Abstract: The interaction between ocean surface waves and the overlying wind leads to a transfer of momentum across the air?sea interface. Atmospheric and oceanic models typically allow for momentum transfer to be directed only ...

Abstract: Generally, ocean waves are thought to act as a drag on the surface wind so that momentum is transferred downward, from the atmosphere into the waves. Recent observations have suggested that when long wavelength waves?which ...

Abstract: A new frontier in weather forecasting is emerging by operational forecast models now being run at convection-permitting resolutions at many national weather services. However, this is not a panacea; significant systematic ...

Abstract: set of high-resolution radar observations of convective storms has been collected to evaluate such storms in the Met Office Unified Model during the Dynamical and Microphysical Evolution of Convective Storms (DYMECS) ...