Abstract
The theory of anticyclonic vortical Rossby solitons has been discussed in Chap. 5. The solitonic concept of anticyclonic Rossby vortices has been used as a foundation for the theoretical solitonic models of the JGRS and similar long-lived vortices in the atmospheres of giant planets and in the oceans. The first consistent solitonic theory of the JGRS was proposed in 1976 (see below). In the light of these theoretical results, it appeared quite important to obtain a Rossby soliton in laboratory experiment. The present chapter describes how this problem was solved.
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