Lunar Reconnaissance Orbiter
The Lunar Reconnaissance Orbiter carries roughly 1.6 million names on a microchip. They belong to ordinary people who answered a NASA invitation before a deadline in July 2008, each asking to be sent, in some small way, to the Moon. The spacecraft that carries those names launched on the 18th of June 2009, and it has not stopped working since. It maps craters, measures radiation, hunts for water ice in permanently shadowed places, and photographs the exact spots where astronauts once walked. How does one spacecraft do all of that at once, and why does it matter so much for what comes next on the Moon?
LRO was the first United States mission to the Moon in over ten years. That gap had left NASA without fresh, high-resolution data for planning any return. Developed at NASA's Goddard Space Flight Center, the spacecraft weighed 1,916 kilograms at launch, making it one of the agency's larger robotic probes. Its mission was planned to last one year, though NASA extended it repeatedly after each review. Getting LRO to the pad was not straightforward. The original launch date of October 2008 slipped first to April, then to the 17th of June 2009, as the spacecraft moved through a thermal vacuum chamber for testing and a priority military launch took precedence. One more day passed before liftoff because Space Shuttle Endeavour needed a window to attempt its own mission, STS-127, after a hydrogen fuel leak had scrubbed an earlier attempt. LRO finally lifted off on June 18, aimed at a point ahead of the Moon rather than at the Moon itself, requiring a mid-course correction along the way.
Six scientific instruments and one technology demonstration ride aboard LRO, each assigned a different question. The Cosmic Ray Telescope for the Effects of Radiation, known as CRaTER, measures how charged particles transfer energy in lunar orbit and what that means for living tissue. Diviner reads the thermal emission from the lunar surface, producing temperature maps that future crews will rely on before they choose where to stand. The Lyman-Alpha Mapping Project, or LAMP, uses ultraviolet light from distant stars, as well as hydrogen atoms diffused through the Solar System, to peer into permanently shadowed craters in search of water ice. The Lunar Exploration Neutron Detector, LEND, also maps possible near-surface water ice by measuring neutrons scattered from the surface. The Lunar Orbiter Laser Altimeter, LOLA, fires a laser to build a precise global topographic model; on the 17th of December 2010, LOLA's data became the basis for the most accurate topographic map of the Moon ever released. The two Narrow Angle Cameras of the Lunar Reconnaissance Orbiter Camera system can resolve objects as small as 0.5 meters across from an altitude of about 50 km, which is sharp enough to see the Lunar Roving Vehicles and the descent stages of the Lunar Modules left behind by Apollo crews. The Mini-RF radar, though it suffered a transmitter anomaly on the 4th of January 2011, had already collected more than 400 strips of radar data before the failure.
On the 9th of October 2009, the companion spacecraft LCROSS sent two impactors into Cabeus crater near the Moon's south pole at 11:31 and 11:36 UTC. Preliminary results from that mission indicated the presence of both water and hydroxyl, an ion related to water. LRO had its own part in the search. On the 21st of August 2009, LRO and the Indian orbiter Chandrayaan-1 attempted a bistatic radar experiment to detect water ice on the surface, though that particular test was unsuccessful. The hunt continued at a different angle in July 2024, when analysis of LRO radar data confirmed an underground cave in Mare Tranquillitatis, the ancient lava plain where Neil Armstrong and Buzz Aldrin first walked. The cave entrance is about 45 metres wide, with a passage running at least 80 metres long; such a structure could shelter future crews from radiation and extreme surface temperatures.
By March 2011, LRO's seven instruments had delivered more than 192 terabytes of data, surpassing the combined total from every other planetary mission flown to that point. That volume is possible partly because the Moon is close, partly because LRO has a dedicated ground station, and partly because it does not compete for time on the Deep Space Network. The Wide Angle Camera on the LROC system covers 100 meters per pixel across a 60 km swath, producing the global mosaic used by scientists worldwide. By March 2016, the LROC team had used 14,092 pairs of images taken at different times to discover more than 47,000 new surface splotches where recent impacts had changed the soil's reflectance. In September 2015, the same temporal-pairing method revealed more than 3,000 lobate scarps distributed across the entire globe, a pattern suggesting the Moon is slowly shrinking as it cools, with some influence from Earth's gravitational tides.
One of LRO's quieter tasks has been documenting the archaeology of space exploration. The Narrow Angle Cameras have flown several times over each Apollo landing site at roughly 50 km altitude, producing images sharp enough to show equipment, cables, and the shadows of descent stages. In January 2013, a different kind of history was made when NASA used the LOLA instrument as a receiver, beaming an image of the Mona Lisa from the Next Generation Satellite Laser Ranging station at Goddard Space Flight Center in Greenbelt, Maryland. It was a one-way laser communication test, but it proved that data could travel to a spacecraft in lunar orbit through a laser link. In 2019, LRO located the crash site of India's Vikram lander, and in 2024 it confirmed the precise touchdown point of Japan's SLIM lander, the first successful soft landing by a Japanese spacecraft. The total cost of the mission stands at $583 million, of which $504 million covered LRO itself and $79 million covered LCROSS. With enough fuel to keep operating until 2027, the orbiter continues to add to a record it has been building since it first entered lunar orbit on the 23rd of June 2009.
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Common questions
When was the Lunar Reconnaissance Orbiter launched?
The Lunar Reconnaissance Orbiter launched on the 18th of June 2009, from Cape Canaveral Air Force Station. It entered lunar orbit on the 23rd of June 2009 after a four-and-a-half-day journey from Earth.
How much did the Lunar Reconnaissance Orbiter mission cost?
The total cost of the LRO mission is reported as $583 million. Of that amount, $504 million covered the main LRO probe and $79 million covered the companion LCROSS satellite.
What instruments does the Lunar Reconnaissance Orbiter carry?
LRO carries six scientific instruments and one technology demonstration: CRaTER, Diviner, LAMP, LEND, LOLA, the Lunar Reconnaissance Orbiter Camera (with Narrow Angle and Wide Angle cameras), and the Mini-RF radar. Together they map topography, search for water ice, measure radiation, and image the surface at resolutions as fine as 0.5 meters.
Has the Lunar Reconnaissance Orbiter found water on the Moon?
LRO contributed to the water search through multiple methods. The companion mission LCROSS impacted Cabeus crater in October 2009 and preliminary results indicated water and hydroxyl. In July 2024, analysis of LRO radar data confirmed an underground cave in Mare Tranquillitatis roughly 45 metres wide and at least 80 metres long, which may hold scientific clues about subsurface water-ice deposits.
How much data has the Lunar Reconnaissance Orbiter collected?
By March 2011, LRO's instruments had delivered more than 192 terabytes of data. NASA noted at that point that LRO had already collected as much data as all other planetary missions combined.
Can the Lunar Reconnaissance Orbiter photograph the Apollo landing sites?
Yes. The Narrow Angle Cameras on LRO image pixels about 0.5 metres across from an altitude of roughly 50 km, making the Lunar Roving Vehicles, Lunar Module descent stages, and other equipment left by Apollo crews clearly visible in the images.
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