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Home›Geophysics›NDVI
Process / pipelineRemote sensing vegetation monitoring

NDVI

Normalized Difference Vegetation Index · Also known as: NDVI

The Normalized Difference Vegetation Index (NDVI) is a spectral index computed from satellite or aerial multispectral imagery that quantifies vegetation greenness and vigor. Introduced by Rouse and colleagues in 1973 using Landsat data, NDVI has become the most widely used remote sensing metric for vegetation monitoring, drought assessment, crop productivity forecasting, and land cover change detection.

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NDVI
General Circulation ModelStandardized Precipitati…Standardized Precipitati…Aerosol Optical DepthInSARUniversal Soil Loss Equa…

When to use it

Use NDVI to monitor vegetation health at regional to global scales, assess drought impacts, forecast crop yields, and detect land cover changes. NDVI works best for large-scale assessments (pixel resolution >10 m) and is less useful for local-scale management where field-level detail is needed. Combine NDVI with other indices (EVI, SAVI) for robustness and with precipitation/temperature data for interpreting drivers.

Strengths & limitations

Strengths
  • Simple and computationally fast, requiring only two satellite bands widely available across sensors and archives
  • Spatially continuous, enabling assessment across regions lacking field observations or ground infrastructure
  • Strong empirical relationship to leaf area index (LAI), photosynthesis rates, and biomass
  • Long temporal archive (Landsat since 1972, MODIS since 2000) enabling decadal trend analysis
Limitations
  • Saturates at high vegetation density; two dense forests with different structure appear similar in NDVI
  • Sensitive to atmospheric effects (aerosols, clouds) that introduce noise unless carefully corrected
  • Cannot distinguish vegetation type or quality; healthy weeds appear similar to healthy crops
  • Temporal resolution depends on cloud cover and satellite revisit frequency; gaps occur in cloudy regions

Frequently asked

Why use NDVI instead of just looking at red reflectance?

Red reflectance alone doesn't account for soil background. A dark soil and a sparse plant canopy both have low red reflectance. By normalizing the difference between NIR and red by their sum, NDVI isolates the vegetation signal from soil. The resulting index correlates strongly with leaf area, photosynthesis, and biomass.

What are typical NDVI values for different land covers?

Water and snow: < 0.1; bare soil: 0.1–0.2; grass and shrubland: 0.2–0.5; crops (depending on growth stage): 0.3–0.8; dense forest: 0.6–0.9. Values vary seasonally (low in winter, peak in mid-summer in temperate regions).

How does cloud cover affect NDVI monitoring?

Clouds block the satellite view entirely; cloudy pixels are masked and must be interpolated or skipped. In tropical regions with persistent cloud cover, useful NDVI data may be infrequent (< 50% of observations clear). Radar-based indices (not affected by clouds) like NDVI-derived backscatter provide alternatives in cloudy areas.

Can NDVI distinguish between crop types?

Not directly. NDVI reflects greenness, not crop identity. Wheat and barley have similar NDVI trajectories. However, phenological timing (peak NDVI date, growing season length) can differ among crops, enabling crop classification when combined with weather data or field observations.

Sources

  1. Rouse, J. W., Haas, R. H., Schell, J. A., & Deering, D. W. (1973). Monitoring vegetation systems in the Great Plains with ERTS. Third Earth Resources Technology Satellite Symposium Proceedings, 1, 309-317. link ↗
  2. Jackson, R. D. (1983). Spectral indices in n-space. Remote Sensing of Environment, 13(5), 409-421. DOI: 10.1016/0034-4257(83)90010-X ↗

How to cite this page

ScholarGate. (2026, June 3). Normalized Difference Vegetation Index. ScholarGate. https://scholargate.app/en/geophysics/ndvi

Related methods

General Circulation ModelStandardized Precipitation Evapotranspiration IndexStandardized Precipitation Index

Which method?

Set this method beside its closest kin and read them side by side — the library lays the books on the table; the choice is yours.

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Referenced by

Aerosol Optical DepthGeneral Circulation ModelInSARStandardized Precipitation Evapotranspiration IndexStandardized Precipitation IndexUniversal Soil Loss Equation

Similar methods

Precision Agriculture with NDVIUrban Green Space AnalysisLeaf Area IndexBurn Severity (dNBR)Crop Yield EstimationOcean Color Chlorophyll-aStandardized Precipitation IndexChange Detection

Related reference concepts

Drought and Water ScarcityEvaporation and EvapotranspirationSpecies Richness and Diversity IndicesIrrigation and DrainageThe Greenhouse Effect and Radiative ForcingPrecipitation

Spotted an issue on this page? Report or suggest a fix →

ScholarGate — NDVI (Normalized Difference Vegetation Index). Retrieved 2026-07-21 from https://scholargate.app/en/geophysics/ndvi · Dataset: https://doi.org/10.5281/zenodo.20539026
Quick facts
Originator
Rouse, Haas, Schell, and Deering
Subfamily
Remote sensing vegetation monitoring
Year
1973
Type
Spectral index for vegetation assessment
Related methods
General Circulation ModelStandardized Precipitation Evapotranspiration IndexStandardized Precipitation Index
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