Atlantic hurricane power in 2008-2025 was below a frozen 1946-2007 absolute-SST regression and near a relative-SST regression; neither had year-to-year skill (HURDAT2, ERSSTv5)
Vecchi, Swanson and Soden (2008) fitted annual Atlantic power dissipation index (PDI) on August-October main development region (MDR) sea surface temperature (SST) for 1946-2007. Absolute and relative SST (MDR minus 30S-30N mean) fitted equally well but gave very different futures. After 2007 the MDR warmed about twice as much as relative SST (+0.66 C against +0.31 C), so 2008-2025 is an out-of-sample test. We fitted both regressions on 1946-2007 with HURDAT2 and ERSSTv5, froze them, and predicted 18 seasons. The observed mean PDI was 3.05 x 10^11 m^3 s^-2. The absolute model predicted 4.15 (95% interval 3.12-5.19, p = 0.018) and was too high in 16 of 18 seasons. The relative model predicted 3.34 (2.67-4.07, p = 0.20). A predictor MDR minus k times tropical mean matched the observed mean at k = 1.11 (ERSSTv5) and 1.03 (HadISST); k below 0.85 (0.65) failed. In 32 variants (SST set, MDR box, PDI/ACE/log PDI, training from 1946 or 1970), the absolute model over-predicted by 18-33% and the relative model by 0.3-19%; with 1970 training the relative model also failed in 12 of 16. Year by year, neither model beat the 1946-2007 mean: the MSE difference had a 95% interval of -0.98 to 2.13. Limits: 18 seasons, one mean level, no pre-1970 intensity correction, possible observing changes and multidecadal variability. Code, annual aggregates, hashes and a retrieval script are included.
tropical cyclones · power dissipation index · relative SST · Atlantic hurricanes · out-of-sample test · HURDAT2 · ERSSTv5 · HadISST · main development region · forecast verification
References
10- uses, reviews, supportsdoi:10.1126/science.1164396
Source of the absolute and relative MDR SST regressions of Atlantic PDI and their fit period that we test out of sample.
- challengesdoi:10.1038/nature03906
Absolute MDR SST and PDI relation; our 2008-2025 test questions its use for extrapolation. MDR box used in a sensitivity variant.
- supportsdoi:10.1038/nature06423
Theory for control of potential intensity by relative SST.
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Relative SST as proxy for potential intensity under local forcing.
- usesdoi:10.1175/MWR-D-12-00254.1
HURDAT2 database format and uncertainty.
- useshttps://www.nhc.noaa.gov/data/hurdat/hurdat2-1851-2025-092326.txt
HURDAT2 Atlantic revision used; SHA-256 in files/provenance.json.
- usesdoi:10.1175/JCLI-D-16-0836.1
ERSSTv5, the primary SST data set.
- useshttps://downloads.psl.noaa.gov/Datasets/noaa.ersst.v5/sst.mnmean.nc
ERSSTv5 file used; SHA-256 in files/provenance.json.
- usesdoi:10.1029/2002JD002670
HadISST1, sensitivity SST data set (Open Government Licence v2).
- useshttps://www.metoffice.gov.uk/hadobs/hadisst/data/HadISST_sst.nc.gz
HadISST1 file used; SHA-256 in files/provenance.json.
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