Yale University
Center for Earth Observation
Classifying Vegetation in the Semi-Arid Near East Using Fourier
Series Techniques
Motivation
- Conventional clustering classification schemes (unsupervised classification) are often used to
group multitemporal satellite imagery into distinct vegetative classes with similar temporal
signatures. These techniques strive to minimize variability in each class by using euclidean
distance to measure the separation between pixels. This tends to put a heavy emphasis on the
annual mean while ignoring the sequential order of images (e.g. March follows February).
- Here we investigate a scheme that emphasizes the cyclic properties of a temporal vegetation
signature. The fourier coefficients for a given time series will retain information on the "shape"
of that series in a set of independent physically meaningful values.
- The central question of this work is does this fourier representation provide any advantages to
studying vegetation patterns?
Data and Methods
- Start with the NASA (GSFC) AVHRR Pathfinder data set.
- Normalized Difference Vegetation Index (NDVI) images
(NDVI ranges from -1 to +1 and has a positive correlation
with biomass)
- Maximum Value Composites (to reduce cloud cover)
- 8 kilometer spatial resolution
- One image per month from 1982 - 1993
- Average 1982 - 1993 to produce a 12 month "average year"
- Helps reduce noise and effects of interannual variability
- Compute the first six fourier coefficients for each pixel
- Threshold certain coefficients to classify the average year
- Compare this result with a traditional unsupervised classification, focusing on "double peaked"
(two vegetation maxima per year) classes
- Use Landsat TM imagery (30 meter spatial resolution) to relate the regional scale AVHRR
classification to local agricultural practices
Regional Scale Classification
- The classification based on thresholding fourier coefficients is presented in
figure 1. Compare
this with the result of the (k-means) unsupervised classification of the
averaged NDVI data in figure 2.
Take special note of the "double peaked" classes (highlighted
in purple and green).
- The annual NDVI cycles of pixels 3a,b,c,and d are plotted in
figure 3 to illustrate some
differences between the techniques. The fourier technique classifies pixels 3a and 3d in the
same double peak class (#3) while the unsupervised method places them in two different
classes (#10 and #15). This is a good example of the importance of the annual mean in the
unsupervised technique. Furthermore, the fourier scheme does not classify either pixel 3b or
3c as double peaked, while the unsupervised technique places 3b in same class as 3a (#15)
and 3c in the same class as 3d (#10).
High Resolution Analysis
- Identifying areas of double vegetation maxima on a regional scale has value for certain resource
calculations (water budget analysis etc..), but to understand the physical processes behind the
double crop signal we need to relate the coarse resolution NDVI signal to finer resolution
imagery.
- In figure 4
we "zoom in" to a small test site near Netanya, Israel using Landsat TM imagery
taken on four different dates to focus
on an area of approximately six of the coarser AVHRR pixels (outlined in white). For the four TM
scenes, we have computed the average NDVI within each of the six large AVHRR pixels. These
values are plotted as points in figure 5
(connected by dashed lines to make them easier to see)
along with the annual cycle for each of the AVHRR pixels. The offset in absolute value is due to
calibrations we have not performed, but notice the similarities in the trends for each AVHRR / TM
pair.
- In this case, as in many other areas in the region, the "double" cropping signal is not a result of
the same field producing two crops per year, but rather a system where half the fields produce
spring crops and the other half produce summer crops.
Conclusions
- The emphasis of shape over mean value allows the rules-based fourier series classification to
better identify areas with two crops per year. This seems to work well in this region in part
because the magnitude of NDVI signals for double peaked pixels varies widely across the
scene.
- Regional scale AVHRR imagery, which is composed of large heterogeneous pixels, can be
explained on a fine scale with high resolution images at lower temporal frequency. Perhaps this
will allow end member "unmixing" of these coarse pixels in the future.