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We conclude that this “heat island” is a local phenomenon, occurring during the early springimage, and that our “hot” pixel of 302.7 K from a more typical part of the image is valid. Thisvalue for T hot is probably not a good value to apply for the southeast region. It would bebest to separate this region into a separate <strong>SEBAL</strong> application. In our application, we willinclude this region, but we will ignore the ET estimates for this region since it is outside ourarea of interest.After selecting a “hot” pixel, T hot should be recorded along with its coordinates.79
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