April 12th, 2022
Key Findings
- Climate simulations from multiple models in this study show that future changes in the patterns and frequency of tropical cyclone genesis are largely governed by dynamic effects, i.e., human-induced changes in the atmospheric circulation.
- These large-scale circulation changes include decreases in the mid-level upward motion and lower-to-mid level cyclonic vorticity, and increases in vertical wind shear.
- Conversely, the thermodynamic effect would yield tropical cyclone genesis patterns that are opposite to the model projections.
- Dynamic changes in response to anthropogenic greenhouse gas emissions are an important factor in determining the response of tropical cyclones to global warming.
Hiroyuki Murakami and Bin Wang. Nature Communications Earth and Environment. DOI: 10.1038/s43247-022-00410-z
Potential future changes in the genesis frequency and distribution of tropical cyclones are important for society, yet uncertain. Confidence in model projections largely relies on whether we can physically explain why the models projected such changes. After analyzing climate simulations from multiple models, the authors find that future changes in the patterns and frequency of tropical cyclone genesis are largely governed by dynamic effects—that is, by human-induced changes in the atmospheric circulation.
These large-scale circulation changes include decreases in the mid-level upward motion and lower-to-mid level cyclonic vorticity, and increases in vertical wind shear. Conversely, the thermodynamic effect—a result of increased maximum potential intensity in a warmer climate—would yield tropical cyclone genesis patterns that are opposite to the model projections. These findings suggest that dynamic changes in response to anthropogenic greenhouse gas emissions are an important factor in determining the response of tropical cyclones to global warming.
Most previous studies project decreases in global tropical cyclone genesis frequency. Specifically, the projected decreases are more significant over the Southern Hemisphere, including the South Indian Ocean and South Pacific Ocean, than the Northern Hemisphere. However, recent studies project future increases in the total global tropical cyclone frequency. It is, therefore, critical to try to understand the physical reasons behind the projected changes. Although consensus has not been reached regarding the theory determining global tropical cyclone frequency and the projected future changes, it has been widely accepted that changes in tropical cyclone genesis depends on the changes in the large-scale environmental conditions of the atmosphere and ocean.
The authors show that greenhouses gas radiative forcing–induced horizontally differential heating drives the circulation changes, shaping future changes in tropical cyclone genesis. The differential heating is associated with the robust “warmer Northern Hemisphere than Southern Hemisphere” and “warmer land than ocean” patterns, as well as the uncertain tropical SST patterns (e.g., El Niño-like warming).
