Stochastic transport in upper ocean dynamics (STUOD)
Producing a new systematic capability for dealing with the changing regimes of uncertainty in upper ocean fluid transport.
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Predicting the Oceans in a Warming World
Climate change is changing our oceans in ways that we are still working to understand. The sea absorbs vast amounts of heat and carbon, and even more so as the global temperature rises. But predicting how that energy moves through the ocean – and what it means for climate, sea level, marine life, and weather – remains a major scientific challenge.
Discover more from STUOD
Cycle
An example 1
Algae bloom
Example 4
Example 5
An example 2
Gulf Stream
Caption
Caption
Lofoten Vortex courtesy of https://ovl.oceandatalab.com/
“Relative vorticity over planetary vorticity” in the Gulf stream region. The picture is a close-up of a global simulation with the ocean general circulation model ICON-O of the Max-Planck Institute of Meteorology.