Normalized Difference Vegetation Index (NDVI) quantifies vegetation by measuring the difference between near-infrared (which vegetation strongly reflects) and red light (which vegetation absorbs).
NDVI always ranges from -1 to +1. But there isn’t a distinct boundary for each type of land cover.
For example, when you have negative values, it’s highly likely that it’s water. On the other hand, if you have an NDVI value close to +1, there’s a high possibility that it’s dense green leaves.
But when NDVI is close to zero, there are likely no green leaves and it could even be an urbanized area.
NDVI is the most common index that analysts use in remote sensing.
As shown below, Normalized Difference Vegetation Index (NDVI) uses the NIR and red channels in its formula:
Healthy vegetation (chlorophyll) reflects more near-infrared (NIR) and green light compared to other wavelengths. But it absorbs more red and blue light.
This is why our eyes see vegetation as the color green. If you could see near-infrared, then it would be strong for vegetation too. Satellite sensors like Landsat and Sentinel-2 both have the necessary bands with NIR and red.
Reflectance percentage of different leaves (source: NASA)
The result of this formula generates a value between -1 and +1. If you have low reflectance (or low values) in the red channel and high reflectance in the NIR channel, this will yield a high NDVI value. And vice versa.
Overall, NDVI is a standardized way to measure healthy vegetation. When you have high NDVI values, you have healthier vegetation. When you have low NDVI, you have less or no vegetation. Generally, if you want to see vegetation change over time, then you will have to perform an atmospheric correction.
Example of NDVI calculation (source: NASA):
Here's how the red, green, and blue bands appear in true color. Since true color is what our eyes actually see, we use that term.
You can see how NDVI makes use of near-infrared (NIR) in the formula. Therefore, we get color infrared when we set the NIR band to display as red. Since near-infrared is in the red channel, we refer to it as color infrared. The pivot irrigation vegetation should already be screaming at you in bright red, as you can see below.
The formula results in a bright green color, which denotes a high NDVI. Red, however, has a low NDVI. As a result, it measures the difference between red light, which vegetation absorbs, and near-infrared light, which vegetation strongly reflects.
We observe NDVI in many different sectors. For instance, in agriculture, farmers use NDVI to measure biomass and practice precision farming. While in forestry, foresters use the NDVI to calculate the amount of forest and the leaf area index. Additionally, NASA claims that NDVI is a reliable drought indicator. When water restricts vegetation growth, the relative NDVI and vegetation density are lower. NDVI and other remote sensing applications are actually used in hundreds of different applications in the real world.