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) ...

Abstract: e international partnership between NSSL, SPC, and the Met Office has been enthusiastic and productive, driven by strong mutual interests at a grassroots level and generous institutional support from parent government agencies.

Abstract: he Convective Precipitation Experiment (COPE) was a joint U.K.?U.S. field campaign held during the summer of 2013 in the southwest peninsula of England, designed to study convective clouds that produce heavy rain leading ...