A sudden rise in aerosols makes clouds more active for about a day. Then the effect fades as the atmosphere adjusts and warms aloft, reducing the contrast that helps clouds grow, according to cloud-resolving model simulations…
Source: Nature Geoscience | Springer Nature Limited
Nature Geoscience | Springer Nature Limited
- An Arctic ice shelf in the Last Glacial Maximum rivalled Antarctica’s modern ice shelves
- The Baffin Bay Ice Shelf stabilized three adjacent ice sheets during the last glacial period
- Antarctic marine-based ice destabilized when warming outpaces solid-Earth feedbacks
- Trade-offs between soil inorganic and organic carbon driven by multiple global environmental changes
- Decolonize soil erosion modelling
- Palaeoclimate constraints narrow uncertainty in future Arctic winter sea ice projections
- Progressive oxidative weathering raised sub-arc mantle fugacity on the Archaean Earth
- Dry pebble rain could have delivered water to Earth through hydrogen reduction of iron oxide
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