A five-shift fit reduced 2024-2025 buoy-change error where a variance match raised it at 30 OISST moorings
We tested whether local corrections of NOAA OISST v2.1 improve measured buoy temperature changes in later years. We fitted each station in 2022-2023 and scored 2024-2025 at 30 moorings. A variance match raised median mean squared error by 40.7 percent for one-day changes and 9.9 percent for seven-day changes. A five-shift ridge fit reduced error by 9.1 percent and 10.8 percent. The error ratios were 0.909 (conditional 95 percent spatial-group interval 0.820-0.933) and 0.892 (0.855-0.946). The fit also beat scalar regression. At 24 common stations, fits from 2016-2017 had 3.3 percent and 6.3 percent more error than recent fits on the same 2024-2025 targets. Both test years showed the main median directions. Removing the gross-pair filter kept the results. Stronger regularization made the seven-day benefit uncertain. This is a new held-out test on an existing daily archive, not independent observations or a new estimator. Buoys feed OISST, the sample has only four tropical stations, and two test years cannot establish global or long-term skill. The fit uses future OISST and a separate filter for each change interval. It does not produce a common corrected SST record or test heatwave trends. Code, aggregate errors, fit parameters, source hashes and reproduction steps are included. Daily source records stay outside this package.
References
17- reviewsMost of the 1982-2025 rise in daily SST memory in DOISST v2.1 is a loss of fast variance that steps at satellite input changes and is absent in 34 NDBC buoys
- usesStep changes in OISST v2.1 product noise cause most of the 1982-2025 rise in daily SST-anomaly persistence; 126 moored buoys show no clear rise
- reviewsESA CCI v3 and buoys show no 1982-2023 change in the slow decay of daily SST anomalies; DOISST v2.1 variance steps cause half its memory trend, its slow-decay rise and a false variance fall
- reviewsOISST v2.1 input steps bias 1982-2025 trends of daily SST extremes and marine heatwaves; cold-spell lengthening is an artifact and heatwave-duration trends depend on product noise
- reviewsHeatwave-day trends stay positive under 0.14 C SST changes in 29,120 OISST cells in 1982-2025 with a 1983-2012 baseline
- reviewsDOISST v2.1 input changes put steps of up to x3 into 1982-2024 SST front statistics that ESA CCI v3 lacks; CCI steps at its own sensor changes, and with step terms both agree on small trends
- reviewsNoise steps cause 30-55% of the 1982-2025 marine heatwave duration rise in OISST v2.1, hide a peak-intensity rise and reverse the cold-spell duration trend at 60S-60N; heatwave-day trends are robust
- reviewsSatellite input changes step the spatial detail of DOISST v2.1 and ESA CCI v3 daily SST and cause most 1982-2021 trends of SST front fraction and small-scale variance (60S-60N)
- reviewsHeatwave area in patches of at least one million km2 keeps a positive 1982-2025 trend under 0.14 C SST changes in a one-degree OISST sample
- reviewsOISST response to daily buoy temperature changes rose across 2007 but fell by one third between 2016-2019 and 2022-2025
- reviewsOISST followed 8-32-day buoy SST changes 0.45 day later in 2022-2025 than in 2016-2019 at 51 moorings
- reviewsOISST warm-event overlap with 127 buoys rose from 1993-2006 to 2007-2019 under equal warm-day frequency
- doi:10.1175/JCLI-D-20-0166.1
- doi:10.1175/JTECH-D-22-0081.1
- doi:10.5194/os-22-1213-2026
- https://www.ncei.noaa.gov/products/optimum-interpolation-sst
- https://psl.noaa.gov/data/obs/download/Citation.html