ESAEducationHomeWeather and ClimateGlobal ChangeNatural Disasters
   
Weather
Foehn windInteractive MeteosatMeteosat images
Climate
African climateEl NiƱoGulf StreamHimalayan climateExplore the world and its climate with JP ExplorerLake Chad
 
 
 
 
 
printer friendly page
Seasonal change of the NDVI
Seasonal change of the NDVI
Seasonal change of the NDVI
 
Click to see an animation of the seasonal change of the NDVI

The Normalized Difference Vegetation Index (NDVI) is used to show the amount of vegetation cover in remote sensing images. Vegetation gives a strong reflection in the 0.7 - 0.9 micrometre area (near infrared), whereas it gives a weak reflection in the 0.6 - 0.7 area (red) because of absorption by chlorophyll.

Because the spectral signature of vegetation is so characteristic, there are usually no problems in distinguishing between bare ground and green vegetation. As explained above, the difference between reflection in the visible and the near infrared ranges can be used to determine the extent of photosynthesis and plant growth. This can also be used to obtain information on the health status of the vegetation.

In the case of Landsat, channel4 is in the near infrared, and channel3 in the red spectral range, so the equation for the NDVI is:
(channel4 - channel3) / (channel4 + channel3)

In the animation, dark green indicates dense, healthy vegetation, whereas beige areas represent bare soil. Note the seasonal north-south movement of the vegetation belt. (Source of the animation: NASA/Goddard Space Flight Center Scientific Visualization Studio)  
 

 


African climate
IntroductionBackground
Exercises
IntroductionManual exercisesExercises using LEOWorks
Links
Meteosat imagesActual weather
animation using
Meteosat
Weather broadcast worldwideClimate system
Eduspace - Software
LEOWorks 3
Eduspace - Download
Africa - Meteosat visible channelAfrica - Meteosat thermal infrared channelAfrica - Meteosat water vapour channel
 
 
 
   Copyright 2000 - 2014 © European Space Agency. All rights reserved.