| Summary: | 52 pages, figures, tables, appendix This work aims at creating a preliminary machine learning (ML) model for correcting the European Centre for Medium-Range Weather Forecasts (ECMWF) ERA5 reanalysis stress-equivalent local wind biases, based on atmospheric and oceanic parameters. Several errors in the ECMWF global output for near surface ocean winds have been reported when validated against scatterometer observations. An existing approach for correcting these biases (the so-called ERA* method) consists of scatterometer-based corrections accumulated over a certain time window at each grid point, which allows to reduce local persistent biases. This approach is sensitive to scatterometer sampling and, to collect a statistically significant number of samples, assumes that such biases are static. This is not the case for errors due to moist convection or the diurnal cycle. For operational purposes, the temporal window is lagged with respect to the reanalysis forecast time and the time difference betweeen scatterometer-based correction (SC) and sample data collections can be ten days. We propose a preliminary ML setup that looks for the functional relationship between several oceanic and atmospheric variables that describe the persistent NWP errors as observed in the NWP-scatterometer differences. This would allow to predict the biases of the stressequivalent wind forecasts and using the bias corrections in coupled weather or seasonal forecasts, or to account for these in climate runs. Such variables are first identified as ECMWF model parameters, such as stress-equivalent winds, their derivatives (curl and divergence), atmospheric stability related parameters, i.e., sea-surface temperature (SST), air temperature (Ta), relative humidity (rh), surface pressure (sp), as well as SST gradients and ocean currents. This work evaluates the feasibility of such approach and provides an overview of possible implementations of this regression Peer reviewed
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