Earth shows mysterious east-west albedo symmetry

Researchers have identified a second line of symmetry dividing Earth into halves with equal reflectivity along the 27° east and 153° west meridians. The finding, based on 25 years of satellite data, reveals unexpected balance in clear-sky albedo, cloud reflectivity and ice-free ocean coverage. It may connect to the El Niño-Southern Oscillation and affect future geoengineering plans.

A team led by Jianhao Zhang at the National Oceanic and Atmospheric Administration uncovered the east-west division after analysing satellite records. The symmetry has held steady across the full observation period despite year-to-year shifts tied to ENSO phases. Zhang noted that the triple balance in land-ocean distribution, clear-sky reflection and cloudy-sky reflection makes the pattern unlikely to be random. Øivind Hodnebrog of the Centre for International Climate Research agreed the feature appears robust and potentially linked to major climate variability. Martin Jucker at the University of New South Wales cautioned it could still prove coincidental given global atmospheric circulation. Zhang added that stronger understanding of cloud and circulation responses is needed before assessing geoengineering impacts. Unlike north-south albedo symmetry, which shows signs of weakening, the east-west line remains stable in current models.

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A patch of cooling ocean south-east of Greenland, known as the cold blob, is likely caused by a slowdown in the Atlantic Meridional Overturning Circulation, according to new research. The findings add to concerns about potential future climate impacts in Europe and beyond. Scientists remain divided on the exact causes.

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Low-lying clouds have expanded since 1979, reflecting sunlight and reducing energy absorbed at Earth's surface by 0.32 watts per square metre. Researchers now warn this cooling effect could soon reverse and speed up global warming.

China’s Chang’e-6 mission returned lunar soil that shows solar wind particles reached greater depths on the Moon’s far side than on the near side. The difference stems from Earth’s magnetosphere, which slows incoming particles that strike the near side.

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China and Europe launched their first jointly developed satellite on Tuesday to explore Earth’s magnetic shield against solar wind. The mission, named SMILE, stems from a 2015 project between the Chinese Academy of Sciences and the European Space Agency.

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