International Scholarly Research Notices / 2012 / Article / Fig 5

Research Article

Implementation and Validation of Dynamical Downscaling in a Microscale Simulation of a Lake Michigan Land Breeze

Figure 5

Simulation output from grid 5. The land breeze shows up very clearly in the surface zonal velocity field (a) and the return flow in the zonal velocity field at 570 m above lake level (b). The land breeze front and convective boundary layer is shown in the vertical velocity field at 75 m above lake level (c). The 113 m relative humidity field also shows very clearly the horizontal extent of the land breeze (d).

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