A new study by the Indian Space Research Organisation (ISRO) using high resolution data from the Chandrayaan 2 orbiter has identified what may be some of the clearest evidence yet of subsurface water ice hidden beneath craters near the Moon south pole, with findings reported widely on 28 May 2026 and published in the peer reviewed journal npj Space Exploration. The team used observations from the Dual Frequency Synthetic Aperture Radar (DFSAR) aboard Chandrayaan 2 launched in July 2019, which is the first fully polarimetric radar instrument ever sent to study the Moon, operating in L and S band microwave frequencies. The DFSAR can penetrate up to a few metres beneath the lunar regolith and is therefore capable of detecting ice deposits that are not visible to optical sensors. The study identified radar signatures consistent with buried water ice beneath four doubly shadowed craters in the lunar south polar region. The strongest evidence was found in a 1.1 kilometre wide crater located within the larger Faustini crater near the Moon south pole, where the Circular Polarisation Ratio values are anomalously high, a tell tale signature of water ice mixed with regolith. Doubly shadowed craters are zones permanently in shadow that act as cold traps trapping volatiles for billions of years. The discovery has major implications for ISRO Chandrayaan 4 sample return mission, the planned Lunar Polar Exploration Mission (LUPEX) jointly with Japan JAXA, the Bharatiya Antariksh Station 2035 and crewed lunar landing by 2040 announced by Prime Minister Narendra Modi, as in situ water ice is critical for life support, propellant and human settlement at the lunar south pole.
ISRO Chandrayaan 2 Dual Frequency Synthetic Aperture Radar Study Published in npj Space Exploration With Findings Reported on 28 May 2026 Identifies Radar Signatures Consistent With Subsurface Water Ice Beneath Doubly Shadowed Craters Near the Lunar South Pole With the Strongest Evidence in a 1.1 Kilometre Crater Inside the Larger Faustini Crater Marking a Major Boost for Future Crewed Lunar Missions and Resource Utilisation
An ISRO study published in npj Space Exploration and reported on 28 May 2026 uses Chandrayaan 2 DFSAR data to identify subsurface water ice beneath four doubly shadowed craters near the lunar south pole, with strongest evidence in a 1.1 km crater inside Faustini, supporting Chandrayaan 4, LUPEX and the 2040 crewed lunar landing.
Key facts
- ISRO Chandrayaan 2 DFSAR radar study reported on 28 May 2026 and published in npj Space Exploration identifies subsurface water ice beneath four doubly shadowed craters near the lunar south pole
- The Dual Frequency Synthetic Aperture Radar DFSAR is the first fully polarimetric radar instrument sent to study the Moon operating in L and S band microwave frequencies and can penetrate a few metres beneath the regolith
- Strongest evidence of subsurface ice was found in a 1.1 kilometre wide crater inside the larger Faustini crater near the Moon south pole with anomalously high Circular Polarisation Ratio values
- Doubly shadowed craters act as cold traps trapping volatiles including water ice for billions of years and are prime targets for in situ resource utilisation
- Findings strengthen ISRO Chandrayaan 4 sample return mission and the planned Lunar Polar Exploration Mission LUPEX jointly with Japan JAXA
- Discovery directly supports the Bharatiya Antariksh Station 2035 and crewed lunar landing by 2040 announced by Prime Minister Narendra Modi by providing in situ resources for life support and propellant
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According to the ISRO Chandrayaan 2 study reported on 28 May 2026, in which specific crater near the Moon south pole was the strongest evidence of subsurface water ice found?
The strongest evidence of subsurface water ice was found in a 1.1 kilometre wide crater located within the larger Faustini crater near the Moon south pole. The DFSAR data showed anomalously high Circular Polarisation Ratio values in this crater, a tell tale signature of water ice mixed with regolith.
Source: ISRO and npj Space Exploration
Frequently asked questions
What did the ISRO Chandrayaan 2 radar study reported on 28 May 2026 reveal?
The study using the Dual Frequency Synthetic Aperture Radar DFSAR aboard Chandrayaan 2 revealed radar signatures consistent with subsurface water ice beneath four doubly shadowed craters near the lunar south pole, with the strongest evidence in a 1.1 kilometre wide crater inside the larger Faustini crater.
What is the DFSAR instrument and what makes it unique?
The Dual Frequency Synthetic Aperture Radar (DFSAR) is the first fully polarimetric radar instrument sent to study the Moon. It operates in L and S band microwave frequencies and can penetrate a few metres beneath the lunar regolith, allowing it to detect ice deposits not visible to optical sensors.
What are doubly shadowed craters and why are they significant?
Doubly shadowed craters are zones near the lunar poles that are permanently in shadow and act as cold traps, trapping volatiles including water ice for billions of years. They are prime targets for in situ resource utilisation for future lunar missions.
How does this discovery support ISRO future Moon missions?
The discovery directly supports ISRO Chandrayaan 4 sample return mission, the planned Lunar Polar Exploration Mission (LUPEX) jointly with Japan JAXA, the Bharatiya Antariksh Station 2035 and the crewed lunar landing by 2040 announced by Prime Minister Narendra Modi, by confirming the availability of in situ water resources for life support and propellant.
Where was the study published?
The study was published in the peer reviewed journal npj Space Exploration and the findings were widely reported in Indian and international media on 28 May 2026.
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