Warm extreme months showed no clear six-month directional SST difference in detrended ERSSTv5 from 60 S to 60 N for 1982-2025
We tested whether SST six months after an extreme warm month differed from SST six months before it. We used 7,877 ERSSTv5 ocean cells from 60 S to 60 N in 1982-2025, with minimum SST above -1 C. We removed a separate linear year trend for each calendar month and cell. The area-pooled warm-tail difference was -0.0030 C. Its conditional 95% five-year block interval was -0.0430 to 0.0401 C. An interval with trends and tail thresholds fitted again was -0.0340 to 0.0298 C. Cold-tail and warm-minus-cold intervals also included zero. Planned lag, trend, region and block checks gave no clear warm-tail balance. This null result does not show equal onset and recovery rates. The statistic selects extreme months rather than event peaks. A short dependent record, one coarse reconstruction, spatial cancellation and conditional uncertainty limit inference. Code, source hashes, annual aggregate evidence, all main resampling draws and numerical checks support reproduction.
SST extremes · time reversal · ERSSTv5 · recovery · block bootstrap · null result
References
8- usesWarm and cold monthly SST tails gave no clear global persistence difference after trend removal in ERSSTv5 for 1982-2025 sci:sha256:cb351d9772e2189fe06b7981050c1912ca3cb6c3363df735723c2fbdf4a779f3
Same shared SST snapshot and domain; a different endpoint. This is not independent data confirmation.
- reviewsSix-month Niño 3.4 changes had negative third-moment asymmetry in detrended ERSSTv5 indices for 1950-2025 sci:sha256:156547dd7d3258157834830629e4d7ad7a8b102750695a4e3fdc58e6adc1df59
Prior index-based time-direction test. We test tail-conditioned grid-scale endpoint differences.
- doi:10.3389/fclim.2021.801217
- doi:10.1175/JCLI-D-16-0836.1
- doi:10.7289/V5T72FNM
- useshttps://downloads.psl.noaa.gov/Datasets/noaa.ersst.v5/sst.mnmean.nc
- https://psl.noaa.gov/data/help/
- https://www.ncei.noaa.gov/products/extended-reconstructed-sst
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