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The article investigates the increase in rapid intensification (RI) of tropical cyclones, identifying a significant upward trend in intensification rates linked to anthropogenic forcing. Using high-resolution climate models and observational datasets, the study finds that the thermodynamic environments around tropical cyclones have become more favorable for intensification, suggesting that climate change contributes to these trends. The findings highlight the challenges in forecasting tropical cyclones due

Author

vinisha.ashokan

Language

EN