4.6 Article

Application of the Pseudo-Global Warming Approach in a Kilometer-Resolution Climate Simulation of the Tropics

Journal

Publisher

AMER GEOPHYSICAL UNION
DOI: 10.1029/2022JD037958

Keywords

tropical clouds; Hadley cell; ITCZ; tropical low clouds; kilometer-resolution model; climate simulation

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Clouds over tropical oceans play a crucial role in the Earth's response to greenhouse gas concentrations, but modeling their behavior is challenging due to small-scale convective processes. In this study, a kilometer-resolution simulation (COSMO) is compared with global climate models (GCMs) to understand their response to global warming. The COSMO simulation shows a different behavior, with no double ITCZ bias, making it valuable for further research.
Clouds over tropical oceans are an important factor in the Earth's response to increased greenhouse gas concentrations, but their representation in climate models is challenging due to the small-scale nature of the involved convective processes. We perform two 4-year-long simulations at kilometer-resolution (3.3 km horizontal grid spacing) with the limited-area model COSMO over the tropical Atlantic on a 9,000 x 7,000 km(2) domain: A control simulation under current climate conditions driven by the ERA5 reanalysis, and a climate change scenario simulation using the Pseudo-Global Warming approach. We compare these results to the changes projected in the CMIP6 scenario ensemble. Validation shows a good representation of the annual cycle of albedo, in particular for trade-wind clouds, even compared to the ERA5 reanalysis. Also, the vertical structure and annual cycle of the intertropical convergence zone (ITCZ) is accurately simulated, and the simulation does not suffer from the double ITCZ problem commonly present in global climate models (GCMs). The response to global warming differs between the COSMO simulation and the analyzed GCMs. While both exhibit an overall weakening of the Hadley circulation, the narrowing of the ITCZ (known as the deep-tropics squeeze) is not so pronounced in the kilometer-resolution simulation, likely due to the absence of a double ITCZ bias. Also, there is a more pronounced intensification of the ITCZ at the equator in the kilometer-resolution COSMO simulation, and a stronger associated increase in the anvil cloud fraction.

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