Climate Dynamics

Workshop on Atlantic Variability and Tropical Basin Interactions at Interannual to Multi-decadal Timescales: Mechanisms, Drivers and Impacts

Atlantic Variability and Tropical Basin Interactions at Interannual to Multi-decadal Timescales: Mechanisms, Drivers and Impacts

Draft Programme is available!

4th Summer School on Theory, Mechanisms and Hierarchical Modeling of Climate Dynamics: Atlantic Variability and Tropical Basin Interactions at Interannual to Multi-Decadal Time Scales

4th Summer School on Theory, Mechanisms and Hierarchical Modeling of Climate Dynamics: Atlantic Variability and Tropical Basin Interactions at Interannual to Multi-Decadal Time Scales
 

[Save your date] 4th Summer School on Theory, Mechanisms and Hierarchical Modeling of Climate Dynamics

The 4th Summer School on Theory, Mechanisms and Hierarchical Modeling of Climate Dynamics: Atlantic Variability and Tropical Basin Interactions at Interannual to Multi-Decadal Time Scales will be organized during 31 July - 11 August 2023 at ICTP, Trieste, Italy.

Robb Jnglin Wills leads the Climate Dynamics Group at ETH Zurich. He obtained his PhD in 2016 from the California Institute of Technology and had research appointments at ETH Zurich, University of Washington, and the National Center for Atmospheric Research before his appointment as assistant professor at ETH in 2023. Robb and his group use a combination of climate modeling, physics-based theoretical understanding, and data science methods to pursue research on a broad range of topics in climate science.

Matthew England is Scientia Professor of Ocean & Climate Dynamics at the University of New South Wales, Sydney, Australia, and the Deputy Director of the Australian Centre for Excellence in Antarctic Science.  England previously held appointments at CSIRO Australia, the CNRS in France, and a Fulbright Scholarship at Princeton University.  His research focuses on large-scale ocean circulation and the influence of the oceans on regional and global climate, from the tropics to the North Atlantic and Antarctica, spanning time-scales of seasons to millennia.

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