Scientists Measured the Coldest Natural Surface on Earth
New satellite analysis has revealed surface temperatures on the East Antarctic Plateau dropping below -98°C, surpassing the previous ground-based record. These extreme cold pools form in shallow depressions where dense, cold air accumulates under ...


Unlike traditional meteorological readings taken 2 meters above the ground, these new measurements focused on surface skin temperature, the temperature of the snow itself. While surface temperatures can be lower than air temperatures, the magnitude of this extreme cooling surprised researchers and prompted a detailed analysis of atmospheric and topographic conditions.
How Extreme Cooling Happens
The East Antarctic Plateau sits at elevations exceeding 3,000 meters, where thin, dry air already promotes heat loss. During the austral winter, the region experiences continuous darkness for months, eliminating incoming solar radiation. Under clear skies, the snow surface radiates infrared energy directly into space, allowing rapid cooling through radiative heat loss.Researchers discovered that the coldest temperatures occurred not on exposed ridges, but inside shallow depressions in the ice sheet. These subtle dips in the landscape allow cold, dense air to drain downward and accumulate, creating small “cold pools” where temperatures can drop dramatically. Ted Scambos, lead author of the study and senior research scientist at the National Snow and Ice Data Center, explained that these depressions function like natural basins where “cold air settles and continues to cool under clear sky conditions.” Satellite data collected over several winters showed that temperatures in these pockets repeatedly reached between minus 90 and minus 98 degrees Celsius, with some brief readings possibly dipping slightly lower. The research team cross-validated satellite observations using multiple sensors to ensure accuracy.
Implications for Climate Science
Understanding extreme surface cooling is important for refining climate models, particularly those that simulate polar heat exchange and atmospheric circulation. The Antarctic Plateau plays a critical role in regulating global heat balance because it radiates significant energy back into space during winter. These newly identified cold zones improve estimates of the amount of energy the continent emits and of how surface processes interact with atmospheric dynamics.Although these extreme temperatures occur in remote and sparsely populated areas, their existence demonstrates how subtle geographic features can amplify climate extremes. Scientists continue to monitor these sites to assess whether changes in cloud cover, wind patterns, or atmospheric composition alter the frequency or intensity of such record-breaking cooling events in a warming world.
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