Posted by Chris on Saturday, February 4, 2012 at 1:33am.
Use conservation of energy. At angle A (measured from vertical), the particles elevation has decreased by a (1 - cosA).
m g (1-cosA) = (1/2) m V^2
V = sqrt[2*(1-cosA)/g]
This assumes that the particle remains in contact with the hemisphere. At some point it may (or may not) be fast enough to leave the surface. That is a separate problem.
According to the analysis here, the particle does leave the sphere 1/3 of the way down:
http://www.feynmanlectures.info/solutions/particle_on_sphere_sol_1.pdf
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