Final answer:
Western boundary currents are relatively shallow, broad, and slow. They transport enormous volumes of water from the polar regions towards the equator.
Step-by-step explanation:
Western boundary currents are relatively shallow, broad, and slow.
These currents transport enormous volumes of water from the polar regions towards the equator.
An example of a western boundary current is the Gulf Stream, which carries cool polar water from the Gulf of Mexico to Western Europe, providing it with a temperate climate.