Early dynamo models fail because they require unrealistic parameters that contradict both physical estimates and planetary constraints, undermining their ability to explain Earth’s early magnetic field.
Recent research highlights that the role of calcifying plankton in regulating global climate may be more significant than previously represented in existing climate models.
Scientists discover remarkable sequestration and symbiosis in fig trees, pointing to fine-tuning while raising questions about long-age geological assumptions and climate projections.
Atmospheric scientists call for deeper analyses of climate complexities, as predictions fail, and warn of the potentially unforeseen consequences of geoengineering.