Jessie Sagona SARP Presentation

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    Estimation ofEvapotranspiration with

    Jessie Sagona

    Student Airborne Research

    Program

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    Outline

    Introduction

    What is ET, why is it important?

    Method

    How can we estimate ET? Whatassumptions go into it?

    Results

    Conclusions

    Acknowledgements

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    How does METRIC calculate

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    Solar radiation

    Inputs:

    Day of year

    Time of day

    Latitude

    Elevation

    Transmissivity of atmosphere

    Albedo

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    Longwave radiation

    Inputs:

    Surface temperature (from Cassie andJames)

    Emissivity (both atmosphere and crop)

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    Sensible heat flux

    Difficult to measure directly

    In METRIC, calculated via iterationswith aerodynamic resistance.

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    Latent heat flux

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    Inputs to Code

    Once code was ready, usedtemperature and SAVI estimates asinputs, with other variables set the

    same for every pixel (i.e. latitude).

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    Two types of runs

    LAI from MASTER bandmath

    LAI from Emilys analysis

    Temperature always from MASTER data

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    ~3.3

    ~0.78

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    Almond irrigation

    Drip irrigation

    Fanjet irrigation

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    Almond ET using Emilys LAI

    For 2nd field: average LAI = 2.65

    For 3rd field: average LAI = 2.28

    Resulting ET values: Field 2: 1.064 mm/hr

    Field 3: 1.058 mm/hr

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    1.110 mm/hr

    1.074

    1.081

    1.053

    1.078

    1.064

    1.056

    ET using LAI from

    ET using LAI fromground

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    ET from CIMIS Penman-

    The Penman-Monteith equationcalculates ET based onmeteorological parameters.

    The CIMIS version has a slightlydifferent treatment of wind speedcompared to the classic version.

    For almond orchard at time of flight:

    ET = 1.38 mm hr

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    Cotton Fields

    ~2.56

    ~3.15

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    1.059

    0.929

    1.024

    1.027

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    Cotton ET using Emilys LAI

    Overall LAI for cotton was 1.49.

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    ET from CIMIS Penman-

    For cotton fields at time of flight:

    ET = 0.572 mm/hr

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    Conclusions - Almonds

    The fanjet irrigation is more effectivethan drip irrigation, leading to higherET. METRIC underestimates ET

    compared to the CIMIS PM equation.

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    Conclusions - Cotton

    METRIC strongly overestimates ETcompared to the CIMIS PM equation.

    However, ground LAI measurements

    and LAI from SAVI are very similar,resulting in similar ET values.

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    Acknowledgements

    Cassie, James, and Emily for directuse of data

    Shawn for guiding our project

    All of the SARP staff for this greatprogram!

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    Questions?