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Did it rain and snow on Mars like Earth?

Did it rain and snow on Mars like Earth?

India Today23-04-2025

Did it rain and snow on Mars like Earth?
23 Apr, 2025
Credit: Nasa
A new study suggests that billions of years ago, Mars experienced snow or rain, creating rivers and lakes—indicating a much warmer and wetter planet than today.
Rain & Rivers
Led by Amanda Steckel, the research was published in the Journal of Geophysical Research: Planets and uses new simulations to understand Mars' ancient climate.
New Research
The study supports the idea that Mars had widespread precipitation, challenging the long-standing theory that it was always cold and dry with only occasional ice melt.
Cold-and-Dry Theory
Satellite data show valley networks on Mars similar to Earth's, especially places like Utah, suggesting formation through flowing water—not just melting ice.
Earth-Like Valley
Researchers simulated both melting ice caps and precipitation. Rainfall scenarios created more realistic valley formations across varied elevations, closely matching Mars' real terrain.
Rainfall Hypothesis
Mars' Jezero Crater, currently explored by NASA's Perseverance rover, is an example of an ancient lake fed by a strong river—likely requiring meters-deep water flow.
Perseverance Rover Hunts
While the study strengthens the warm-and-wet theory, scientists still don't fully understand how early Mars stayed warm enough for liquid water. The planet may be a snapshot of what early Earth once looked like.
Still a Mystery

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Dickson Fjord's 650-foot mega-tsunami: How a giant wave sent shockwaves worldwide
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But what exactly had triggered this steady, global beat?The answer lay in a massive natural disaster: on 16 September 2023, more than 25 million cubic metres of rock and ice—a volume large enough to fill 10,000 Olympic swimming pools—collapsed from the mountainside into Dickson Fjord. This triggered a mega-tsunami with waves reaching 650 feet high, about half the height of the Empire State waves surged along the two-mile-long fjord, smashing against cliffs and bouncing back, creating a prolonged sloshing motion known as a seiche. Unlike tsunamis, which travel outward as single giant waves, seiches occur when water oscillates repeatedly in an enclosed space. This ongoing motion produced rhythmic seismic pulses detectable around the are caused by sudden, large displacements of water—usually due to earthquakes, landslides, or volcanic eruptions—and travel as single massive waves. 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This steady pulse continued for nine days and returned briefly a month later. It was faint, unlike a typical earthquake, but strong enough to register across continents—from Alaska to Australia. Scientists were baffled. No known earthquake, volcanic eruption, or explosion had caused source was traced to the remote Dickson Fjord in East Greenland, a narrow inlet bordered by towering cliffs. But what exactly had triggered this steady, global beat?The answer lay in a massive natural disaster: on 16 September 2023, more than 25 million cubic metres of rock and ice—a volume large enough to fill 10,000 Olympic swimming pools—collapsed from the mountainside into Dickson Fjord. This triggered a mega-tsunami with waves reaching 650 feet high, about half the height of the Empire State waves surged along the two-mile-long fjord, smashing against cliffs and bouncing back, creating a prolonged sloshing motion known as a seiche. Unlike tsunamis, which travel outward as single giant waves, seiches occur when water oscillates repeatedly in an enclosed space. This ongoing motion produced rhythmic seismic pulses detectable around the are caused by sudden, large displacements of water—usually due to earthquakes, landslides, or volcanic eruptions—and travel as single massive waves. Seiches, however, are standing waves formed in enclosed or semi-enclosed bodies of water, like lakes or fjords. They can be triggered by landslides or strong winds, causing the water to rock back and forth in a steady Dickson Fjord, the narrow, enclosed shape trapped the tsunami energy. The waves couldn't escape, so they kept bouncing, sending low-frequency seismic energy through the Earth's crust for mystery was unraveled thanks to the Surface Water and Ocean Topography (SWOT) satellite, a joint NASA and French space agency mission launched in December 2022. Unlike traditional satellites that scan narrow lines, SWOT uses Ka-band Radar Interferometer (KaRIn) technology to map wide swaths of ocean surface in high SWOT data, researchers observed subtle water elevation changes—slopes of up to two metres—sloshing across the fjord. These shifts matched the oscillations expected from fill gaps, scientists employed machine learning to simulate wave behaviour over time. They also analysed crustal deformation data from sensors thousands of kilometres away, plus weather and tidal records, ruling out other causes like researcher Thomas Monahan, a University of Oxford engineering student, said, 'Climate change is giving rise to new, unseen extremes. These changes are happening fastest in remote areas like the Arctic, where our ability to monitor them has historically been limited.'The underlying cause of the landslide was the rapid melting of Greenland's glaciers. As glacier ice shrinks, it removes the natural support holding mountainsides in place. 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To fully harness these data, we need to innovate using both machine learning and ocean physics.'A Danish military vessel patrolled the fjord three days after the first pulse but observed nothing unusual. This shows how even massive natural events can leave little trace without sophisticated monitoring are now searching through historical seismic data for similar slow, rhythmic pulses. Carl Ebeling from UC San Diego said, 'This shows there is stuff out there that we still don't understand and haven't seen before.'Every new discovery will improve forecasts of how landslides, fjord shapes, and water depth interact. The hope is to provide early warnings that could save lives in remote, high-latitude silent, powerful waves in Greenland's fjord prove one thing: the most isolated places on Earth are changing fast—and we must listen carefully to what they tell us.

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