Physical processes at play in the genesis and evolution of tropical cyclones are conducive to the formation of warm cores at their centres. When the warm anomaly is particularly large in the upper troposphere, it is referred to as a high‐level warm core. Previous works documented the generation of high‐level warm cor...
A. Davin, Giousef Alexandros Charinti, C. Muller et al.· Quarterly Journal of the Roy...· 0 citations
Deep convection from tropical cyclones (TCs) can reach the height of the tropopause and as such an interaction between the upper troposphere and lower stratosphere is likely to occur. Such interactions have been reported in both numerical and observational studies, mainly showing that subsidence from the stratosphere i...
Giousef Alexandros Charinti, A. Davin, Andrea Polesello et al.· Geophysical Research Letters· 0 citations
A large share of energy within the global oceans lies within the mesoscale range, (100 km), where very large dynamic and thermodynamic variability has been observed. We address how the marine atmospheric boundary layer (MABL) in a trade‐wind region adapts to fast and spatially varying sea‐surface temperature (SST) st...
Alessandro Storer, M. Borgnino, C. Pasquero et al.· Quarterly Journal of the Roy...· 0 citations
We use cookies to run the site and, with your consent, for analytics and to show ads.
See our Cookie Policy.