Climate Engine documentation is moving to a new support site. Please visit ClimateEngine.org and click “Get Started” to access the latest documentation. This site will transition fully on May 1, so please update your bookmarks before then.

Normalized Difference Water Index (NDWI)

Example map of median Normalized Difference Water Index (NDWI) (NIR/SWIR) in the central Rocky Mountains region, USA during June 23-July 22, 2023

Description

The normalized difference water index can be utilized for evaluating vegetation liquid water contents or water-inundated areas (Gao, 1996). NDWI is useful for evaluating reflectance from vegetation canopies that have similar scattering properties, but slightly different liquid water absorption due to canopy water content. As a result, NDWI is sensitive to changes in the liquid water content of vegetation canopies and open water areas. The common range of NDWI for green vegetation is -0.1 to 0.4 with 0.4 indicating high vegetation water content. 

Climate Engine provides a couple different versions of NDWI, utilizing normalized differences of different bands, which can be more useful for different applications: 

  • NDWI (NIR/SWIR1) = (NIR-SWIR1)/(NIR+SWIR1)
  • NDWI (GREEN/NIR) = (GREEN-NIR)/(GREEN+NIR)
  • NDWI (GREEN/SWIR1) = (GREEN-SWIR1)/(GREEN+SWIR1)
  • NDWI (GREEN/SWIR2) = (GREEN-SWIR2)/(GREEN+SWIR2)
  • NDWI (SWIR1/GREEN) = (SWIR1-GREEN)/(SWIR1+GREEN)

where NIR = near infra-red band, GREEN = green band, SWIR1 = 1.55 - 1.75 micrometer band, SWIR2 =2.08 - 2.35 micrometer band. 

References

Gao, B.C., 1996, NDWI - A normalized difference water index for remote sensing of vegetation liquid water from space. Remote Sensing of Environment, 58, 257–266.

Still need help? Contact Us Contact Us