Lesson 6 of 6 • 91 upvotes • 9:18mins
The equatorial counter currents are driven by a distinct surface wind pattern in the tropics. Strong westward trade winds result in westward surface flow in most of the tropical Atlantic and Pacific Oceans. However, several hundred mi. (km.) north of the equator the winds are much weaker, in comparison. The stronger winds to the south pile up water where the winds are weak.
6 lessons • 51m
Overview of the course (in Hindi)
9:03mins
Part 1: Living roots and vegetation of India (in Hindi)
8:06mins
Part 2: Forests of India and Narmada (in Hindi)
7:18mins
Part 3:Planetary winds (in Hindi)
8:40mins
Part 4: Equatorial rain forest and tropical cyclone (in Hindi)
9:26mins
Part 5: Oceanic currents and IR (in Hindi)
9:18mins