Extratropical transition of tropical cyclones in a multiresolution ensemble of atmosphere-only and fully coupled global climate models

• Published in: Journal of Climate
• Main Authors: Baker, Alexander J., Roberts, Malcolm J., Vidale, Pier Luigi, Hodges, Kevin I., Seddon, Jon, Vanniere, Benoit, Haarsma, Rein J., Schiemann, Reinhard, Kapetanakis, Dimitris, Tourigny, Etienne, Lohmann, Katja, Roberts, Christopher D., Terray, Laurent
• Format: Article in Journal/Newspaper
• Language: English
• Published: American Meteorological Society 2022
• Subjects: Pacific; North Atlantic
• Online Access: https://centaur.reading.ac.uk/105122/; https://centaur.reading.ac.uk/105122/8/CentAUR_version.pdf; https://centaur.reading.ac.uk/105122/1/CentAUR_version.pdf; https://journals.ametsoc.org/view/journals/clim/aop/JCLI-D-21-0801.1/JCLI-D-21-0801.1.xml

Tropical cyclones undergo extratropical transition (ET) in every ocean basin. Projected changes in ET frequency under climate change are uncertain and differ between basins, so multimodel studies are required to establish confidence. We used a feature-tracking algorithm to identify tropical cyclones and performed cyclone phase-space analysis to identify ET in an ensemble of atmosphere-only and fully coupled global model simulations, run at various resolutions under historical (1950–2014) and future (2015–2050) forcing. Historical simulations were evaluated against five reanalyses for 1979–2018. Considering ET globally, ensemble-mean biases in track and genesis densities are reduced in the North Atlantic and Western North Pacific when horizontal resolution is increased from ∼100 to ∼25km. At high resolution, multireanalysis-mean climatological ET frequencies across most ocean basins as well as basins’ seasonal cycles are reproduced better than in low-resolution models. Skill in simulating historical ET interannual variability in the North Atlantic and Western North Pacific is ∼0.3, which is lower than for all tropical cyclones. Models project an increase in ET frequency in the North Atlantic and a decrease in the Western North Pacific. We explain these opposing responses by secular change in ET seasonality and an increase in lower-tropospheric, pre-ET warm-core strength, both of which are largely unique to the North Atlantic. Multimodel consensus about climate-change responses is clearer for frequency metrics than for intensity metrics. These results help clarify the role of model resolution in simulating ET and help quantify uncertainty surrounding ET in a warming climate.