Evaluating the Characteristics of Trapped Lee Waves in a High-Resolution Forecast Model using Satellite Imagery Oral Presentation Orographic gravity waves, which are generated by the restoring force of gravity when stably stratified atmospheres flow over mountains, may exert frictional forces on the atmosphere and thus influence atmospheric circulation. While the effects of these waves may be large-scale, the mountains causing them are often of a smaller scale than can be resolved by most weather and climate models. Parametrisations are therefore necessary to approximate their effects on atmospheric circulation. Vertically propagating orographic gravity waves often are parametrised but trapped lee waves – their horizontally propagating counterparts, which occur at low levels and are of shorter wavelength – are often not. Before a parametrisation can be designed, however, a study of the conditions causing trapped lee waves must be conducted. Because measurements of trapped lee waves are scarce, the Met Office’s UK variable resolution model (UKV, 1.5 km grid spacing) could be used to investigate the atmospheric conditions associated with trapped lee waves. However, the use of this high-resolution model as a substitute for observations requires an evaluation of the model’s accuracy.To this end, the occurrence of trapped lee waves in the UKV is compared to their occurrence in geostationary satellite imagery during the year 2023. Continuous wavelet transforms are employed to compare the wavelength and orientation of the waves between both sources, showing that the UKV manages to accurately reproduce waves of wavelengths above 9 km (~6 times its grid spacing). There is very good agreement between the satellite imagery and the UKV on the orientation of the waves. In addition, their orientation is shown to be strongly correlated with wind direction. The application of linear gravity wave theory to UKV-derived vertical profiles identifies the model’s limited vertical resolution as a potential shortcoming in representing the relevant atmospheric conditions. Despite this, trapped lee waves are found to be generally well-reproduced in the UKV, which suggests a sufficiently accurate representation of the relevant atmospheric conditions in the model. It may therefore be considered a suitable substitute for observations in assessing the atmospheric conditions associated with trapped lee waves. Speaker/s Hette Houtman