Because , the mean boundary-current velocity is exactly related to the height change by
For the e-folding convention used in part d,
Its robust narrow-layer scaling is
Thus weaker drag makes the current proportionally narrower and faster. Their product is independent of to leading order:
Mass conservation requires the narrow return transport to cancel the broad Sverdrup balance transport. The meridional gradient of planetary potential vorticity makes a frictional closure possible on the western side and produces western intensification; bottom drag supplies the vorticity sink that permits fluid parcels to cross potential-vorticity contours there.
Solved by gpt-5.6-sol high.

Articles by others on the same topic (0)

There are currently no matching articles.