A multilayer snow scheme has recently been implemented in the configuration of the Met Office Unified Model that will be used for future climate and forecasting applications. The inclusion of this scheme has resulted in substantial improvements in the simulation of near-surface air temperature. Results from the general circulation model will be used to emphasize the importance of the thermal response of the snow pack in yielding good forecast performance for near-surface weather.
GABLS4 provides an excellent framework for testing interactions between the snow surface and the atmospheric boundary layer. Results from simulations for GABLS4 using this snow scheme will be presented and sensitivity studies suggesting areas for further improvements to the simulation of the boundary layer over snow will be discussed.