The Indian Monsoon Climate:
India possesses a Tropical Monsoon type of climate characterized by a distinct seasonal reversal of wind directions and highly seasonal precipitation patterns.
Key Factors Determining India's Climate:
- The Himalayas (The Great Climatic Divide): (i) Act as a colossal meteorological barrier shielding northern India from the freezing, blizzard-like Arctic katabatic winds originating from Central Asia and Siberia; (ii) Force moisture-laden South-West monsoon winds to rise, precipitating heavy orographic rainfall across the Indo-Gangetic plains.
- Latitude & Tropic of Cancer: The southern half lies in the Tropical Zone (warm temperatures throughout the year); the northern half lies in the Sub-Tropical / Temperate Zone (large annual temperature ranges).
- Altitude: Places at higher elevations are significantly cooler (Normal Lapse Rate: temperature drops by $1^\circ\text{C}$ for every $166\text{ meters}$ of vertical ascent; e.g. Ooty on the equator is cool, while Agra and Darjeeling on the same latitude have starkly different temperatures).
- Distance from the Sea (Continentality): Coastal maritime locations (Mumbai, Chennai, Kolkata) experience equable (maritime) climates with small annual temperature ranges ($3^\circ - 5^\circ\text{C}$) due to moderating land and sea breezes. Continental interior locations (Delhi, Jaipur, Kanpur) experience extreme (continental) climates with scorching summers ($> 45^\circ\text{C}$) and freezing winter nights ($< 5^\circ\text{C}$).
- Relief & Orographic Barriers: The windward slopes of the Western Ghats receive $> 300\text{ cm}$ of rainfall, while the leeward Deccan plateau (Pune) receives $< 60\text{ cm}$ (rain-shadow zone). The Aravalli Range lies parallel to the Arabian Sea branch of the monsoon, failing to obstruct it, rendering Rajasthan a dry desert (Thar)!