Abstract This study investigates the impacts of anthropogenic warming on the El Niño–Southern Oscillation (ENSO) modulation of tropical cyclones (TCs) in CMIP6 models using synthetic storms downscaled by the Columbia Hazard (CHAZ) model. The multimodel mean of CHAZ–CMIP6 simulations accurately captures the observed ENSO–TC relationship, defined as the differences between anomalous TC activity during El Niño and La Niña events. TC activity is represented by density maps of genesis, track, and accumulated cyclone energy. We found that anthropogenic warming indeed affects the historical ENSO–TC relationship. There is an overall reduction (increase) in TC activity during El Niño (La Niña) events in both the North Atlantic and eastern North Pacific, where the historical ENSO–TC relationships have opposite signs. A warming climate reduces this contrast between the two regions. Other ENSO–TC relationship changes include increased (reduced) TC activity in the South Pacific during El Niño (La Niña) events, which enhances the historically positive anomaly in tropical South Pacific TC activity but weakens the negative anomaly south of 15°S. There is also a westward shift of the positive anomaly of the southeast–northwest dipole pattern in the western North Pacific. These changes, however, are relatively small, and thus, the currently known ENSO–TC relationship persists as the climate warms. The analysis of individual CMIP6 models suggests that warming-induced changes in the ENSO–TC relationship vary by model and basin, with differences likely due to the changes in ENSO characteristics within the models.
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Near-term tropical cyclone risk and coupled Earth system model biases
Most current climate models predict that the equatorial Pacific will evolve under greenhouse gas–induced warming to a more El Niño-like state over the next several decades, with a reduced zonal sea surface temperature gradient and weakened atmospheric Walker circulation. Yet, observations over the last 50 y show the opposite trend, toward a more La Niña-like state. Recent research provides evidence that the discrepancy cannot be dismissed as due to internal variability but rather that the models are incorrectly simulating the equatorial Pacific response to greenhouse gas warming. This implies that projections of regional tropical cyclone activity may be incorrect as well, perhaps even in the direction of change, in ways that can be understood by analogy to historical El Niño and La Niña events: North Pacific tropical cyclone projections will be too active, North Atlantic ones not active enough, for example. Other perils, including severe convective storms and droughts, will also be projected erroneously. While it can be argued that these errors are transient, such that the models’ responses to greenhouse gases may be correct in equilibrium, the transient response is relevant for climate adaptation in the next several decades. Given the urgency of understanding regional patterns of climate risk in the near term, it would be desirable to develop projections that represent a broader range of possible future tropical Pacific warming scenarios—including some in which recent historical trends continue—even if such projections cannot currently be produced using existing coupled earth system models.
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- PAR ID:
- 10492536
- Publisher / Repository:
- National Academy of Sciences
- Date Published:
- Journal Name:
- Proceedings of the National Academy of Sciences
- Volume:
- 120
- Issue:
- 33
- ISSN:
- 0027-8424
- Page Range / eLocation ID:
- e2209631120
- Format(s):
- Medium: X
- Sponsoring Org:
- National Science Foundation
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