Tropical cyclones (TCs) significantly impact air-sea heat and gas fluxes, influencing the global climate system in essential ways. TCs extract heat from the ocean surface through strong winds and heavy rainfall. This process leads to mixing the upper ocean layers, bringing cooler water from below to the surface and resulting in a noticeable cooling effect, known as the cold wake of a TC. This cooling can affect local and regional sea surface temperatures (SSTs), influencing atmospheric circulation patterns and subsequent weather events. The intense mixing caused by TCs can enhance the exchange of gases between the ocean and the atmosphere. The turbulent conditions can increase the uptake of CO2 by the ocean, which has implications for the global carbon cycle. Enhanced CO2 fluxes can temporarily increase the ocean's capacity to sequester carbon, influencing atmospheric CO2 concentrations and, thus, the global carbon budget.
High-resolution models that can accurately simulate TCs and their interactions would improve the representation of these processes in climate models, leading to more accurate climate predictions and a better understanding of climate feedback. This provides a strong motivation to push for higher resolution in Earth system models, as the benefits extend to both global and regional scales, with significant implications for climate science, policy, and planning.