Abstract

The problem of mixed convection over a semi-infinite vertical flat plate is studied by the method of series truncation for both cases when buoyancy adds and opposes the main flow. The present analysis is valid from leading edge to far downstream. The solutions show that the results are very accurate over an entire flow regime spanning from pure forced convection to moderately large free convection flows. In the buoyancy dominated limit the heat transfer is underestimated by 4 percent and skin friction is overestimated by 22 percent.

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