The Normalized Difference Moisture Index (NDMI) is a spectral index that uses
Near-Infrared (NIR) and Shortwave Infrared (SWIR) bands to highlight canopy and surface moisture.
It is widely used for soil moisture assessment, vegetation water stress and
drought monitoring.
1. Concept & Formula
NDMI exploits the different responses of NIR and SWIR reflectance to moisture content in vegetation
and soils. Moist targets tend to have higher NIR and lower SWIR
reflectance, while dry or stressed surfaces show the opposite behaviour.
Mathematical Definition
The standard NDMI formulation is:
NDMI = (NIR - SWIR) / (NIR + SWIR)
Typical range: -1 to +1
Higher values → higher moisture content
Lower values → dry or water-stressed conditions
Main Applications
Monitoring crop and canopy water status
Drought and vegetation stress mapping
Supporting irrigation planning and scheduling
Complementing NDVI for better moisture interpretation
Moisture / Water StressVegetation HealthDrought Analysis
2. Data & Bands for NDMI
Common Sensors & Bands
Sentinel-2 (ESA) – 10–20 m
NIR: B8 (~842 nm)
SWIR1: B11 (~1610 nm)
Landsat 8/9 OLI – 30 m
NIR: B5
SWIR1: B6
Good Practice
Use surface reflectance products (atmospherically corrected).
Mask out clouds, cirrus and cloud shadows before computing NDMI.
Analyse NDMI alongside NDVI and land cover maps for better interpretation.
Interpretation Hints
High positive NDMI → healthy, moist vegetation or wet surfaces.