Preprints
https://doi.org/10.5194/egusphere-2026-2715
https://doi.org/10.5194/egusphere-2026-2715
27 May 2026
 | 27 May 2026
Status: this preprint is open for discussion and under review for Weather and Climate Dynamics (WCD).

Intermodel differences in seasonal and regional CMIP6 divergent atmospheric heat transport

Ruth Geen, Robert Fajber, Marysa Laguë, and Ishani Mistry

Abstract. The tropical rainband's location is closely tied to divergent atmospheric heat transport (AHT). Recent work decomposed annual and zonal-mean AHT into radiative fluxes, evaporative fluxes and sensible heat, finding that the latitudinal structure of divergent AHT strongly resembled that associated with the evaporative fluxes, and that imposed changes to evaporation in model simulations altered total divergent AHT.

Here, we generalise this decomposition to explore regional and seasonal intermodel differences in CMIP6 simulations. In historical climate, we find that the spatial structure of the total JJA and DJF AHT most resembles that linked to evaporative and radiative fluxes. Intermodel differences in divergent AHT predominantly relate to east-west rather than north-south rainband shifts. In future climate, in JJA most models show enhanced southward interhemispheric energy transport, while in DJF models instead undergo a zonal change towards more energy export from a warmer eastern Pacific.

We identify groups of models from different families that show similar decompositions of their total AHT response to climate change into the individual flux terms. This suggests that distinct storylines may exist through which warming affects the energy budget and associated tropical rainfall.

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Ruth Geen, Robert Fajber, Marysa Laguë, and Ishani Mistry

Status: open (until 08 Jul 2026)

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Ruth Geen, Robert Fajber, Marysa Laguë, and Ishani Mistry
Ruth Geen, Robert Fajber, Marysa Laguë, and Ishani Mistry
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Short summary
We explore spatial patterns of atmospheric heat transport (AHT) in state-of-the-art climate models, which are important for understanding tropical rainband shifts. We find that model AHT differences link to east-west rainband shifts. Future changes link to stronger southward AHT in Jun-Aug but stronger AHT from the eastern Pacific in Dec-Feb. We find groups of models that have similar energetic responses to climate change, suggesting distinct storylines by which warming affects tropical rain.
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