How NDVI depends on LAI and vegetation cover ?

September 7, 2000

Kenlo Nishida (NTSG, School of Forestry, Univ. of Montana)


NDVI is one of the most famous spectral vegetation indices observable with satellite sensors such as NOAA/AVHRR, Landsat/TM, SPOT/HRV, JERS1/OPS, Terra/MODIS, and so on. In this simulation study, I tested the relationship between NDVI and canopy structure, say, LAI and vegetation cover.


For a rigorous study, three-dimensional canopy transfer model may be necessary especially for checking BRDF. However, in this study, I focused on heterogeneity of canopy which may be complicated for three dimensional modeling. Hence, I adopted a simple 1-dimensional radiative transfer model.

Suppose n layers of horizontal leaves on a soil. Another words, stack n leaves horizontally on a soil. If we denote the reflectance of this gcanopyh as Rn, we can easily get the following formula:

Where, rleaf and tleaf are reflectance and transmittance of each leaf, respectively. If the reflectance of earth surface beneath the canopy is given (and denoted as R0), Rn can be calculated with this equation.

Though some gclumping effecth is well known, I assumed spacially random distribution (Poisson Distribution) of leaves as a first approximation. It gives the following formula:

Where, Pm is the portion of canopy at which m layers of leaves are stacked on, and k is a coefficient which projects LAI perpendicularly onto the earth surface. It can be defined as:

where, L(theta) is the leaf angle distribution and theta is the angle between nadir and the normal vector of a leaf.

The reflectance of canopy can be expressed with the above equations as:

where, R is the canopy reflectance.

Parameter settings

I configured those parameters of leaf reflectance, leaf transmittance, earth reflectance, and k-parameter based on the observed data in TERC grassland in 1999. The spectral bands for red and near-infrared regions are taken on 580-680nm and 725-1073nm respectively. They mimic the NOAA/AVHRR CH1 and CH2.

Table 1 Parameters



Leaf reflectance



Leaf transmittance



Earth reflectance (Case 1)



Earth reflectance (Case 2)



Earth reflectance (Case 3)






Here, I tested 3 cases. The first case gives small reflectance of earth surface, second one is a middle reflectance, and the third one is high reflectance. The first 2 cases stand for actual observations of dead grass materials.


Fig. 1, 2, and 3 represents the results of simulation with case 1, 2, and 3. The most notable thing is that the relation between NDVI and vegetation cover changed greatly between the cases. Some studies assume that this relation can be represented with square function (i.e., vegetation cover is linearly related to the square of NDVI). However, this relation can be linear when the albedo of leaf and earth get close to each other.