








• 
Define the
shelfbreak section along the 1000 m isobath in the



model. Include
acrossshelf sections at either end to close the box.



• 
At every point,
calculate the gradient of bathymetry. Get the



component of
vertically integrated flow in that direction.



• 
Calculate the
curvature, and the change of curvature, along the



shelfbreak
section.



• 
Calculate the
lagged correlation of onshelf transport and shelfbreak


curvature.

