Analysis of experimental results for slender delta wings reveals that
asymmetric liftoff of the leading-edge vortices on slender delta wings
does not start the wing rock, although it is responsible for the larg
e limit cycle amplitude observed in experiments. As a consequence, the
interaction of slender wing rock does not depend upon the interaction
between the two leading-edge vortices, but can be generated by one wi
ng half by itself, making slender wing rock more likely to occur on hi
gh agility aircraft than previously thought.