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@@ -2,21 +2,21 @@
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<em>i.eb.eta</em> calculates the actual evapotranspiration (ETa ; mm/d) for
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diurnal period after [1], implemented in [3].
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-It takes input of Diurnal Net Radiation (see r.sun), evaporative fraction (see
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-r.eb.evapfr) and surface skin temperature.
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+It takes input of Diurnal Net Radiation (see <i>r.sun</i>), evaporative fraction (see
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+<i>i.eb.evapfr</i>) and surface skin temperature.
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<h2>NOTES</h2>
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Full ETa processing will need those:
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<ul>
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<li>i.vi, i.albedo, r.latlong, i.emissivity
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- <li>i.evapo.potrad
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+ <li>i.evapo.potrad (Addon)
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<li>i.eb.netrad, i.eb.soilheatflux, i.eb.h_sebal01
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<li>i.eb.evapfr, i.eb.eta
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</ul>
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(for time integration: i.evapo.time_integration)
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-<p>For more details on the algorithms see [1][2][3].
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+<p>For more details on the algorithms see [1][2][3][4].
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<h2>SEE ALSO</h2>
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@@ -42,6 +42,12 @@ Zalidis G.C. Integrated methodology for estimating water use in Mediterranean
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agricultural areas. Remote Sensing. 2009, 1, 445-465.
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(<a href="http://www.mdpi.com/2072-4292/1/3/445">PDF</a>)
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+<p>[4] Chemin, Y., 2012.
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+A Distributed Benchmarking Framework for Actual ET Models,
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+in: Irmak, A. (Ed.), Evapotranspiration - Remote Sensing and Modeling. InTech.
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+(<a href="http://www.intechopen.com/books/evapotranspiration-remote-sensing-and-modeling/a-distributed-benchmarking-framework-for-actual-et-models">PDF</a>)
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+
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+
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<h2>AUTHORS</h2>
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Yann Chemin, Asian Institute of Technology, Thailand
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