(1 2004
DIS
. On
1der-
than
ence
the
land
y the
leto
jon of
over
ation
6 as
land
body,
rtion
1 the
ed to
s and
jatial
> Me
jah
nd
were
ed on
he
International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences, Vol XXXV, Part B-YF. Istanbul 2004
cloud covers, some pixels certainly has continuing cloud cover
during the eight days. Fortunately, such cloud cover
information is supplied with the MODIS LAI product. Figure 6
showed the cloud coverage at every pixel location and the LAI
estimation algorithm used. As seen in Figure 6, about 30%
pixels of the MODIS LAI image were affected by cloud cover.
The 5% pixels of this MODIS LAI image were produced by the
backup algorithm based on NDVI. In particular, most of the
pixels corresponding to the backup algorithm were forest.
Although the MODIS LAI product at this study area was
mainly estimated by main RT algorithm and not affected by
cloud, the effects of the backup algorithm and cloud should be
considered at the quality assessment of MODIS LAI over other
sites.
ey
=A,
oe
I =
Figure 6. MODIS LAI QA images of cloud effect (left: white-
cloud, black- no cloud) and estimation algorithm
(right: white- RT model, black-backup model).
As seen in Table 2 and Figure 7, the MODIS LAI values, which
were estimated by the backup algorithm and affected by cloud
cover, showed large difference as compared to the reference
LAI map. In these pixels, the MODIS LAI is lower than the
reference LAI value. Since the portion of area of the backup
algorithm and the cloud cover was relatively small, they might
have not affected the overall statistics of MODIS LAL
However, since the more than two third of the study area is
occupied by forest, the over-estimation of MODIS LAI in
forest shows great influence on the total image (Figure 7). In
grass and cropland, although they were small portion, the
MODIS LAI values were lower than the reference LAI value.
Under-estimatior II Over-estimation
E etf mm
Total image [-
RT model
Back-up model |
Cloud area 7
Nan-cloud area :
Forest
Crop&Grass a
0. 10. 20. 30 40.50 60. 70 80 - 90; 100
Coverage(%)
Figure 7. Estimation patterns of MODIS LAI for each schemes
(Under-estimation means MODIS LAI was lower than
reference LAI Over-estimation means MODIS LAI
was higher than reference LAI)
4. CONCLUSIONS
During the last decades, there was a great amount of time and
efforts to develop the global ecological variables by the earth
observing system (EOS) program. The MODIS global LAI
product is one of such variables that are now being provided.
To use such valuable information at regional and local scales, it
is crucial to validate the quality of the product. In this study, we
made a simple and direct comparison between the MODIS LAI
data and the reference LAI surface that was derived by an
empirical approach to relate the field-measured LAI to Landsat
ETM+ reflectance.
Although the validation can be further expanded into larger
areas, the preliminary results obtained from this study indicate
that the MODIS LAI product is different from the reference
data. At the temperate forest, the MODIS LAI estimates were
higher than the reference LAI values during the leaf-on season
of September. The discrepancy between the MODIS LAI and
the reference LAI may be caused by the uncertainties in the
input variables of MODIS LAI algorithm, effects of cloud at
each pixels, estimation algorithm, and land cover type. In
general, MODIS LAI values were higher than the reference
LAI in forest and they were lower than in grass and cropland.
Additionally, MODIS LAI data affected by backup algorithm
and cloud showed higher value as compared RT algorithm and
no-cloud condition.
The validations of MODIS LAI product are being carried out at
the several study sites throughout the world. Due to the km
spatial resolution of the data, the validation is often restricted
by the size of test area and the collection of accurate ground-
truth data. Temperate forest is even more complicated than any
other ecosystems, which include a variety of species and stand
structure. Further study is planned to assess the quality of the
. MODIS LAI estimate for local and regional applications.
5. REFERENCES
Bonan, G, 1993. Importance of leaf area index and forest type
when estimating photosynthesis in boreal forests. Remote
sensing of Environment, 43, pp.303-314.
Brown, L., J. M. Chen, S.G Leblanc, and J. Cihlar, 2000. A
Shortwave modification to the simple ratio for LAI
retrieval in boreal forest: An image and model analysis.
Remote sensing of Environment, 71, pp. 16-25.
Carlson, T.N. and D.A. Reley, 1997. On the relation between
NDVI, Fractional Vegetation Cover, and Leaf Area Index.
Remote Sensing of Environment, 62, pp. 241-252.
Chen, J.M. and J. Cihlar, 1996. Retrieving leaf area index of
Boreal conifer forests using Landsat TM images. Remote
Sensing of Environment, 55, pp. 153-162.
Chen, J. M., PM. Rich, S.T. Gower, J.M. Norman, and
S.Plummer, 1997. Leaf area index of boreal forests:
Theory, techniques, and measurements. Journal of
Geophysical Research, 102 (D24), pp.29429-29443.
Chen, J.M., G Palic, L. Brown, 2002. Derivation and validation
of Canada-wide coarse-resolution leaf area index maps
using high-resolution satellite imagery and ground
measurements. Remote Sensing of Environment, 80,
pp.165-184.
Cohen, W.B., T.K. Maierpserger, S.T. Gower, and D. P. Turner,
2003. An improved strategy for regression of biophysical
variables and Landsat ETM+ data. Remote Sensing of
Environment, 84, pp.561-571.