Bhutan packs extreme climatic variety into a small Himalayan kingdom—subtropical jungles to glacial peaks. Eight factors drive this diversity.
Elevation ranges **97 m (Drangme Chhu) to 7,570 m (Gangkhar Puensum)**. Temperature drops ~6.5°C per 1,000 m. Creates distinct belts: subtropical (<1,800 m), temperate (1,800–3,500 m), alpine (3,500–4,500 m), nival (>4,500 m).
Moisture from Bay of Bengal hits the southern slopes → **orographic rainfall**. Southern foothills: 2,500–5,000 mm/yr. Central valleys: 1,000–2,500 mm. Rain shadow in north: <500 mm.
Subtropical zone — strong seasonal sun-angle variation. Winter sun lower, cooler; summer high, intense. Modulates temperature baseline across elevations.
High peaks block cold, dry **Central Asian air masses** (Siberian High) in winter. Creates a "thermal shield" — Bhutan warmer than same-latitude Tibet/China. Also forces monsoon uplift → extreme rainfall on windward slopes.
North-south valleys (Punakha, Wangdue, Bumthang) funnel sun → **warmer, drier** than surrounding slopes. South-facing slopes: more sun, earlier crops. North-facing: cooler, moister, forest retention.
~400 km from Bay of Bengal. **Continental climate** signature: larger diurnal/annual temperature swings than coastal Bengal. Winter nights freezing in valleys; summer days hot.
| Zone | Elevation | Climate | Key Areas |
|---|---|---|---|
| Subtropical | <1,800 m | Hot, humid, heavy monsoon | Samdrup Jongkhar, Gelephu |
| Temperate | 1,800–3,500 m | Cool winters, warm summers, mod. rain | Thimphu, Paro, Punakha |
| Alpine | 3,500–4,500 m | Cold, short summer, snow | Laya, Lunana, high passes |
| Nival | >4,500 m | Perennial snow/ice | Gangkhar Puensum, glacial peaks |
Bhutan's climate is a vertical mosaic—written by altitude, etched by monsoon, guarded by the Himalaya.