Ice
Site news
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Although climate models predicted Antarctic sea ice would steadily dwindle, its extent grew for decades until 2016. A new study finds the ice finally receded when wind-driven upwelling unleashed warmer, deeper water.
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For the first time, researchers report that Arctic algae can hustle along in -15 C – the lowest-temperature movement ever recorded in complex, living cells. This discovery raises new questions about how algal communities regulate the overall health of the Arctic environment.
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Stanford researchers found increased meltwater and rain explain 60% of a decades-long mismatch between predicted and observed temperatures in the ocean around Antarctica.
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Stanford researchers have combined machine learning with high-resolution satellite and airplane observations to understand the physics behind large-scale ice movements in Antarctica. The results show that current models are missing key complexity needed to accurately predict the dynamics and mass loss of the Antarctic ice sheet now and in the future.
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Stanford researchers have created an open-source tool so other scientists can make ice-penetrating radar systems at a fraction of the cost of current methods. Ice-penetrating radar is a core tool used by glaciologists monitoring how ice sheets contribute to rising sea levels.
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The possibility of detecting a pocket of habitable water under the surface of Europa is just one of the reasons to be excited about NASA's mission, says Dustin Schroeder, an expert in using radar to assess glaciers and a member of Clipper's science team.
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Stanford researchers have found large thawed or close-to-thawed areas under coastal portions of the ice sheet that holds back glaciers in the Wilkes Subglacial Basin.
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Ching-Yao Lai combines her passion for physics with climate science to better understand Earth’s polar ice sheets and how they contribute to climate change.
