Rise of activity, i.e. inverse cascading, at the approach of an extreme event

Normalized counts of S(t)


l	Averages –

				S(t)/N(t)

l	Concentrations –

		( S(t)/N(t) ) / ( N(t) )^d/3

			where d is concentration dimension


		Sixth Workshop on Non-Linear
Dynamics and Earthquake Prediction
	The Abdus Salam ICTP, Miramare

16/10/2001