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The similarity method is presented for the determination of the velocity and the temperature distribution in the boundary-layer next to a horizontal moving surface heated convectively from below. The basic partial differential equations are transformed to a system of ordinary differential equations subjected to boundary conditions.
PAPER REVISED: 2016-08-26
PAPER ACCEPTED: 2016-08-26
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THERMAL SCIENCE YEAR 2017, VOLUME 21, ISSUE Issue 6, PAGES [2795 - 2802]
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