CHRISPROBA Workshop Noordwijk, Netherlands, April 34, 2003 PowerPoint PPT Presentation

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Title: CHRISPROBA Workshop Noordwijk, Netherlands, April 34, 2003


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CHRIS/PROBA Workshop Noordwijk, Netherlands,
April 3-4, 2003
  • Estimating land surface variables from CHRIS at
    Arizona, USA
  • Shunlin Liang, Ph.D
  • Department of Geography
  • University of Maryland at College Park, USA

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Funded Project
  • Establising a basis for carbon management policy
    at the sate level Carbon dynamics at site,
    landscape, and regional scales for arizona sate
    lands led by Prof. C. Hutchinson
  • Funded by NASA Carbon Cycle Program

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Objectives
  • assess carbon sequestration potential on state
    trust lands, as well as how that potential might
    vary under different management regimes, and
    during periodic climate variations
  • assess potential economic return to the state
    that might derive from a carbon sequestration
    program, and a comparison of those to current
    returns
  • assess potential monitoring systems that might be
    implemented by Arizona State Land Department
    (ASLD) for contract performance verification on
    any carbon sequestration project.

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Calibrated TOA radiance
Atmospheric correction

Surface spectral reflectance
Inversion algorithms
Broadband albedos
LAI
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Atmospheric correction
  • Liang S., H. Fallah-Adl, S. Kalluri, J. JaJa, Y.
    Kaufman, and J. Townshend, Development of an
    Operational Atmospheric Correction Algorithm for
    TM Imagery, Journal of Geophysical Research -
    Atmosphere, 10217173-17186, 1997.
  • Liang, S., H. Fang, M. Chen, Atmospheric
    correction of Landsat ETM imagery, I. Method,
    IEEE Trans. Geos. Remote Sens.,392940-2948, 2001
  • Liang, S., H. Fang, J. Morisette, M. Chen, C.
    Walthall, C. Daughtry, and C. Shuey, Atmospheric
    correction of Landsat ETM imagery, II.
    Validation and applications, IEEE Trans. Geos.
    Remote Sens., 402736-2746, 2002

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ETM atmospheric correction
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MODIS imagery of Chinese northeastern coast, May
7, 2000
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Broadband albedo estimation
Atmospheric correction
BRDF modeling
Raw data
Narrowband to broadband albedo conversion
Broadband albedos
Conventional
Alternative
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broadband albedo
  • Conventional Method
  • Liang, S., Narrowband to Broadband Conversions of
    Land Surface Albedo. I.Algorithms, Remote Sensing
    of Environment,76,218-238, 2001
  • Liang, S., C. Shuey, A. Russ, H. Fang, M. Chen,
    C. Walthall, C. Daughtry, and R. Hunt, Narrowband
    to broadband conversions of land surface albedo.
    II. Validation, Remote Sensing of Environment,
    84(1)25-41, 2003.
  • An alternative solution
  • Liang, S., A direct algorithm for estimating land
    surface broadband albedos from MODIS imagery,
    IEEE Trans. Geosci. Remote Sen., 41(1)136-145,
    2003.

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LAI Inversion algorithms
  • Liang, S., H. Fang, M. Kaul, T. Van Niel, T.
    McVicar, J. Pearlman, C. Walthall, C. Daughtry,
    F. Huemmerich, (2003), Estimation of land surface
    broadband albedos and leaf area index from EO-1
    ALI data and validation, EO-1 special issue of
    IEEE Transactions on Geoscience and Remote
    Sensing, in press.
  • Fang, H. and S. Liang, (2002), "Retrieve LAI from
    Landsat 7 ETM Data with a Neural Network Method
    Simulation and Validation Study," IEEE
    Transactions on Geoscience and Remote Sensing, in
    press.
  • Fang, H. and S. Liang, (2002), Retrieving Leaf
    Area Index (LAI) Using a Genetic Algorithm with a
    Canopy Radiative Transfer Model, Remote Sensing
    of Environment, in press.

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Hybrid inversion algorithm
Canopy radiative transfer simulations
Remote sensing data
Canopy soil parameters(e.g., LAI)
Canopy spectral reflectance
Atmospheric correction
Nonparametric regression
Surface reflectance
LAI products
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Two test sites
  • These two sites selected to document the impact
    of differing intensities of grazing and climate
    variability that can be linked to changes in
    carbon storage rates are in different rangeland
    settings (1) Sonoita plains grassland, and (2)
    Santa Rita semidesert grassland.
  • These two settings differ considerably and
    represent a range of conditions typical of lands
    managed by ASLD. Both have areas that have been
    protected for at least 25 years. At each
    location, we have established one site within a
    protected area, and another on an adjacent area
    that has been grazed.

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Santa Rita Semidesert Grassland Sonoita
Plains GrasslandSouthern Arizona
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Santa Rita Semidesert Grassland Sonoita
Plains GrasslandSouthern Arizona
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Santa Rita Semidesert Grassland Sonoita
Plains GrasslandSouthern Arizona
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Santa Rita Semidesert Grassland Sonoita
Plains GrasslandSouthern Arizona
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Thank you !
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