Remote Sensing of Evapotranspiration The Surface Energy Balance Algorithm for Land (SEBAL)

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Remote Sensing of Evapotranspiration The Surface Energy Balance Algorithm for Land (SEBAL)

Transcript of Remote Sensing of Evapotranspiration The Surface Energy Balance Algorithm for Land (SEBAL)

Page 1: Remote Sensing of Evapotranspiration The Surface Energy Balance Algorithm for Land (SEBAL)

Remote Sensing of

Evapotranspiration

The Surface Energy Balance Algorithm for Land (SEBAL)

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What is MODIS?• Moderate-Resolution Imaging Spectroradiometer

• Launched in 1999 aboard the EOS AM (Terra); EOS PM (Aqua) followed in 2002

• Monitors 36 spectral bands between 0.4 m and 14.4 m

• Images entire Earth every 1-2 days at 1 km resolution

• X data products provided by NASA with full QA/QC

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Accessing MODIS Data• Level 1 and Atmosphere Archive and Distribution

System (LAADS)

• Warehouse Inventory Search Tool (WIST) submits orders via EOS ClearingHouse (ECHO)

• Direct access via FTP

• HDF files can be manipulated with C, Fortran, Perl, MATLAB, IDL, Mathmatica and now ArcGIS

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ET

Sensible Heat Flux

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Evapotranspirationand Land Use

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Validating the Method

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ET

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0 1 2 3 4 5 60

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Terra

Aqua

Actual ET (mm/day)

Esi

mate

d E

T

(mm

/day)

RMSE = 2.43 mm/dayBIAS = 2.27 mm/day

SEBAL vs Flux Tower Data

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Next Steps

• Develop principle for constraining maximum evapotranspiration

• Develop principle for estimating net radiation on cloudy days

Any Questions?