Lunar south pole

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The lunar south pole at the center of this image, situated on the rim of Shackleton Crater. Mosaic image created by LROC (Lunar Reconnaissance Orbiter) and ShadowCam Shackleton Crater.jpg
The lunar south pole at the center of this image, situated on the rim of Shackleton Crater. Mosaic image created by LROC (Lunar Reconnaissance Orbiter) and ShadowCam
A view of the south pole of the Moon showing where reflectance and temperature data indicate the possible presence of surface water ice

The lunar south pole is the southernmost point on the Moon. It is of interest to scientists because of the occurrence of water ice in permanently shadowed areas around it. The lunar south pole region features craters that are unique in that the near-constant sunlight does not reach their interior. Such craters are cold traps that contain fossil records of hydrogen, water ice, and other volatiles dating from the early Solar System. [1] [2] In contrast, the lunar north pole region exhibits a much lower quantity of similarly sheltered craters. [3]

Contents

Geography

Full Moon with south polar region features marked Full Moon with south polar markings.jpg
Full Moon with south polar region features marked
The several hundred kilometer wide Lunar south polar region as irradiated during summer. The south pole lies at the rim of Shackleton crater. The region is shadowed by the well illuminated Leibnitz plateau, flanked on the right by the Nobile crater and to the left by the partly shadowed Malapert crater and its Malapert peak illuminated at the rim of Haworth crater. Lunar south pole summer annotated.jpg
The several hundred kilometer wide Lunar south polar region as irradiated during summer. The south pole lies at the rim of Shackleton crater. The region is shadowed by the well illuminated Leibnitz plateau, flanked on the right by the Nobile crater and to the left by the partly shadowed Malapert crater and its Malapert peak illuminated at the rim of Haworth crater.

The lunar south pole is located on the center of the polar Antarctic Circle (80°S to 90°S). [2] [4] (The axis spin is 88.5 degrees from the plane of the ecliptic.) The lunar south pole has shifted 5 degrees from its original position billions of years ago.[ citation needed ] This shift has [5] changed the rotational axis of the Moon, allowing sunlight to reach previously shadowed areas, but the south pole still features some completely shadowed areas. Conversely, the pole also contains areas with permanent exposure to sunlight. The south pole region features many craters and basins such as the South Pole–Aitken basin, which appears to be one of the most fundamental features of the Moon, [6] and mountains, such as Epsilon Peak at 9.050 km, taller than any mountain found on Earth. The south pole temperature averages approximately 260 K (−13 °C; 8 °F). [6]

Craters

Aerial view of the polar region craters with elevation colouring Lunar South Pole Terrain in Coded Color (SVS5127 - lola sp still 4k).tiff
Aerial view of the polar region craters with elevation colouring

The pole defined by the rotational axis of the Moon lies within Shackleton Crater. Notable craters nearest to the lunar south pole include de Gerlache, Sverdrup, Shoemaker, Faustini, Haworth, Nobile, and Cabeus.

Discoveries

Illumination

The lunar south pole features a region with crater rims exposed to near-constant solar illumination, yet the interior of the craters are permanently shaded from sunlight. The area's illumination was studied using high-resolution digital models produced from data by the Lunar Reconnaissance Orbiter. [7] The lunar surface can also reflect solar wind as energetic neutral atoms. On average, 16% of these atoms have been protons that vary based on location. These atoms have created an integral flux of backscattered hydrogen atoms due to the reflected amount of plasma that exists on the surface of the Moon. They also reveal the line boundary and the magnetic dynamics within the regions of these neutral atoms on the Moon' surface. [8]

Cold traps

Cold traps are some of the important places on the lunar south pole region in terms of possible water ice and other volatile deposits. Cold traps can contain water and ice that were originally from comets, meteorites and solar wind-induced iron reduction. From experiments and sample readings, scientists were able to confirm that cold traps do contain ice. Hydroxyl has also been found in these cold traps. The discovery of these two compounds has led to the funding of missions focusing primarily on the lunar poles using global-scale infrared detection. The ice stays in these traps because of the thermal behavior of the Moon that are controlled by thermophysical properties such as scattered sunlight, thermal re-radiation, internal heat and light given off by the Earth. [9]

Magnetic surface

There are areas of the Moon where the crust is magnetized. This is known as a magnetic anomaly due to the remnants of metal iron that was emplaced by the impactor that formed the South Pole–Aitken basin (SPA basin). However, the concentration of iron that is thought to be in the basin was not present in the mappings, as they could be too deep in the Moon's crust for the mappings to detect. Or the magnetic anomaly is caused by another factor that does not involve metallic properties. The findings were proven inadequate due to the inconsistencies between the maps that were used, and also, they were not able to detect the magnitude of the magnetic fluctuations at the Moon's surface. [10] [ needs update ]

Exploration

Missions

Lunar south polar region map (>80degS) Lunar south pole.jpg
Lunar south polar region map (>80°S)
Degree of the slopes found near the south pole of the Moon Starry night.jpg
Degree of the slopes found near the south pole of the Moon

Orbiters from several countries have explored the region around the lunar south pole. Extensive studies were conducted by the Lunar Orbiters, Clementine, Lunar Prospector, Lunar Reconnaissance Orbiter, Kaguya, and Chandrayaan-1, that discovered the presence of lunar water. NASA's LCROSS mission found a significant amount of water in Cabeus. [11] The LCROSS mission deliberately crashed into the floor of Cabeus and from samples found that it contained nearly 5% water. [12]

Lunar Reconnaissance Orbiter

The Lunar Reconnaissance Orbiter (LRO) was launched by NASA on 18 June 2009 and is still mapping the lunar south pole region. This mission will help scientists see if the lunar south pole region has enough sustainable resources to sustain a permanent crewed station. The LRO carries the Diviner Lunar Radiometer Experiment, which investigates the radiation and thermophysical properties of the south pole surface. It can detect reflected solar radiation and internal infrared emissions. The LRO Diviner is able to detect where water ice could be trapped on the surface. [9]

LCROSS

The Lunar Crater Observation and Sensing Satellite (LCROSS) was a robotic spacecraft operated by NASA. The mission was conceived as a low-cost means of determining the nature of hydrogen detected at the polar regions of the Moon. [13] Launched immediately after discovery of lunar water by Chandrayaan-1, [14] the main LCROSS mission objective was to further explore the presence of water in the form of ice in a permanently shadowed crater near a lunar polar region. [15] It was launched together with the Lunar Reconnaissance Orbiter (LRO) and it's Centaur Upper stage. It was successful in confirming water in the southern lunar crater Cabeus. [16]

Moon Impact Probe

The Moon Impact Probe (MIP) developed by the Indian Space Research Organisation (ISRO), India's national space agency, was a lunar probe that was released by ISRO's Chandrayaan-1 lunar remote sensing orbiter which in turn was launched, on 22 October 2008. The Moon Impact Probe separated from the Moon-orbiting Chandrayaan-1 on 14 November 2008, 20:06 IST and after nearly 25 minutes crashed as planned, near the rim of the crater Shackleton. With this mission India became the first to hard land or impact on the lunar South Pole.

Luna 25

Russia launched its Luna 25 lunar lander on August 10, 2023. [17] Luna-25 spent five days journeying to the Moon, then was circling the natural satellite for another five to seven days. The spacecraft then was planned to be set down in the Moon's south polar region, near the crater Boguslawsky. Luna developed an "emergency situation" that occurred during the reduction of the probe to a pre-landing orbit. The lunar lander abruptly lost communication at 2:57 p.m. (11:57 GMT). Luna 25 was a lander only, with a primary mission of proving the landing technology. The mission was carrying 30 kg (66 lb) of scientific instruments, including a robotic arm for soil samples and possible drilling hardware. [18] The launch took place on a Soyuz-2.1b rocket with Fregat upper stage, from Vostochny Cosmodrome. [19] [20]

Chandrayaan-3

On August 23, 2023 12:34 UTC, India's Chandrayaan-3 became the first lunar mission to achieve a soft landing near the lunar south pole. The mission consisted of a lander and a rover for carrying out scientific experiments. [21]

IM-1

The IM-1 Odysseus lander has taken about six days to travel from the Earth to the Moon. Once in the vicinity of the Moon, the lander spent approximately one more Earth-day orbiting the Moon. This set February 22, 2024 at 11:24 PM UTC as the lander's lunar landing date. [22] [23] The initial aim was to land within the Malapert-A crater, which is about 300 km (190 mi) from the lunar south pole. [24] [25] Later, the exact time of landing was announced as 11:24 PM UTC.[ citation needed ] Odysseus made history by becoming the first US moon landing in the 21st century.

EagleCam to record lunar landing

Just before landing, at approximately 30 m (98 ft) above the lunar surface, the Odysseus lander was planned to eject the EagleCam camera-equipped CubeSat, which would have been dropped onto the lunar surface near the lander, with an impact velocity of about 10 m/s (22 mph). However, due to complications arising from a software patch, it was decided that EagleCam would not be ejected upon landing. It was later ejected on 28 February but was partially a failure as it returned all types of data, except post IM-1 landing images that were the main aim of its mission. [26] [27] [28] [29]

Role in future exploration and observations

Geological map of the lunar south pole region Lunar south pole geology.jpg
Geological map of the lunar south pole region

The lunar south pole region is deemed to be a compelling place for future exploration missions and suitable for a lunar outpost. The permanently shadowed places on the Moon could contain ice and other minerals, which would be vital resources for future explorers. The mountain peaks near the pole are illuminated for large periods of time and could be used to provide solar energy to an outpost. With an outpost on the Moon, scientists will be able to analyze water and other volatile samples dating to the formation of the Solar System. [2]

Scientists used LOLA (Lunar Orbiter Laser Altimeter), which was a device used by NASA to provide an accurate topographic model of the Moon. [30] With this data, locations near the south pole at Connecting Ridge, which connects Shackleton to the crater de Gerlache, [7] were found that yielded sunlight for 92.27–95.65% of the time based on altitude ranging from 2 m above ground to 10 m above ground. At the same spots it was discovered that the longest continuous periods of darkness were only 3 to 5 days. [7]

The lunar south pole is a place where scientists may be able to perform unique astronomical observations of radio waves under 30 MHz. The Chinese Longjiang microsatellites were launched in May 2018 to orbit the Moon, and Longjiang-2 operated in this frequency until 31 July 2019. [31] [32] [33] [34] Before Longjiang-2, no space observatory had been able to observe astronomical radio waves in this frequency because of interference waves from equipment on Earth. The lunar south pole has mountains and basins, such as the south side of Malapert Mountain, that do not face Earth and would be an ideal place to receive such astronomical radio signals from a ground radio observatory. [35]

Resources

Lunar surface chemical composition [36]
CompoundFormulaComposition
Maria Highlands
silica SiO245.4%45.5%
alumina Al2O314.9%24.0%
lime CaO11.8%15.9%
iron(II) oxide FeO14.1%5.9%
magnesia MgO9.2%7.5%
titanium dioxide TiO23.9%0.6%
sodium oxide Na2O0.6%0.6%
Total99.9%100.0%

Solar power, oxygen, and metals are abundant resources in the south polar region. [37] By locating a lunar resource processing facility near the south pole, solar-generated electrical power will allow for nearly constant operation. [38] Elements known to be present on the lunar surface include, among others, hydrogen (H), [39] oxygen (O), silicon (Si), iron (Fe), magnesium (Mg), calcium (Ca), aluminium (Al), manganese (Mn) and titanium (Ti). Among the more abundant are oxygen, iron and silicon. The oxygen content is estimated at 45% (by weight).

Future

Visualization Shackleton Crater with Lunar South Pole visible as the thinnest illuminated rim of the half visible large Shackleton crater Shackelton crater visualization.jpg
Visualization Shackleton Crater with Lunar South Pole visible as the thinnest illuminated rim of the half visible large Shackleton crater

Blue Origin is planning a mission to the south polar region in about 2024. [40] [41] [42] The Blue Moon lander derives from the vertical landing technology used in Blue Origin's New Shepard sub-orbital rocket. [43] This would lead to a series of missions landing equipment for a crewed base in a south polar region crater using their Blue Moon lander. [41] [42]

NASA's Artemis program has proposed to land several robotic landers and rovers (CLPS) in preparation for the 2025 Artemis 3 crewed landing at the south polar region. [44]

See also

Related Research Articles

<span class="mw-page-title-main">Lander (spacecraft)</span> Type of spacecraft

A lander is a spacecraft that descends towards, then comes to rest on the surface of an astronomical body other than Earth. In contrast to an impact probe, which makes a hard landing that damages or destroys the probe upon reaching the surface, a lander makes a soft landing after which the probe remains functional.

<span class="mw-page-title-main">Chandrayaan-1</span> First lunar orbiter of Indias Chandrayaan Programme

Chandrayaan-1 was the first Indian lunar probe under the Chandrayaan programme. It was launched by the Indian Space Research Organisation (ISRO) in October 2008, and operated until August 2009. The mission included an orbiter and an impactor. India launched the spacecraft using a PSLV-XL rocket on 22 October 2008 at 00:52 UTC from Satish Dhawan Space Centre, at Sriharikota, Andhra Pradesh. The mission was a major boost to India's space program, as India researched and developed indigenous technology to explore the Moon. The vehicle was inserted into lunar orbit on 8 November 2008.

<span class="mw-page-title-main">Cabeus (crater)</span> Lunar impact crater

Cabeus is a lunar impact crater that is located about 100 km (62 mi) from the south pole of the Moon. At this location the crater is seen obliquely from Earth, and it is almost perpetually in deep shadow due to lack of sunlight. Hence, not much detail can be seen of this crater, even from orbit. Through a telescope, this crater appears near the southern limb of the Moon, to the west of the crater Malapert and to the south-southwest of Newton.

<span class="mw-page-title-main">Moon landing</span> Arrival of a spacecraft on the Moons surface

A Moon landing or lunar landing is the arrival of a spacecraft on the surface of the Moon, including both crewed and robotic missions. The first human-made object to touch the Moon was Luna 2 in 1959.

<span class="mw-page-title-main">Lunar water</span> Presence of water on the Moon

Lunar water is water that is present on the Moon. Diffuse water molecules in low concentrations can persist at the Moon's sunlit surface, as discovered by the SOFIA observatory in 2020. Gradually, water vapor is decomposed by sunlight, leaving hydrogen and oxygen lost to outer space. Scientists have found water ice in the cold, permanently shadowed craters at the Moon's poles. Water molecules are also present in the extremely thin lunar atmosphere.

<span class="mw-page-title-main">Exploration of the Moon</span> Missions to the Moon

The physical exploration of the Moon began when Luna 2, a space probe launched by the Soviet Union, made a deliberate impact on the surface of the Moon on September 14, 1959. Prior to that the only available means of exploration had been observation from Earth. The invention of the optical telescope brought about the first leap in the quality of lunar observations. Galileo Galilei is generally credited as the first person to use a telescope for astronomical purposes; having made his own telescope in 1609, the mountains and craters on the lunar surface were among his first observations using it.

<span class="mw-page-title-main">LCROSS</span> Lunar Impactor

The Lunar Crater Observation and Sensing Satellite (LCROSS) was a robotic spacecraft operated by NASA. The mission was conceived as a low-cost means of determining the nature of hydrogen detected at the polar regions of the Moon. Launched immediately after discovery of lunar water by Chandrayaan-1, the main LCROSS mission objective was to further explore the presence of water in the form of ice in a permanently shadowed crater near a lunar polar region. It was successful in confirming water in the southern lunar crater Cabeus.

<span class="mw-page-title-main">Lunar Reconnaissance Orbiter</span> NASA robotic spacecraft orbiting the Moon

The Lunar Reconnaissance Orbiter (LRO) is a NASA robotic spacecraft currently orbiting the Moon in an eccentric polar mapping orbit. Data collected by LRO have been described as essential for planning NASA's future human and robotic missions to the Moon. Its detailed mapping program is identifying safe landing sites, locating potential resources on the Moon, characterizing the radiation environment, and demonstrating new technologies.

<span class="mw-page-title-main">Moon Impact Probe</span> Lunar robotic craft developed by ISRO

The Moon Impact Probe (MIP) developed by the Indian Space Research Organisation (ISRO), India's national space agency, was a lunar probe that was released by ISRO's Chandrayaan-1 lunar remote sensing orbiter which in turn was launched, on 22 October 2008, aboard a modified version of ISRO's Polar Satellite Launch Vehicle. It discovered the presence of water on the Moon.

<span class="mw-page-title-main">Lunar rover</span> Vehicle that travels on the Moons surface

A lunar rover or Moon rover is a space exploration vehicle designed to move across the surface of the Moon. The Apollo program's Lunar Roving Vehicle was driven on the Moon by members of three American crews, Apollo 15, 16, and 17. Other rovers have been partially or fully autonomous robots, such as the Soviet Union's Lunokhods, Chinese Yutus, Indian Pragyan, and Japan's LEVs. Five countries have had operating rovers on the Moon: the Soviet Union, the United States, China, India, and Japan.

<span class="mw-page-title-main">Permanently shadowed crater</span> Permanently shadowed region of a body in the Solar System

A permanently shadowed crater is a depression on a body in the Solar System within which lies a point that is always in darkness.

<span class="mw-page-title-main">Chandrayaan programme</span> Indian Lunar exploration programme

The Chandrayaan programme also known as the Indian Lunar Exploration Programme is an ongoing series of outer space missions by the Indian Space Research Organization (ISRO) for the exploration of the Moon. The program incorporates a lunar orbiter, an impactor, a soft lander and a rover spacecraft.

The following outline is provided as an overview of and topical guide to the Moon:

<span class="mw-page-title-main">Resource Prospector</span>

Resource Prospector is a cancelled mission concept by NASA of a rover that would have performed a survey expedition on a polar region of the Moon. The rover was to attempt to detect and map the location of volatiles such as hydrogen, oxygen and lunar water which could foster more affordable and sustainable human exploration to the Moon, Mars, and other Solar System bodies.

<i>VIPER</i> (rover) Planned NASA lunar rover

VIPER is a lunar rover developed by NASA, and currently planned to be delivered to the surface of the Moon in November 2024. The rover will be tasked with prospecting for lunar resources in permanently shadowed areas in the lunar south pole region, especially by mapping the distribution and concentration of water ice. The mission builds on a previous NASA rover concept called Resource Prospector, which was cancelled in 2018.

<span class="mw-page-title-main">Chandrayaan-3</span> Indian lunar lander mission

Chandrayaan-3 is the third mission in the Chandrayaan programme, a series of lunar-exploration missions developed by the Indian Space Research Organisation (ISRO). The mission consists of a Vikram lunar lander and a Pragyan lunar rover similar to those launched aboard Chandrayaan-2 in 2019, as well as a propulsion module that carried the spacecraft from Earth orbit to lunar orbit.

Lunar Trailblazer is a planned small lunar orbiter, part of NASA's SIMPLEx program, that will detect and map water on the lunar surface to determine how its form, abundance, and location relate to geology. Its mission is to aid in the understanding of lunar water and the Moon's water cycle. Lunar Trailblazer is currently slated to launch in 2024 as a secondary payload on the IM-2 mission. The Principal Investigator (PI) of the mission is Bethany Ehlmann, a professor at Caltech.

References

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