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A monsoon is traditionally a seasonal reversing wind accompanied by corresponding changes in precipitation, but is now used to describe seasonal changes in atmospheric circulation and precipitation associated with the asymmetric heating of land and sea. The Himalayas is a mountain range in Asia separating the plains of the Indian subcontinent from the Tibetan Plateau. In this video, we will cover:
1. Monsoon
2. Advancing Monsoon
3. Retreating Monsoon
4. Factors Impacting Monsoon
5. Differential Heating & Cooling of land and Water
6. ITCZ (Doldrums)
7. ITCZ Vs. Equator
8. Shift of ITCZ
9. Intensely heated Tibetan Plateau.
10. Jet Streams
11. The Himalayas
12. Southern Oscillations
13. EL Nino
14. Normal (Non –El Nino) time
15. El-Nino time
16. La Nina

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