'Ne usa' presentation slideshows

Processes at the shelf edge.

Processes at the shelf edge. At the shelf edge: The current speed can vary with depth, but the direction of the current is always along the isobaths. This assumes a linear, steady, frictionless flow; i.e. a geostrophic flow cannot move across the shelf slope or shelf edge.

410 views • 16 slides

252 views • 10 slides

Local and Spatial Considerations

Local and Spatial Considerations. David Dodman , Elisabeth Hamin , Lorna Inniss , Tim Randhir , Ulric Trotz , Rae Zimmerman, and Arlen Marin. Preliminary aspects to consider.

175 views • 10 slides