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Using the 13 m diameter LEGI-Coriolis rotating platform, the evolution processes of a generated anticyclonic eddy throughout its lifecycle are analyzed. Experimental results have shown that the eddy lasted for approximately 3 T  0 , where  T  0  is the rotating period of 90 s. After  T  = 0.3 T  0 , the eddy enters its mature phase, whereby following this event, eddy intensity slowly decreases from its maximum rotation speed. By  T  = 2.6 T  0 , the eddy enters a stage of rapid weakening. In its decay period, two underlying mechanisms for this decay have been identified as inertial instability and eddy–eddy interactions.

Strain Evolution and Instability of an Anticyclonic Eddy From a Laboratory Experiment