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  1. 5 giu 2024 · Our findings reveal the Eocene as a transition period from >40 million years of relative tectonic quiescence toward reactivation of the West Antarctic Rift System, coinciding with incipient volcanism, rise of the Transantarctic Mountains, and renewed sedimentation under temperate climate conditions.

  2. 4 giorni fa · Synopsis. An Inconvenient Truth presents in film form an illustrated talk on climate by Al Gore, aimed at alerting the public to an increasing "planetary emergency" due to global warming, and shows re-enacted incidents from his life story which influenced his concerns about environmental issues.

  3. 1 giorno fa · Bradley and his team’s findings were detailed in a new study, “Tipping point in ice-sheet grounding-zone melting due to ocean water intrusion,” co-authored with Ian J. Hewitt and published in the journal Nature Geoscience on June 25, 2024. Micah Hanks is the Editor-in-Chief and Co-Founder of The Debrief.

  4. 10 giu 2024 · Two decades of deep ice cores from Antarctica. In June 2004, the results of an ambitious Antarctic ice-drilling project brought insight into hundreds of thousands of years of climatic...

  5. 10 giu 2024 · Satellite imagery paints a vivid picture, revealing how climate change and human activities reshape this fragile continent. This space-based perspective fuels scientific discovery and underscores the importance of global cooperation in protecting Antarctica for future generations.

  6. 2 giorni fa · Coastal waters along the western Antarctic Peninsula are highly productive polar ecosystems that are vulnerable to anthropogenic change. Rising temperatures have shortened the duration, extent, and thickness of sea ice, affecting primary productivity (Schofield et al. 2018) primarily through the availability of light (Joy-Warren et al. 2019).

  7. 15 giu 2024 · The warm water is carried toward the cavities over the relatively shallow continental shelves by ocean currents. The Antarctic Slope Current, a current that flows along the continental slope between cold and warm water masses, limits the amount of warm water that enters the continental shelf.

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