Stochastic modeling of the time-advanced equations for climate dynamics

Long term, climatologically significant statistical properties of the atmospheric component of the climate system are examined in an effort to correctly and efficiently incorporate this component into larger models for climate that include oceanic and cryospheric influences and deal realistically with climate replication. The magnetic of the unpredictable (noise) component of long term atmospheric behavior is also studied in order to develop the potential for viable climatological forecasting

Stability of the compressible laminar boundary layer with an external pressure gradient

The small perturbation theory of the stability of the laminar boundary layer, as first considered in detail by Tollmien and Schlichting for incompressible flow and applied to compressible flow by Lees and Lin, is extended in this paper to include compressible flow with a pressure gradient in the main stream. Continues