Highly resolved modeling of extreme wind speed in North America and Europe

High wind speed ( U ) is one of the most dangerous natural hazards in North America and Europe. As a result, spatially explicit, statistical estimation of extreme U is of particular relevance for many sectors. However, the most common sources of wind speed data such as reanalysis data and in situ measurements are limited for this purpose due to their coarse spatial resolution and low representativeness. Thus, the main goal was to develop a high spatial resolution (250 m × 250 m) model (GloWiSMo‐X) for monthly mapping of the maximum hourly U for a 10‐year return period ( U 10yr ) in North America and Europe. The multistep development of GloWiSMo‐X is based on 2544 hourly U time series available from the integrated surface global hourly meteorological data set ( U NCEI ), U time series from ERA5 ( U ERA5 ), and mean wind speed from the Global Wind Speed Model ( U ¯ GloWiSMo ). Firstly, the block maxima method was applied to estimate monthly wind speed for a 10‐year return period for both U NCEI ( U 10yr,NCEI ) and U ERA5 ( U 10yr,ERA5 ). Secondly, the least squares boosting approach was used to predict the target variable U 10 yr , NCEIyielding the predictionsU ̂ 10 yr . The predictor variables U 10yr,ERA5 ,U ¯ GloWiSMo , continent, and month were used as input. It was found that the highest monthly continental means ofU ̂ 10 yr( U ¯ 10 yr ) in January are 16.4 m/s in North America and 16.3 m/s in Europe.U ¯ 10 yrdropped to 13.4 m/s and 12.5 m/s in August. The annual cycle ofU ¯ 10 yris more pronounced in Europe than in North America. The central parts of the USA and Western Europe were identified as intracontinental regions with the highestU ¯ 10 yr . GloWiSMo‐X proves to be very broadly applicable as it covers two different continents and all months. The model validation by the mean squared error (MSE) demonstrates its improved predictive power compared to ERA5.