September 27th, 2018
Key Findings
- The 2017 Atlantic hurricane season, which was particularly active for major hurricanes, was predicted well in real-time seasonal predictions using a high-resolution global coupled model (HiFLOR) developed at GFDL.
- This prediction system tool was used to conduct additional simulations that pinpoint the unusual warmth in the tropical Atlantic, relative to the rest of the global ocean, as the main cause of the active season (rather than moderate La Niña conditions).
- Most climate projections show warming throughout this century in response to increasing greenhouse gases. If a hurricane season later this century is characterized by conditions similar to 2017, our results project a hurricane season even more severe. The unusual conditions as seen in 2017 would combine with an overall warmed climate to produce an even higher numbers of MHs.
Hiroyuki Murakami, Emma Levin, Thomas L. Delworth, Richard Gudgel, and Pang-Chi Hsu. Science. DOI: 10.1126/science.aat6711
The 2017 hurricane season in the North Atlantic Ocean was highly active, with six major hurricanes (MH). Three storms made landfall (Hurricanes Harvey, Irma, and Maria) – causing widespread damage over the Gulf Coast and the Caribbean.
A number of factors might be linked to this enhanced MH activity in 2017, including moderate La Niña conditions in the Pacific. Unusually warm sea surface conditions over the tropical Atlantic and off the coast of North America were also observed. GFDL’s global coupled model HiFLOR successfully predicted the very active MH season in real-time seasonal predictions. Results of additional experiments using HiFLOR determined that the unusual warmth in the tropical Atlantic was the main cause of the active season. The key factor controlling MH activity appears to be how much the tropical Atlantic warms relative to the rest of the global ocean, rather than absolute warming in the North Atlantic alone.
The authors also used these model experiments to determine possible future changes in MH activity given similar summer conditions, but with increased anthropogenic forcing. In the future, a similar pattern of the 2017 global surface temperature anomalies, superimposed upon long-term increasing sea surface temperatures from increases in greenhouse gas concentrations and decreases in aerosol loading, will likely lead to even higher numbers of MHs. Thus, continued anthropogenic forcing has the potential to further amplify the risk of MHs in the North Atlantic, with corresponding socio-economic implications.
Major hurricanes are one of the most damaging and deadly natural disasters, and are an energetic element of the climate system. Understanding the character and causes of variations and changes, including potential influences of anthropogenic climate changes, is central to NOAA’s mission and highly relevant to society.