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Title: MODIS LAI and FPAR: Project Status and Validation


1
MODIS LAI and FPAR Project Status and Validation
N. Shabanov, W. Yang, B. Tan, H. Dong, R.B.
Myneni, Y. Knyazikhin /Boston University P.
Votava, R. Nemani /NASA Ames Research Center S.W.
Running /University of Montana
LAI Intercomparison Group Meeting, Missoula, MT,
August 16, 2004
2
Contents
  • MODIS LAI and FPAR Project Highlights
  • Validation Sampling Scheme
  • Validation Summary of Results

3
Contents
  • MODIS LAI and FPAR Project Highlights
  • Validation Sampling Scheme
  • Validation Summary of Results

4
Status of MODIS LAI and FPAR Products
5
MOD15_BU LAI and FPAR 1- and 4-km, monthly
6
Prototype of Collection 5 MODIS TERRA, AQUA and
Combined LAI products for North America for July
20-27, 2003
7
Visualization of MODIS LAI and FPAR data over
FLUXNET sites
  • Convenient web-based tool developed by ORNL DAAC
    for visualization of ASCII subset of MODIS land
    data over about 300 FLUXNET sites.
  • Allows 2 types of data visualization (a) at 7x7
    pixels grid for particular date (b) as a time
    series
  • Tool emphasize Quality Control grid tool allows
    selection of data at particular QC range, while
    time series tool separates best quality and all
    the available data
  • Available from ORNL DAAC, http//daac.ornl.gov/SMM
    /modis_gr.html

Grids of FPAR at 7x7 km
Grids of LAI at 7x7 km
Time series of LAI for 7x7 km Grid
Time series of FPAR for 7x7 km Grid
8
Contents
  • MODIS LAI and FPAR Project Highlights
  • Validation Sampling Scheme
  • Validation Summary of Results

9
Scaling Procedure
Field Measurements
Fine Resolution Satellite Image
Generate Fine Resolution LAI Map
Aggregate to Coarse Resolution
Compare with MODIS LAI product
10
Data Sampling Scheme Objectives
1000m
  • Example field campaign in needle leaf forests,
    Ruokolahti site, Finland. This site is very
    heterogeneous mosaic dense, sparse and
    intermediate needle leaf forests
  • The objective of the optimal data sampling scheme
    is to sample dynamic range of natural variability
    in LAI for main vegetation species over the area
    where validation of satellite product will be
    performed (5x5 to 10x10 km)
  • Prior to field campaign we analyze fine
    resolution satellite images ETM, IKONOS), aerial
    photo (as in Ruokolahti) and forest surveys,
    available locally to identify areas which will
    serve to represent range of variability in LAI at
    the validation area

1000m
Intermediate Forests
Dense Forests
11
Data Sampling Scheme Patches
ETM Surface Reflectances, 1x1km
Corresponding Patches, 1x1km
  • To establish reliable relationship between field
    measured LAI and fine resolution surface
    reflectances, errors of measurements should be
    considered field and satellite data geolocation
    errors, errors of atmospheric correction of
    satellite data, high heterogeneity of forest
    stands at the scale of few meters (mixture of
    dense vegetation elements and gaps).
  • To minimize the impact of the above errors,
    Boston University team proposed to split site
    into set of relatively homogeneous patches and
    sample LAI within each patch. Average LAI over
    the patch can be used for correlation with
    surface reflectances.

12
Data Sampling Scheme Patch Surface Reflectance
  • The coefficient of variation does not exceed
    10-2 indicating that the segments can be trated
    as homogeneous areas with respect to their RED
    and NIR reflectances.

13
Data Sampling Scheme Patch LAI
  • However, the LAI values exhibit higher variation
    within patches. Most of the patches can be
    represented by mean LAI within uncertainty of
    20. However, in some segments (1, 4, 8 and 9)
    the uncertainty can be high.

14
Generation of Fine Resolution LAI Map Correlate
Fine Resolution Surface Reflectances with Field
LAI
  • To generate fine resolution map we first
    establish correlation between fine resolution
    surface reflectances and field LAI
  • Correlation is established at the patch level
    (not pixel) to reduce errors.
  • Various approaches can be used, but empirical
    relationship between reduced simple ratio and LAI
    was found to be most accurate (highest R2)
  • RSR includes Shortwave Infrared (SWIR) band and
    can suppress background influence and the
    difference between land cover types.

15
Generation of Fine Resolution LAI Map
ETM LAI, 1x1 km
LAI
  • Using relationship Reduced Simple Ratio - LAI and
    fine resolution satellite data we can generate
    fine resolution LAI map at 1km, and then
    extrapolate this relationship at a larger area of
    10x10 km
  • 1x1 km area serve as a good representative of
    variability of LAI at 10x10 km area
  • 10x10 km fine resolution LAI map need to be
    degraded to MODIS resolution and can be directly
    compared top MODIS LAI product

16
Contents
  • MODIS LAI and FPAR Project Highlights
  • Validation Sampling Scheme
  • Validation Summary of Results

17
Summary of Publications on LAI and FPAR Validation
18
Example 1 Coniferous Forests
  • Site Ruokolahti, Finland
  • Measurements Dates June 14-21, 2000
  • Land Cover Type Coniferous forests
  • Results Comparison of the aggregated
    high-resolution LAI map and corresponding MODIS
    LAI retrievals suggests satisfactory behavior of
    the MODIS LAI algorithm although variation in
    MODIS LAI product is higher than expected.
  • Publication Wang et al. (2004). Evaluation of
    the MODIS LAI algorithm at a coniferous forest
    site in Finland. Remote Sensing of Environment,
    91, 114-127.

LAI
19
Example 2 Croplands
  • Site Alpilles, France
  • Measurements Dates February 26 March 15, 2001
  • Land Cover Type Croplands
  • Results Collection 4 MODIS LAI is accurate to
    within 0.3LAI precision is 20, uncertainty is
    25. Biome misidentification deteriorates the
    accuracy by factor of 2.
  • Publication Tan et al. (2004). Validation of
    MODIS LAI product in croplands of Alpilles,
    France. Journal of Geophysical Research, (
    Submitted).

Surf. Reflectances, 3x3 km
20
Example 3 Grass Savanna
  • Site Senegal, Western Sudano-Sahelian zone
  • Measurements Dates June-November in years 2001
    and 2002
  • Land Cover Type grass savanna
  • Results Seasonal dynamics of both in situ LAI
    and FPAR were captured well by MODIS LAI and
    FPAR. MODIS LAI is overestimated by approximately
    2-15 and the overall level of FPAR is
    overestimated by 8-20
  • Publication Fensholt, R., Sandlholt, I.,
    Rasmussen, M.S. (2004). Evaluation of MODIS LAI,
    fAPAR and the relation between fAPAR and NDVI in
    a semi-arid environment using in situ
    measurements. Remote Sens. Environ. vol. 91, pp.
    490-507

21
Data Sharing
  • Safari 2000 Botswana, Africa. Savanna, open
    shurbland and grassland. June 25-July 4, 2000.
    LAI, canopy transmittance, PAR
  • Ruokolahti 2000 Ruokolahti, Finland. Needleleaf
    forest. June 14-21, 2000. LAI, canopy
    transmittances and reflectances (helicopter data)
  • Harvard Forest 2000 and 2001 Harvard Forest,
    Massachusetts, USA. Broadleaf forest. July 21-25,
    2000 and August 7-9, 2001. LAI, canopy
    transmittances, PAR
  • Alpilles 2001 Alpilles, France. Croplands.
    February 26 March 15, 2001. LAI
  • Flakaliden 2002 Flakaliden, Sweeden. Needleleaf
    forest. June 25-July 4, 2002. LAI, canopy
    transmittance and reflectance (helicopter data)

Data are posted at MERCURY system
http//mercury.ornl.gov/ or can be downloaded
directly from Boston University FTP
ftp//crsa.bu.edu/pub/rmyneni/mynenimodisvalidatio
n/
22
MODIS LAI and FPAR Future Directions
  • Further improve consistency of simulated by
    LAI/FPAR algorithm surface reflectances with
    MODIS observations to enhance quality of product
    retrievals and agreement with field measurements.
    Substantial changes are expected especially for
    woody vegetation.
  • At least three versions of LAI and FPAR products
    will be generated TERRA, AQUA and Combined
    TERRA/AQUA.
  • Compile all available sources on field
    measurements of LAI and FPAR into one reference
    data base to use in validation of the LAI/FPAR
    algorithm. This data base will help to sample LAI
    and FPAR over a variety of geographical locations
    and climatic conditions. Possible source will
    include FLUXNET, Mercury system, LAI
    intercomparison project and other ongoing
    projects.
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