Showing posts with label IAU. Show all posts
Showing posts with label IAU. Show all posts

Tuesday, January 1, 2013

How are places on the Moon named?

Map of the Moon by Grimaldi and Riccioli, 1651. Most of the names on this map are still in use today.
Paul D. Spudis
The Once & Future Moon
Smithsonian Air & Space

The Moon is remarkable for the variety and unusual nature of the names of its surface features.  The dark, smooth maria are named for weather or states of mind (Sea of Rains, Sea of Tranquility) while many of the abundant craters of the Moon are named for famous scientists, philosophers, mathematicians and explorers.  Before the advent of the space age, only the near side of the Moon was visible from Earth, although most scientists believed that the far side probably looked exactly like the facing one. (How wrong they were!)  Naturally, once we had the ability to see uncharted lunar territory, a new era of name assignment commenced.  But even now, many lunar craters and features await something more than mere coordinates.

The drawings of the Moon in 1610 by Galileo show craters and mountain ranges but he did not assign names to them.  As telescopes improved, revealing finer surface details, several maps appeared with names bestowed by their astronomer authors to flatter patrons or express their nationalism.  Most of those early names have been forgotten to history.  In 1651, an influential map by Jesuit astronomers Grimaldi and Riccioli became the foundation for the official naming reference guide that we use today.

With the flight of the Luna 3 probe in 1959, the Soviet Union was the first nation to image the far side of the Moon.  To the surprise of most, large regions of maria (so prominent on the near side) were mostly missing from the far side.  Although the first images were of very low quality, the Soviets couldn’t resist the urge to name newly discovered features for a variety of Russian heroes and place names, such as Tsiolkovsky and the Sea of Moscow.  Some new “features” were misidentified because of the low resolution – the name “Soviet Mountains” (no longer used) was given to a bright linear streak across the far side globe (a feature that turned out to be a long ray from the fresh crater Giordano Bruno and not a mountain range).

Over subsequent years, as both American and Soviet spacecraft filled in the far side coverage with increasingly higher quality images, most major far side craters received names of various scientists and engineers.   From around the world, a mixed bag of names were submitted to the International Astronomical Union (IAU – the body of scientists who authorize the names of planetary surface features) for consideration and approval.  Although some were historically significant, many were people with whom few were familiar.

Though NASA does not have the authority to assign names to features on the Moon, an informal practice of naming landmarks was common during the Apollo missions.  Names were given to the small craters and mountains near each landing site (e.g., Shorty, St. George, Stone Mountain) but official names were used as well (e.g., Hadley Rille).  NASA adopts informal names for the same reason that names are given to geographical features on Earth – as shorthand to refer to landmarks and other mapped features.  The most recent illustration of this practice occurred on December 17, 2012 when NASA named the location where the deliberately de-orbited GRAIL spacecraft crashed onto the Moon near the crater Goldschmidt (73°N, 4°W) the Sally K. Ride Impact Site.  Sally thus joins other women of science and note who have lunar features named for them – Hypatia, Caroline Herschel and Marie Curie, among others.  Most of the informal names assigned during Apollo were later given “official” status by the IAU.

The Apollo basin (a 540 km diameter crater on the southwestern far side) was named to honor the Apollo missions – the only crater on the Moon so designated.  Within a few years of their missions, smaller craters were named for the living crews of Apollo 8 (Borman, Lovell and Anders) and Apollo 11 (Armstrong, Aldrin and Collins).  Also located around the Apollo basin are craters named for deceased astronauts and NASA employees, including the lost crews of Apollo 1 and the lost crews of the final missions of the Challenger and Columbia Space Shuttles.  It is appropriate that some feature honors humanity’s first efforts to reach the Moon, as well as others who gave their lives pioneering space.  In a similar vein, craters near the poles of the Moon tend to be named for famous polar scientists and explorers, such as Nansen, Shackleton, and Amundsen.

Other than these exceptions, the location of specifically named craters has little rhyme or reason.  Neither scientific prominence nor contribution guarantees any crater-endowed immortality.  Copernicus and Archimedes are rightly honored with spectacular craters named for them.  But Galileo and Newton (titans in the history of science) are fobbed off with insignificant or barely detectable features.  One of the most prominent craters on the Moon is named for the astronomer Tycho Brahe, an eccentric who spent most of his career trying to validate a variant of the Earth-centered, Ptolemaic model of the Solar System (Ptolemy also has a prominent crater in the center of the near side named for him).  It’s not clear why Riccioli assigned the names he did to these craters, though he cannot be blamed for giving Newton short shrift, as the future Sir Isaac was only nine years old when the Grimaldi and Riccioli map was published.

It is possible to both suggest a name and to propose a crater for that name, though the IAU is not obliged to accept either.  Often, a suggested name is approved but assigned to a different crater.  Currently, the guidelines for submission and assignment of new names for lunar craters are: 1) a scientist or explorer who has made some significant contribution, preferably to the study of the Moon and planets; 2) deceased for at least three years before a crater name becomes official; 3) it cannot duplicate any existing lunar name.

In 2005, I proposed the name Ryder (to honor my colleague Graham Ryder, a lunar scientist who passed away in 2002) and suggested a small, bright crater on the far side to carry his name.  Both suggestions were adopted.  We have since found that Ryder crater is actually quite a geologically spectacular feature (Graham would be proud of his namesake).  In a truly singular event, the crater Shoemaker (named in 2000 and located near the south pole of the Moon) actually contains some of Gene Shoemaker’s remains – a small portion of his ashes was carried aboard the Lunar Prospector spacecraft in 1998.  At the conclusion of that mission, the vehicle was crashed into the south polar crater that was subsequently named for him.

We don’t know what the IAU will do concerning the designation of the Sally K. Ride Impact Site but as history suggests, granting of official status is not guaranteed.  No matter – we will continue to assign names to features as needed and the IAU will do what they do.  In the early 1970s, the IAU (by fiat) abolished the famous Mädler nomenclature system (wherein a small, nearby crater is given the name of a large neighbor plus a letter, such as Copernicus H).  Most working lunar scientists stubbornly refused to accept this decision and continued using the old crater names.  After 30 years of bureaucratic intractability, the IAU finally surrendered and formally adopted the Mädler system.

Official or not, with the passage of time, named lunar landmarks will become familiar to those visiting and working on our nearest neighbor.  Perhaps interesting monikers will be attached by those locals, as is done here on Earth when we assign nicknames to places – like the Big Apple, the Windy City, the Big Easy and the City by the Bay.

Just publishedThe Clementine Atlas of the Moon, Revised Edition, an updated atlas and reference guide to lunar features, by Ben Bussey and yours truly.

Originally published at his Smithsonian Air & Space Magazine blog "The Once and Future Moon," Dr. Spudis is a senior staff scientist at the Lunar and Planetary Institute. The opinions expressed are those of the author and are better informed than average.

Tuesday, July 3, 2012

Craters near Lunokhod-1 officially named

Luna 17, the lander that carried Lunokhod 1 to the surface; debarking ramps for the rover visible extending down to the surface to the right. Many rover tracks are visible around the lander and throughout LROC Narrow Angle Camera (NAC) frame M175502049RE, LRO orbit 10998, November 9, 2011. View the original contextual image with enlarged inset, HERE [NASA/GSFC/Arizona State University].
Olga Zakutnyaya
The Voice of Russia
 

A number of moon craters in the vicinity of Lunokhod–1 lunar rover have been given their own names. They were named in honor of the crew members of the first self-propelled vehicle on the surface of the celestial body.

The experiment carried out more than 40 years ago is to be repeated in the course of “Luna-Resource” expedition which should be launched no earlier than 2015.

The International Astronomical Union has approved 12 new names for small craters on the Moon, and now they have names of the members of the first lunar expedition and scientists who were involved in the project. Despite the fact that these people were not able to walk on the Moon’s surface themselves, they were the ones who led Lunokhod–1 – the first planet rover on the surface of an alien celestial body. All craters are located in the area of the “Sea of Rain” (Mare Imbrium) where the landing vehicle of Luna-17 interplanetary automatic station soft-landed in November 1970. It delivered Lunokhod lunar rover onto the Moon’s surface. All craters are comparatively small, their diameter ranging from 100 to 400 meters.

Thus, the names of Albert, Borya, Gena (in honor of the navigator Gabdulkhai Latypov), Igor, Kolya, Kostya, Leonid, Nikolya, Slava, Valera, Vasya, and Vitya appeared on the Moon.

The Luna-17 spacecraft was built by the design and construction bureau of the machine-engineering plant named after S.A. Lavochkin (now NPO Lavochkin). Lunokhod-1 was equipped with a set of scientific devices to explore the lunar soil. In the course of 10 months that it was working on the Moon, the rover traveled over 10.5 kilometers and sent back to Earth information about the mineral composition and characteristics of the lunar surface.

Lunokhod 1 rover in its final parking place (38.315°N, 324.992°E) on the surface of Mare Imbrium. LROC Narrow Angle Camera (NAC) observation M175502049RE, orbit 10998, November 9, 2011, resolution 33 cm per pixel. View original Featured Image released March 14, 2012 (with enlarged inset) HERE. [NASA/GSFC/Arizona State University].
Lunokhod-1 was controlled remotely via the center for space communications by two crews – five people each who worked in shifts. Each crew consisted of a commander, a driver, a navigator, a flight engineer, and a high gain antenna operator. Thus there were 10 people all together, plus a reserve driver and reserve high gain antenna operator.

Even though by the time Lunokhod-1 was launched American astronauts had already landed on the Moon, the soviet rover was no less a remarkable scientific and technical achievement. Unfortunately, at that time, the meaning of this achievement was overshadowed by the defeat in the race to put a man on the moon. Lunokhod-1, with all its novelty and complexity, was more of a consolation prize. At least that was the general attitude – and analysts might object, of course. Sadly, it was what determined the further development of the lunar program. After the improved version Lunokhod-2 in 1973, there was Lunokhod-3 which never made it to the Moon. As a result, the Lunar Program of the USSR was suspended. Forty years on there has been little progress.

Today it can be said that it was a mistake. Weak consolation might be the fact that space programs in other countries primarily in the United States have also been suspended. However, the comparison might not be accurate – paradoxically as it may sound as though the soviet moon explorations at the end of the “manned moon race” were in a better state (if not financially from the strategic point of view). A continuation of manned expeditions demanded huge resources and clear goals, which probably did not exist at that time. Autonomous expeditions were easier from the point of view of their preparation but brought back much more scientific results. Besides, by that time, complicated initial stages with lots of failures were overcome and so reliability was higher.

Far western 1970 Landing Zone of the Soviet Union's Luna 17, and the final parking spot of the first remote-operated lunar rover, Lunokhod-1. The French-built laser reflector array deployed from the Lunokhod eluded detection for four decades until its precise location was reacquired by the LROC Narrow Angle Camera in 2009. It's relocation added vital precision to measurements of the Earth-Moon distance that may answer important questions in astrophysics. LROC Wide Angle Camera 100 meter Global Mosaic overlaid upon LOLA topography and assembled using the NASA LMMP ILIADS application [NASA/GSFC/LMMP/Arizona State University].
Something similar is happening to NASA’s Mars exploration program. A long and ongoing exploration of the planet with more and more sophisticated and complex tasks resulted in the fact that the US became a true leader in the Mars programs. That was, in fact, the main argument by scholars who objected to cuts in NASA’s planetary space budget in 2013. In their opinion to lose such an important scientific and technical foundation would be a poor strategic move.

The current plans of Russia in the area of space exploration include returning to the Moon with landing vehicles and a mini-rover – a self-propelled machine which is being developed by an Indian organization for the purposes of the Luna-Resource program. It is planned to repeat lunar soil collection considering previous experiences. If in the course of the first expeditions the soil was collected only in the places of landing – now the goal is to combine the operation of the mini-rover and returning spacecraft. The mini-rover is to determine the most interesting spots and collect soil from them and then the spacecraft should return the samples to the Earth.

New Names Approved for Twelve Small Lunar Craters - The Working Group for Planetary System Nomenclature has approved 12 new names for small craters on the Moon: Albert, Borya, Gena, Igor, Kolya, Kostya, Leonid, Nikolya, Slava, Valera, Vasya, and Vitya. For details, see the map of LAC 24 and the Lunokhod-1 traverse map in the Gazetteer of Planetary Nomenclature [USGS].
Yet as of now these are only plans. Information from the Moon is coming daily. NASA LRO and GRAIL spacecraft continue to work in the Moon’s orbit (two spacecraft which measure lunar gravity fields). Several days ago, the NASA LRO mission published recent images of the lava fields formed as a result of asteroid impacts. The images were taken by LROC – Lunar Reconnaissance Orbiter Camera. This camera is also connected to the Lunokhods – in 2010, the first high resolution images were printed and it was possible to see Lunokhod-1 and the landing spacecraft and the wheel tracks. Interesting that in the same year a group of American scientists announced that they had managed to intercept a pulse from a laser retroreflector on Lunokhod-1.

It is probable that these circumstances have raised the interest in the Lunokhod program again. Naturally, recognition of the achievements of the soviet scientists is satisfying on the one hand, but on the other the interest is mostly coming from western institutions and space lovers. Without the LROC images, the “favourite lunar tractor” would be remembered only by those who are truly loyal to space science. That is why one of the tasks of the future lunar program is not only to learn again how to land and control spacecraft on the Moon, but also how to inform people about it in plain language, and on a regular basis.

Related: Lunokhod-1 revisited (March 15, 2012)

Wednesday, October 14, 2009

Crater not named for John Lennon, yet...



Lunar Picture of the Day (LPOD) on Oct. 11, 2009, as noted by Charles A. Wood of the long-established web wiki, was Lunar Orbiter IV-086-H2 (not yet restored by LOIRP) notes in passing news reports to the contrary notwithstanding, the bright 6 kilometer-wide crater Daniell D (35.97°N, 25.88°E) has not been named "John Lennon Peace" by an official-sounding mercenary organization called the "International Lunar Geographic Society."

Until the Moon declares its independence and a provisional government is established, such honors will continue to be bestowed by the internationally-recognized International Astronomical Union, or IAU.

USGS Astrogeology: Gazetteer of Planetary Nomenclature.