J6.5
Ensemble downscaling of seasonal forecasts
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Preliminary results show that dynamical downscaling can add regional detail to global seasonal predictions. An example is the strong El Niño event of winter 1982-83, in which the regional models produce heavy precipitation observed over California that was lacking in the CFS. This is attributed mainly to better resolution of terrain in the regional model, as the heavy precipitation is closely related to coastal topography. The fact that not all CFS ensemble members produced the heavy observed precipitation when downscaled by the regional model has two major implications. First, it emphasizes that the skill of this downscaling approach ultimately depends on the ability of the global model to represent large-scale winds and thermodynamics. Second, it shows that while there is potential skill in combining a coupled atmosphere-ocean global seasonal forecast model with nested regional climate models, an ensemble approach is essential to realizing the added value from such an approach.
