April 2026 · Illustrative model · Mumbai

Why did Mumbai
get hot?

Move the sliders to see how each driver contributed — and what partial recovery looks like.

Satellite record

Greenness lost, heat gained

Monthly composites showing NDVI (vegetation) and LST (surface temperature) across five decades.

1973
2000
2024
2026 (Q1)
NDVI (greenness)

Pre-satellite

See IISc LULC
reconstruction below

1973 · pre-satellite

Apr 2000 · MODIS NDVI

Apr 2000 · MODIS NDVI

Apr 2024 · MODIS NDVI

Apr 2024 · MODIS NDVI

Mar 2026 · MODIS NDVI

Mar 2026 · MODIS NDVI

LST (land surface temp)

Pre-satellite

See IISc LULC
reconstruction below

1973 · pre-satellite

Apr 2000 · MODIS LST

Apr 2000 · MODIS LST

Apr 2024 · MODIS LST

Apr 2024 · MODIS LST

Mar 2026 · MODIS LST

Mar 2026 · MODIS LST

NASA EOSDIS GIBS · MODIS Terra monthly composites · 1 km native resolution

The data behind the heat

50 years of urban transformation

Mumbai, 1973 → 2026. Sources cited per card.

0%

Mangrove loss 1990–2001

Vijay et al., IJMS 2005

0 ha

Urban tree cover lost 2016–2021

MCAP 2022

0°C

Peak land surface temp rose 2003–2023

Balasundaram et al. 2025

0 mm/yr

Sea level rise rate — Apollo Bandar

NIO / PSMSL (113-yr record)

What if it played out differently?

Move the sliders to explore how much of Mumbai's temperature rise comes from tree loss, lake loss, built-up growth, and aerosols — and what a different path might have looked like.