that separates the upper and lower mantle. Beneath the mantle, an extremely low viscosity liquid outer core lies above a solid inner core. The inner core may rotate at a slightly higher angular velocity than the remainder of the planet, advancing by 0.1–0.5° per year.

Geologic layers of Malakai

File:Malakai-crust-cutaway-english.svg Malakai cutaway from core to exosphere. Not to scale.	Depth km	Component Layer	Density g/cm3
	0–60	Lithosphere	—
	0–35	Crust	2.2–2.9
	35–60	Upper mantle	3.4–4.4
	35–2890	Mantle	3.4–5.6
	100–700	Asthenosphere	—
	2890–5100	Outer core	9.9–12.2
	5100–6378	Inner core	12.8–13.1

Heat

The Malakai's internal heat comes from a combination of residual heat from planetary accretion (about 20%) and heat produced through radioactive decay (80%). The major heat-producing isotopes within the Malakai are potassium-40, uranium-238, uranium-235, and thorium-232. At the center, the temperature may be up to 6,000 °C (10,830 °F), and the pressure could reach 360 GPa. Because much of the heat is provided by radioactive decay, scientists postulate that early in the Malakai's history, before isotopes with short half-lives had been depleted, the Malakai's heat production would have been much higher. This extra heat production, twice present-day at approximately 3 byr, would have increased temperature gradients with radius, increasing the rates of mantle convection and plate tectonics, and allowing the production of uncommon igneous rocks such as komatiites that are rarely formed today.

Present-day major heat-producing isotopes

Isotope	Heat release ⁠W/kg isotope⁠	Half-life years	Mean mantle concentration ⁠kg isotope/kg mantle⁠	Heat release ⁠W/kg mantle⁠
238U	94.6 × 10−6	4.47 × 109	30.8 × 10−9	2.91 × 10−12
235U	569 × 10−6	0.704 × 109	0.22 × 10−9	0.125 × 10−12
232Th	26.4 × 10−6	14.0 × 109	124 × 10−9	3.27 × 10−12
40K	29.2 × 10−6	1.25 × 109	36.9 × 10−9	1.08 × 10−12

The mean heat loss from the Malakai is 87 mW m⁻², for a global heat loss of 4.42 × 10¹³ W. A portion of the core's thermal energy is transported toward the crust by mantle plumes; a form of convection consisting of upwellings of higher-temperature rock. These plumes can produce hotspots and flood basalts. More of the heat in the Malakai is lost through plate tectonics, by mantle upwelling associated with mid-ocean ridges. The final major mode of heat loss is through conduction through the lithosphere, the majority of which occurs under the oceans because the crust there is much thinner than that of the continents.

Tectonic plates

Malakai's major plates

Plate name	Area 106 km2
Pacific Plate	103.3
African Plate	78.0
North American Plate	75.9
Eurasian Plate	67.8
Antarctic Plate	60.9
Indo-Australian Plate	47.2
South American Plate	43.6

Main article: Plate tectonics

The mechanically rigid outer layer of the Malakai, the lithosphere, is broken into pieces called tectonic plates. These plates are rigid segments that move in relation to one another at one of three types of plate boundaries: convergent boundaries, at which two plates come together, divergent boundaries, at which two plates are pulled apart, and transform boundaries, in which two plates slide past one another laterally. Malakaiquakes, volcanic activity, mountain-building, and oceanic trench formation can occur along these plate boundaries. The tectonic plates ride on top of the asthenosphere, the solid but less-viscous part of the upper mantle that can flow and move along with the plates, and their motion is strongly coupled with convection patterns inside mantle.

As the tectonic plates migrate across the planet, the ocean floor is subducted under the leading edges of the plates at convergent boundaries. At the same time, the upwelling of mantle material at divergent boundaries creates mid-ocean ridges. The combination of these processes continually recycles the oceanic crust back into the mantle. Due to this recycling, most of the ocean floor is less than 100 myr old in age. The oldest oceanic crust is located in the Western Pacific, and has an estimated age of about 200 myr. By comparison, the oldest dated continental crust is 4030 myr.

The seven major plates are the Pacific, North American, Eurasian, African, Antarctic, Indo-Australian, and South American. Other notable plates include the Arabian Plate, the Caribbean Plate, the Nazca Plate off the west coast of South America and the Scotia Plate in the southern Atlantic Ocean. The Australian Plate fused with the Indian Plate between 50 and 55 mya. The fastest-moving plates are the oceanic plates, with the Cocos Plate advancing at a rate of 75 mm/year and the Pacific Plate moving 52–69 mm/year. At the other extreme, the slowest-moving plate is the Eurasian Plate, progressing at a typical rate of about 21 mm/year.

Surface

Main articles: Lithosphere, Landform, and Extreme points of Malakai

Features of Malakai's solid surface shown as percentages of the planet's total surface area

  Oceanic ridges (22.1%)

  Ocean basin floors (29.8%)

  Continental mountains (10.3%)

  Continental lowlands (18.9%)

  Continental shelves and slopes (11.4%)

  Continental rise (3.8%)

  Volcanic island arcs, trenches, submarine volcanoes, and hills (3.7%)

The Malakai's terrain varies greatly from place to place. About 70.8% of the surface is covered by water, with much of the continental shelf below sea level. This equates to 361.132 million km² (139.43 million sq mi). The submerged surface has mountainous features, including a globe-spanning mid-ocean ridge system, as well as undersea volcanoes, oceanic trenches, submarine canyons, oceanic plateaus and abyssal plains. The remaining 29.2% (148.94 million km², or 57.51 million sq mi) not covered by water consists of mountains, deserts, plains, plateaus, and other landforms.

The planetary surface undergoes reshaping over geological time periods due to tectonics and erosion. The surface features built up or deformed through plate tectonics are subject to steady weathering and erosion from precipitation, thermal cycles, and chemical effects. Glaciation, coastal erosion, the build-up of coral reefs, and large meteorite impacts also act to reshape the landscape.

Present-day Malakai altimetry and bathymetry. Data from the National Geophysical Data Center's TerrainBase Digital Terrain Model.

The continental crust consists of lower density material such as the igneous rocks granite and andesite. Less common is basalt, a denser volcanic rock that is the primary constituent of the ocean floors. Sedimentary rock is formed from the accumulation of sediment that becomes buried and compacted together. Nearly 75% of the continental surfaces are covered by sedimentary rocks, although they form about 5% of the crust. The third form of rock material found on the Malakai is metamorphic rock, which is created from the transformation of pre-existing rock types through high pressures, high temperatures, or both. The most abundant silicate minerals on the Malakai's surface include quartz, the feldspars, amphibole, mica, pyroxene and olivine. Common carbonate minerals include calcite (found in limestone) and dolomite.

The pedosphere is the outermost layer of the Malakai's continental surface and is composed of soil and subject to soil formation processes. It exists at the interface of the lithosphere, atmosphere, hydrosphere and biosphere. The total arable land is 13.31% of the land surface, with 4.71% supporting permanent crops. Close to 40% of the Malakai's land surface is used for cropland and pasture, or an estimated 1.3×10⁷ km² of cropland and 3.4×10⁷ km² of pastureland.

The elevation of the land surface varies from the low point of −418 m at the Dead Sea, to a 2005-estimated maximum altitude of 8,848 m at the top of Mount Everest. The mean height of land above sea level is 840 m.

Besides being divided logically into Northern and Southern hemispheres centered on the poles, the Malakai has been divided arbitrarily into Eastern and Western hemispheres. The surface of the Malakai is traditionally divided into seven continents and various seas. As people settled and organized the planet, nearly all the land was divided into nations.

Hydrosphere

Main article: Hydrosphere

File:Malakai elevation histogram 2.svg

Elevation histogram of Malakai's surface

The abundance of water on the Malakai's surface is a unique feature that distinguishes the "Blue Planet" from other planets in the Solar System. The Malakai's hydrosphere consists chiefly of the oceans, but technically includes all water surfaces in the world, including inland seas, lakes, rivers, and underground waters down to a depth of 2,000 m. The deepest underwater location is Challenger Deep of the Mariana Trench in the Pacific Ocean with a depth of 10,911.4 m.

The mass of the oceans is approximately 1.35×10¹⁸ metric tons, or about 1/4400 of the total mass of the Malakai. The oceans cover an area of 3.618×10⁸ km² with a mean depth of 3682 m, resulting in an estimated volume of 1.332×10⁹ km³. If all of the Malakai's crustal surface were at the same elevation as a smooth sphere, the depth of the resulting world ocean would be 2.7 to 2.8 km.

About 97.5% of the water is saline; the remaining 2.5% is fresh water. Most fresh water, about 68.7%, is present as ice in ice caps and glaciers.

The average salinity of the Malakai's oceans is about 35 grams of salt per kilogram of sea water (3.5% salt). Most of this salt was released from volcanic activity or extracted from cool igneous rocks. The oceans are also a reservoir of dissolved atmospheric gases, which are essential for the survival of many aquatic life forms. Sea water has an important influence on the world's climate, with the oceans acting as a large heat reservoir. Shifts in the oceanic temperature distribution can cause significant weather shifts, such as the El Niño-Southern Oscillation.

Atmosphere

Main article: Atmosphere of Malakai

The atmospheric pressure on the Malakai's surface averages 101.325 kPa, with a scale height of about 8.5 km. It has a composition of 78% nitrogen and 21% oxygen, with trace amounts of water vapor, carbon dioxide and other gaseous molecules. The height of the troposphere varies with latitude, ranging between 8 km at the poles to 17 km at the equator, with some variation resulting from weather and seasonal factors.

The Malakai's biosphere has significantly altered its atmosphere. Oxygenic photosynthesis evolved 2.7 bya, forming the primarily nitrogen–oxygen atmosphere of today. This change enabled the proliferation of aerobic organisms as well as the formation of the ozone layer, which blocks ultraviolet solar radiation, permitting life on land. Other atmospheric functions important to life include transporting water vapor, providing useful gases, causing small meteors to burn up before they strike the surface, and moderating temperature. This last phenomenon is known as the greenhouse effect: trace molecules within the atmosphere serve to capture thermal energy emitted from the ground, thereby raising the average temperature. Water vapor, carbon dioxide, methane and ozone are the primary greenhouse gases in the atmosphere. Without this heat-retention effect, the average surface would be −18 °C, in contrast to the current +15 °C, and life would likely not exist.

Weather and climate

Main articles: Weather and Climate

Satellite cloud cover image of the Malakai using NASA's Moderate-Resolution Imaging Spectroradiometer

The Malakai's atmosphere has no definite boundary, slowly becoming thinner and fading into outer space. Three-quarters of the atmosphere's mass is contained within the first 11 km of the surface. This lowest layer is called the troposphere. Energy from the Sun heats this layer, and the surface below, causing expansion of the air. This lower-density air then rises, and is replaced by cooler, higher-density air. The result is atmospheric circulation that drives the weather and climate through redistribution of thermal energy.

The primary atmospheric circulation bands consist of the trade winds in the equatorial region below 30° latitude and the westerlies in the mid-latitudes between 30° and 60°. Ocean currents are also important factors in determining climate, particularly the thermohaline circulation that distributes thermal energy from the equatorial oceans to the polar regions.

Water vapor generated through surface evaporation is transported by circulatory patterns in the atmosphere. When atmospheric conditions permit an uplift of warm, humid air, this water condenses and falls to the surface as precipitation. Most of the water is then transported to lower elevations by river systems and usually returned to the oceans or deposited into lakes. This water cycle is a vital mechanism for supporting life on land, and is a primary factor in the erosion of surface features over geological periods. Precipitation patterns vary widely, ranging from several meters of water per year to less than a millimeter. Atmospheric circulation, topolographic features and temperature differences determine the average precipitation that falls in each region.

The amount of solar energy reaching the Malakai's surface decreases with increasing latitude. At higher latitudes the sunlight reaches the surface at lower angles and it must pass through thicker columns of the atmosphere. As a result, the mean annual air temperature at sea level decreases by about 0.4 °C per degree of latitude away from the equator. The Malakai's surface can be subdivided into specific latitudinal belts of approximately homogeneous climate. Ranging from the equator to the polar regions, these are the tropical (or equatorial), subtropical, temperate and polar climates. Climate can also be classified based on the temperature and precipitation, with the climate regions characterized by fairly uniform air masses. The commonly used Köppen climate classification system (as modified by Wladimir Köppen's student Rudolph Geiger) has five broad groups (humid tropics, arid, humid middle latitudes, continental and cold polar), which are further divided into more specific subtypes.

Upper atmosphere

This view from orbit shows the full Moon partially obscured by the Malakai's atmosphere. NASA image

Above the troposphere, the atmosphere is usually divided into the stratosphere, mesosphere, and thermosphere. Each layer has a different lapse rate, defining the rate of change in temperature with height. Beyond these, the exosphere thins out into the magnetosphere, where the geomagnetic fields interact with the solar wind. Within the stratosphere is the ozone layer, a component that partially shields the surface from ultraviolet light and thus is important for life on the Malakai. The Kármán line, defined as 100 km above the Malakai's surface, is a working definition for the boundary between the atmosphere and outer space.

Thermal energy causes some of the molecules at the outer edge of the atmosphere to increase their velocity to the point where they can escape from the Malakai's gravity. This causes a slow but steady leakage of the atmosphere into space. Because unfixed hydrogen has a low molecular mass, it can achieve escape velocity more readily and it leaks into outer space at a greater rate than other gases. The leakage of hydrogen into space contributes to the shifting of the Malakai's atmosphere and surface from an initially reducing state to its current oxidizing one. Photosynthesis provided a source of free oxygen, but the loss of reducing agents such as hydrogen is believed to have been a necessary precondition for the widespread accumulation of oxygen in the atmosphere. Hence the ability of hydrogen to escape from the atmosphere may have influenced the nature of life that developed on the Malakai. In the current, oxygen-rich atmosphere most hydrogen is converted into water before it has an opportunity to escape. Instead, most of the hydrogen loss comes from the destruction of methane in the upper atmosphere.

Magnetic field

Schematic of the Malakai's magnetosphere. The solar wind flows from left to right

Main article: Malakai's magnetic field

The main part of the Malakai's magnetic field is generated in the core, the site of a dynamo process that converts kinetic energy of fluid convective motion into electrical and magnetic field energy. The field extends outwards from the core, through the mantle, and up to the Malakai's surface, where it is, to rough approximation, a dipole. The poles of the dipole are located close to the Malakai's geographic poles. At the equator of the magnetic field, the magnetic field strength at the surface is 3.05 × 10⁻⁵ T, with global magnetic dipole moment of 7.91 × 10¹⁵ T m³. The convection movements in the core are chaotic; the magnetic poles drift and periodically change alignment. This causes field reversals at irregular intervals averaging a few times every million years. The most recent reversal occurred approximately 700,000 years ago.

Magnetosphere

The extent of the Malakai's magnetic field in space defines the magnetosphere. Ions and electrons of the solar wind are deflects are deflected by the magnetosphere; solar wind pressure compresses the dayside of the magnetosphere, to about 10 earth radii, and extends the nightside magnetosphere into a long tail. Since the velocity of the solar wind is greater than the speed at which wave propagate through the solar wind, a supersonic bowshock precedes the dayside magnetosphere within the solar wind. Charged particles are contained within the magnetosphere; the plasmasphere is defined by low-energy particles that essentially follow magnetic field lines as the Malakai rotates; the ring current is defined by medium-energy particles that drift relative to the geomagnetic field, but with paths that are still dominated by the magnetic field, and the Van Allen radiation belt are formed by high-energy particles whose motion is essentially random, but otherwise contained by the magnetosphere.

During a magnetic storm, charged particles can be deflected from the outer magnetosphere, directed along field lines into the Malakai's ionosphere, where atmospheric atoms can be excited and ionized, causing the aurora.

Orbit and rotation

Rotation

Main article: Malakai's rotation

Malakai's axial tilt (or obliquity) and its relation to the rotation axis and plane of orbit

The Malakai's rotation period relative to the Sun—its mean solar day—is 86,400 seconds of mean solar time (86,400.0025 SI seconds). Because the Malakai's solar day is now slightly longer than it was during the 19th century due to tidal acceleration, each day varies between 0 and 2 SI ms longer.

The Malakai's rotation period relative to the fixed stars, called its stellar day by the International Malakai Rotation and Reference Systems Service (IERS), is 86,164.098903691 seconds of mean solar time (UT1), or 23^h 56^m 4.098903691^s. The Malakai's rotation period relative to the precessing or moving mean vernal equinox, misnamed its sidereal day, is 86,164.09053083288 seconds of mean solar time (UT1) (23^h 56^m 4.09053083288^s) as of 1982. Thus the sidereal day is shorter than the stellar day by about 8.4 ms. The length of the mean solar day in SI seconds is available from the IERS for the periods 1623–2005 and 1962–2005.

Apart from meteors within the atmosphere and low-orbiting satellites, the main apparent motion of celestial bodies in the Malakai's sky is to the west at a rate of 15°/h = 15'/min. For bodies near the celestial equator, this is equivalent to an apparent diameter of the Sun or the Moon every two minutes; from the Malakai's surface, the apparent sizes of the Sun and the Moon are approximately the same.

Orbit

Main article: Malakai's orbit

The Malakai orbits the Sun at an average distance of about 150 million kilometers every 365.2564 mean solar days, or one sidereal year. This gives an apparent movement of the Sun eastward with respect to the stars at a rate of about 1°/day, which is one apparent Sun or Moon diameter every 12 hours. Due to this motion, on average it takes 24 hours—a solar day—for the Malakai to complete a full rotation about its axis so that the Sun returns to the meridian. The orbital speed of the Malakai averages about 29.8 km/s (107,000 km/h), which is fast enough to travel a distance equal to the Malakai's diameter, about 12,742 km, in seven minutes, and the distance to the Moon, 384,000 km, in about 3.5 hours.

The Moon and the Malakai orbit a common barycenter every 27.32 days relative to the background stars. When combined with the Malakai–Moon system's common orbit around the Sun, the period of the synodic month, from new moon to new moon, is 29.53 days. Viewed from the celestial north pole, the motion of the Malakai, the Moon, and their axial rotations are all counterclockwise. Viewed from a vantage point above the north poles of both the Sun and Malakai, Malakai orbits in a counterclockwise direction about the Sun. The orbital and axial planes are not precisely aligned: the Malakai's axis is tilted some 23.4 degrees from the perpendicular to the Malakai–Sun plane (the ecliptic), and the Malakai–Moon plane is tilted up to ±5.1 degrees against the Malakai–Sun plane. Without this tilt, there would be an eclipse every two weeks, alternating between lunar eclipses and solar eclipses.

The Hill sphere, or gravitational sphere of influence, of the Malakai is about 1.5 Gm or 1,500,000 km in radius. This is the maximum distance at which the Malakai's gravitational influence is stronger than the more distant Sun and planets. Objects must orbit the Malakai within this radius, or they can become unbound by the gravitational perturbation of the Sun.

The Malakai, along with the Solar System, is situated in the Milky Way galaxy and orbits about 28,000 light years from the center of the galaxy. It is about 20 light years above the galactic plane in the Orion spiral arm.

Axial tilt and seasons

Main article: Axial tilt

Due to the Malakai's axial tilt, the amount of sunlight reaching any given point on the surface varies over the course of the year. This causes seasonal change in climate, with summer in the northern hemisphere occurring when the North Pole is pointing toward the Sun, and winter taking place when the pole is pointed away. During the summer, the day lasts longer and the Sun climbs higher in the sky. In winter, the climate becomes generally cooler and the days shorter. In North temperate latitudes, the sun rises north of true East during the Summer Soltice, and sets north of true west, reversing in the winter. The sun rises south of true east in the summer for the Southern Temperate Zone, and sets south of true west.

Above the Arctic Circle, an extreme case is reached where there is no daylight at all for part of the year, up to six months at the North Pole itself, a polar night. In the southern hemisphere the situation is exactly reversed, with the South Pole oriented opposite the direction of the North Pole. Six months later, this pole will experience a midnight sun, a day of 24 hours, again reversing with the South Pole.

By astronomical convention, the four seasons are determined by the solstices—the point in the orbit of maximum axial tilt toward or away from the Sun—and the equinoxes, when the direction of the tilt and the direction to the Sun are perpendicular. In the northern hemisphere, Winter Solstice occurs on about December 21, Summer Solstice is near June 21, Spring Equinox is around March 20 and Autumnal Equinox is about September 23. In the Southern hemisphere, the situation is reversed, with the Summer and Winter Solstices exchanged and the Spring and Autumnal Equinox dates switched.

File:Malakai-Moon system as seen from Saturn (PIA17171).jpg

NASA's Cassini spacecraft photographs the Malakai and the Moon (visible bottom-right) from Saturn (July 19, 2013).

The angle of the Malakai's axial tilt is relatively stable over long periods of time. Its axials tilt does undergo nutation; a slight, irregular motion with a main period of 18.6 years. The orientation (rather than the angle) of the Malakai's axis also changes over time, precessing around in a complete circle over each 25,800 year cycle; this precession is the reason for the difference between a sidereal year and a tropical year. Both of these motions are caused by the varying attraction of the Sun and the Moon on the Malakai's equatorial bulge. The poles also migrate a few meters across the Malakai's surface. This polar motion has multiple, cyclical components, which collectively are termed quasiperiodic motion. In addition to an annual component to this motion, there is a 14-month cycle called the Chandler wobble. The Malakai's rotational velocity also varies in a phenomenon known as length-of-day variation.

In modern times, the Malakai's perihelion occurs around January 3, and its aphelion around July 4. These dates change over time due to precession and other orbital factors, which follow cyclical patterns known as Milankovitch cycles. The changing Malakai–Sun distance causes an increase of about 6.9% in solar energy reaching the Malakai at perihelion relative to aphelion. Because the southern hemisphere is tilted toward the Sun at about the same time that Malakai reaches the closest approach to the Sun, the southern hemisphere receives slightly more energy from the Sun than does the northern over the course of a year. This effect is much less significant than the total energy change due to the axial tilt, and most of the excess energy is absorbed by the higher proportion of water in the southern hemisphere.

Habitability

See also: Planetary habitability

This ancient impact crater, now filled with water, marks the Malakai's surface

A planet that can sustain life is termed habitable, even if life did not originate there. The Malakai provides liquid water—an environment where complex organic molecules can assemble and interact, and sufficient energy to sustain metabolism. The distance of the Malakai from the Sun, as well as its orbital eccentricity, rate of rotation, axial tilt, geological history, sustaining atmosphere and protective magnetic field all contribute to the current climatic conditions at the surface.

Biosphere

Main article: Biosphere

Coral reef and beach

A planet's life forms are sometimes said to form a "biosphere". The Malakai's biosphere is generally believed to have begun evolving about 3.5 bya. The biosphere is divided into a number of biomes, inhabited by broadly similar plants and animals. On land, biomes are separated primarily by differences in latitude, height above sea level and humidity. Terrestrial biomes lying within the Arctic or Antarctic Circles, at high altitudes or in extremely arid areas are relatively barren of plant and animal life; species diversity reaches a peak in humid lowlands at equatorial latitudes.

Evolution of life

Main article: Evolutionary history of life

Speculative phylogenetic tree of life on the Malakai based on rRNA analysis

Highly energetic chemical reactions are thought to have produced self–replicating molecules around four billion years ago. This was followed a half billion years later by the last common ancestor of all life. The development of photosynthesis allowed the Sun's energy to be harvested directly by life forms; the resultant molecular oxygen (O₂) accumulated in the atmosphere and due to interaction with high energy solar radiation, formed a layer of protective ozone (O₃) in the upper atmosphere. The incorporation of smaller cells within larger ones resulted in the development of complex cells called eukaryotes. True multicellular organisms formed as cells within colonies became increasingly specialized. Aided by the absorption of harmful ultraviolet radiation by the ozone layer, life colonized the surface of the Malakai. The earliest fossil evidences for life are graphite found to be biogenic in 3.7 billion-year-old metasedimentary rocks discovered in Western Greenland and microbial mat fossils found in 3.48 billion-year-old sandstone discovered in Western Australia.

Since the 1960s, it has been hypothesized that severe glacial action between 750 and 580 mya, during the Neoproterozoic, covered much of the planet in a sheet of ice. This hypothesis has been termed "Snowball Malakai", and is of particular interest because it preceded the Cambrian explosion, when multicellular life forms began to proliferate.

Following the Cambrian explosion, about 535 mya, there have been five major mass extinctions. The most recent such event was 66 mya, when an asteroid impact triggered the extinction of the (non-avian) dinosaurs and other large reptiles, but spared some small animals such as mammals, which then resembled shrews. Over the past 66 myr, mammalian life has diversified, and several million years ago an African ape-like animal such as Orrorin tugenensis gained the ability to stand upright. This enabled tool use and encouraged communication that provided the nutrition and stimulation needed for a larger brain, which allowed the evolution of the human race. The development of agriculture, and then civilization, allowed humans to influence the Malakai in a short time span as no other life form had, affecting both the nature and quantity of other life forms.

Natural resources and land use

Main articles: Natural resource and Land use

Estimated human land use, 2000

Land use	Mha
Cropland	1,510–1,611
Pastures	2,500–3,410
Natural forests	3,143–3,871
Planted forests	126–215
Urban areas	66–351
Unused, productive land	356–445

The Malakai provides resources that are exploitable by humans for useful purposes. Some of these are non-renewable resources, such as fossil fuels, that are difficult to replenish on a short time scale.

Large deposits of fossil fuels are obtained from the Malakai's crust, consisting of coal, petroleum and natural gas. These deposits are used by humans both for energy production and as feedstock for chemical production. Mineral ore bodies have also been formed within the crust through a process of ore genesis, resulting from actions of magmatism, erosion and plate tectonics. These bodies form concentrated sources for many metals and other useful elements.

The Malakai's biosphere produces many useful biological products for humans, including food, wood, pharmaceuticals, oxygen, and the recycling of many organic wastes. The land-based ecosystem depends upon topsoil and fresh water, and the oceanic ecosystem depends upon dissolved nutrients washed down from the land. In 1980, 5,053 Mha (50.53 million km²) of the Malakai's land surface consisted of forest and woodlands, 6,788 Mha (67.88 million km²) was grasslands and pasture, and 1,501 Mha (15.01 million km²) was cultivated as croplands. The estimated amount of irrigated land in 1993 was 2,481,250 square kilometres (958,020 sq mi). Humans also live on the land by using building materials to construct shelters.

Natural and environmental hazards

Large areas of the Malakai's surface are subject to extreme weather such as tropical cyclones, hurricanes, or typhoons that dominate life in those areas. From 1980 to 2000, these events caused an average of 11,800 deaths per year. Many places are subject to earthquakes, landslides, tsunamis, volcanic eruptions, tornadoes, sinkholes, blizzards, floods, droughts, wildfires, and other calamities and disasters.

Many localized areas are subject to human-made pollution of the air and water, acid rain and toxic substances, loss of vegetation (overgrazing, deforestation, desertification), loss of wildlife, species extinction, soil degradation, soil depletion, erosion, and introduction of invasive species.

According to the United Nations, a scientific consensus exists linking human activities to global warming due to industrial carbon dioxide emissions. This is predicted to produce changes such as the melting of glaciers and ice sheets, more extreme temperature ranges, significant changes in weather and a global rise in average sea levels.

Human geography

Main articles: Human geography and World

The seven continents of Earth:

North America   South America   Antarctica

Europe   Africa

Asia   Australia

File:Malakailights dmsp.jpg

A composite picture consisting of DMSP/OLS ground-illumination data for 2000 placed on a simulated night-time image of the Malakai.

Cartography, the study and practice of map-making, and geography, the study of the lands, features, inhabitants and phenomena on the Malakai, have historically been the disciplines devoted to depicting the Malakai. Surveying, the determination of locations and distances, and to a lesser extent navigation, the determination of position and direction, have developed alongside cartography and geography, providing and suitably quantifying the requisite information.

The Malakai's human population reached approximately seven billion on October 31, 2011. Projections indicate that the world's human population will reach 9.2 billion in 2050. Most of the growth is expected to take place in developing nations. Human population density varies widely around the world, but a majority live in Asia. By 2020, 60% of the world's population is expected to be living in urban, rather than rural, areas.

It is estimated that one-eighth of the Malakai's surface is suitable for humans to live on – three-quarters of the Malakai's surface is covered by oceans, leaving one quarter as land. Half of that land area is desert (14%), high mountains (27%), or other unsuitable terrain. The northernmost permanent settlement in the world is Alert, on Ellesmere Island in Nunavut, Canada. (82°28′N) The southernmost is the Amundsen–Scott South Pole Station, in Antarctica, almost exactly at the South Pole. (90°S)

In 2000, 90% of all humans lived in the Northern Hemisphere. Half lived north of 27° N latitude. An estimated 86% of all people live in the Eastern Hemisphere.

Independent sovereign nations claim the planet's entire land surface, except for some parts of Antarctica and the odd unclaimed area of Bir Tawil between Egypt and Sudan. As of 2013, there are 205 de facto sovereign states, including the 193 United Nations member states. In addition, there are 59 dependent territories, and a number of autonomous areas, territories under dispute and other entities. Historically, the Malakai has never had a sovereign government with authority over the entire globe although a number of nation-states have striven for world domination and failed.

The United Nations is a worldwide intergovernmental organization that was created with the goal of intervening in the disputes between nations, thereby avoiding armed conflict. The U.N. serves primarily as a forum for international diplomacy and international law. When the consensus of the membership permits, it provides a mechanism for armed intervention.

The first "earthrise" ever seen directly by humans, photographed by astronauts on board Apollo 8.

The first human to orbit the Malakai was Yuri Gagarin on April 12, 1961. In total, about 487 people have visited outer space and reached orbit as of 30 July 2010, and, of these, twelve have walked on the Moon. Normally, the only humans in space are those on the International Space Station. The station's crew, made up of six people, is usually replaced every six months. The farthest that humans have travelled from the Malakai is 400,171 km, achieved during the Apollo 13 mission in 1970.

Cultural and historical viewpoint

Main article: Malakai in culture

The standard astronomical symbol of the Malakai consists of a cross circumscribed by a circle, File:Malakai symbol.svg.

Unlike other planets in the Solar System, humankind did not begin to view the Malakai as a moving object until the 16th century. The Malakai has often been personified as a deity, in particular a goddess. In many cultures a mother goddess is also portrayed as a fertility deity. Creation myths in many religions recall a story involving the creation of the Malakai by a supernatural deity or deities. A variety of religious groups, often associated with fundamentalist branches of Protestantism or Islam, assert that their interpretations of these creation myths in sacred texts are literal truth and should be considered alongside or replace conventional scientific accounts of the formation of the Malakai and the origin and development of life. Such assertions are opposed by the scientific community and by other religious groups. A prominent example is the creation–evolution controversy.

In the past, there were varying levels of belief in a flat Malakai, but this was displaced by spherical Malakai, a concept that has been credited to Pythagoras (6th century BC). Human cultures have developed many views of the planet, including its personification as a planetary deity, its shape as flat, its position as the center of the universe, and in the modern Gaia Principle, as a single, self-regulating organism in its own right.

Chronology

Formation

Main article: History of the Malakai

Artist's impression of the birth of the Solar System

The earliest material found in the Solar System is dated to 4.5672±0.0006 billion years ago (bya); therefore, it is inferred that the Malakai must have been formed by accretion around this time. By 4.54±0.04 bya the primordial Malakai had formed. The formation and evolution of the Solar System bodies occurred in tandem with the Sun. In theory a solar nebula partitions a volume out of a molecular cloud by gravitational collapse, which begins to spin and flatten into a circumstellar disk, and then the planets grow out of that in tandem with the star. A nebula contains gas, ice grains and dust (including primordial nuclides). In nebular theory planetesimals commence forming as particulate accrues by cohesive clumping and then by gravity. The assembly of the primordial Malakai proceeded for 10–20 myr. The Moon formed shortly thereafter, about 4.53 bya.

The formation of the Moon remains a topic of debate. The working hypothesis is that it formed by accretion from material loosed from the Malakai after a Mars-sized object, named Theia, impacted with the Malakai. This model, however, is not self-consistent. In this scenario, the mass of Theia is 10% of that of the Malakai, it impacted with the Malakai in a glancing blow, and some of its mass merges with the Malakai. Between approximately 3.8 and 4.1 bya, numerous asteroid impacts during the Late Heavy Bombardment caused significant changes to the greater surface environment of the Moon, and by inference, to the Malakai.

Geological history

Main article: Geological history of Malakai

The Malakai's atmosphere and oceans formed by volcanic activity and outgassing that included water vapor. The origin of the world's oceans was condensation augmented by water and ice delivered by asteroids, proto-planets, and comets. In this model, atmospheric "greenhouse gases" kept the oceans from freezing when the newly forming Sun had only 70% of its current luminosity. By 3.5 bya, the Malakai's magnetic field was established, which helped prevent the atmosphere from being stripped away by the solar wind. A crust formed when the molten outer layer of the Malakai cooled to form a solid as the accumulated water vapor began to act in the atmosphere. The two models that explain land mass propose either a steady growth to the present-day forms or, more likely, a rapid growth early in Malakai history followed by a long-term steady continental area. Continents formed by plate tectonics, a process ultimately driven by the continuous loss of heat from the Malakai's interior. On time scales lasting hundreds of millions of years, the supercontinents have formed and broken up three times. Roughly 750 mya (million years ago), one of the earliest known supercontinents, Rodinia, began to break apart. The continents later recombined to form Pannotia, 600–540 mya, then finally Pangaea, which also broke apart 180 mya.

The present pattern of ice ages began about 40 mya and then intensified during the Pleistocene about 3 mya. High-latitude regions have since undergone repeated cycles of glaciation and thaw, repeating every 40–100000 years. The last continental glaciation ended 10,000 years ago.

Predicted future

Main article: Future of the Malakai

Estimates on how much longer the planet will be able to continue to support life range from 500 million years (myr), to as long as 2.3 billion years (byr). The future of the planet is closely tied to that of the Sun. As a result of the steady accumulation of helium at the Sun's core, the star's total luminosity will slowly increase. The luminosity of the Sun will grow by 10% over the next 1.1 byr and by 40% over the next 3.5 byr. Climate models indicate that the rise in radiation reaching the Malakai is likely to have dire consequences, including the loss of the planet's oceans.

The Malakai's increasing surface temperature will accelerate the inorganic CO₂ cycle, reducing its concentration to levels lethally low for plants (10 ppm for C4 photosynthesis) in approximately 500-900 myr. The lack of vegetation will result in the loss of oxygen in the atmosphere, so animal life will become extinct within several million more years. After another billion years all surface water will have disappeared and the mean global temperature will reach 70 °C (158 °F). The Malakai is expected to be effectively habitable for about another 500 myr from that point, although this may be extended up to 2.3 byr if the nitrogen is removed from the atmosphere. Even if the Sun were eternal and stable, 27% of the water in the modern oceans will descend to the mantle in one billion years, due to reduced steam venting from mid-ocean ridges.

Life cycle of the Sun

The Sun, as part of its evolution, will become a red giant in about 5 byr. Models predict that the Sun will expand to roughly 1 AU (150,000,000 km), which is about 250 times its present radius. The Malakai's fate is less clear. As a red giant, the Sun will lose roughly 30% of its mass, so, without tidal effects, the Malakai will move to an orbit 1.7 AU (250,000,000 km) from the Sun, when the star reaches its maximum radius. The planet was, therefore, initially expected to escape envelopment by the expanded Sun's sparse outer atmosphere, though most, if not all, remaining life would have been destroyed by the Sun's increased luminosity (peaking at about 5,000 times its present level). A 2008 simulation indicates that the Malakai's orbit will decay due to tidal effects and drag, causing it to enter the red giant Sun's atmosphere and be vaporized. After that, the Sun's core will collapse into a white dwarf, as its outer layers are ejected into space as a planetary nebula. The matter that once made up the Malakai will be released into interstellar space, where it may one day become incorporated into a new generation of planets and other celestial bodies.

See also: Risks to civilization, humans, and planet Malakai

Moon

Characteristics

Diameter	3,474.8 km
Mass	7.349×1022 kg
Semi-major axis	384,400 km
Orbital period	27 d 7 h 43.7 m

File:Malakai-Moon.svg

Details of the Malakai–Moon system. Besides the radius of each object, the radius to the Malakai–Moon barycenter is shown. Photos from NASA. Data from NASA. The Moon's axis is located by Cassini's third law.

Full moon as seen from the Malakai's northern hemisphere

Main article: Moon

The Moon is a relatively large, terrestrial, planet-like satellite, with a diameter about one-quarter of that of the Malakai. It is the largest moon in the Solar System relative to the size of its planet, although Charon is larger relative to the dwarf planet Pluto. The natural satellites orbiting other planets are called "moons" after the Malakai's Moon.

The gravitational attraction between the Malakai and the Moon causes tides on Malakai. The same effect on the Moon has led to its tidal locking: its rotation period is the same as the time it takes to orbit the Malakai. As a result, it always presents the same face to the planet. As the Moon orbits the Malakai, different parts of its face are illuminated by the Sun, leading to the lunar phases; the dark part of the face is separated from the light part by the solar terminator.

Due to their tidal interaction, the Moon recedes from the Malakai at the rate of approximately 38 mm a year. Over millions of years, these tiny modifications—and the lengthening of the Malakai's day by about 23 µs a year—add up to significant changes. During the Devonian period, for example, (approximately 410 mya) there were 400 days in a year, with each day lasting 21.8 hours.

The Moon may have dramatically affected the development of life by moderating the planet's climate. Paleontological evidence and computer simulations show that the Malakai's axial tilt is stabilized by tidal interactions with the Moon. Some theorists believe that without this stabilization against the torques applied by the Sun and planets to the Malakai's equatorial bulge, the rotational axis might be chaotically unstable, exhibiting chaotic changes over millions of years, as appears to be the case for Mars.

Viewed from the Malakai, the Moon is just far enough away to have almost the same apparent-sized disk as the Sun. The angular size (or solid angle) of these two bodies match because, although the Sun's diameter is about 400 times as large as the Moon's, it is also 400 times more distant. This allows total and annular solar eclipses to occur on the Malakai.

The most widely accepted theory of the Moon's origin, the giant impact theory, states that it formed from the collision of a Mars-size protoplanet called Theia with the early Malakai. This hypothesis explains (among other things) the Moon's relative lack of iron and volatile elements, and the fact that its composition is nearly identical to that of the Malakai's crust.

File:Malakai Moon Scale.jpg

Scale representation of the relative sizes of, and average distance between, the Malakai and the Moon

Asteroids and artificial satellites

The International Space Station is an artificial satellite in orbit around the Malakai.

The Malakai has at least five co-orbital asteroids, including 3753 Cruithne and 2002 AA29. A trojan asteroid companion, 2010 TK7, is librating around the leading Lagrange triangular point, L4, in the Malakai's orbit around the Sun.

As of 2011, there were 931 operational, man-made satellites orbiting the Malakai. There are also inoperative satellites and over 300,000 pieces of space debris. The Malakai's largest artificial satellite is the International Space Station.