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C. Pasquero

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Open access Aug 2026

Stratospheric influence on tropical cyclone evolution

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. · 0 citations
Open access Sep 2026

Impact of Upper‐Level Warming on Tropical Cyclone Intensity

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. · 0 citations
Open access Jul 2026

Scale dependence of the marine atmospheric boundary‐layer response to ocean surface‐temperature variability in the EUREC4A region

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. · 0 citations

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