The global rise of sea level has made developing predictions of coastal flooding risk on subseasonal timescales (2-6 weeks in advance) an emerging priority for the National Oceanic and Atmospheric Administration (NOAA). In this study, we assess the ability of two current operational forecast systems, the European Centre for Medium-Range Weather Forecasts Integrated Forecasting System (IFS) and the Centre National de Recherches Météorologiques climate model (CNRM), to make subseasonal ensemble predictions of the non-tidal residual component of coastal water levels at United States coastal gauge stations for the period 2000-2019. These models were chosen because they assimilate satellite altimetry at forecast initialization and attempt to predict the mean sea level, including a global mean component whose absence in other forecast systems complicates assessment of tide gauge reforecast skill. Both forecast systems have skill that exceeds damped persistence for forecast leads through 2-3 weeks, with IFS skill exceeding damped persistence for leads up to six weeks. Post-processing forecasts to include the inverse barometer effect, derived from mean sea level pressure forecasts, improves skill for relatively short forecast leads (1-3 weeks). Accounting for vertical land motion of each gauge primarily improves skill for longer leads (3-6 weeks), especially for the Alaskan and Gulf Coasts; sea-level trends contribute to reforecast skill for both model and persistence forecasts, primarily for the East and Gulf Coasts. Overall, we find that current forecast systems have sufficiently high levels of deterministic and probabilistic skill to be used in support of operational coastal flood guidance on subseasonal timescales.
