With a long and complex deformational history since the initiation of the collision between India and Eurasia in the early Cenozoic, the Himalaya has undergone multiple deformat
Speaker: Dr Adele Morrison (RSES)
Global deep waters (below 2000 m) upwell back to the sea surface overwhelmingly in the Southern Ocean.
Speaker: Alice Barthel (RSES/UNSW)
In the Southern Ocean surrounding Antarctica, strong ocean currents interact with underwater topographic features.
Speaker: Dr James Munroe (Memorial University of Newfoundland)
Pangeo Data, a community effort for big data geoscience, identified several building crises facing the Atmosphere / Ocean / Land / Climate (AOC) science community:
Speaker: Prof Thorsten Becker (University of Texas, Austin)
Plate tectonics can be understood from the dynamics of the cold, top thermal boundary layer of Earth's mantle which is convecting over timescales of millions of years.