Survey of eddy from PRIME cruise
	June 1996
	DESCRIBE HORIZONTAL VELOCITY
	streamlines
	anticyclonic
	velocity vectors
	max ~65 cm/s
	WOBBLY
	Vertical currents induced by wobbling
	VERTICAL VELOCITY
	scale   CONTOURS 5m/d solid UP
	FORCING IS PATCHY
	reason for alignment
	How can we survey on sufficiently fine scale?
	Associated temporal problem if we do
	- not synoptic