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@@ -8,13 +8,13 @@ pressure (ea[KPa]) and the (x,y) pairs for wet and dry pixels.
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Full process 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 (Addon)
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- <li>i.eb.netrad, i.eb.soilheatflux, i.eb.hsebal01
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- <li>i.eb.evapfr, i.eb.eta
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+ <li><em>i.vi</em>, <em>i.albedo</em>, <em>r.latlong</em>, <em>i.emissivity</em>
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+ <li><em>i.evapo.potrad</em> (GRASS Addon)
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+ <li><em>i.eb.netrad</em>, <em>i.eb.soilheatflux</em>, <em>i.eb.hsebal01</em>
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+ <li><em>i.eb.evapfr</em>, <em>i.eb.eta</em>
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</ul>
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-(for time integration: i.evapo.time_integration)
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+(for time integration: <em>i.evapo.time_integration</em>) <!-- TODO unknown module -->
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<p>
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<em>i.eb.hsebal01</em> performs the computation of <i>sensible heat flux</i>
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@@ -23,7 +23,7 @@ in this code in [3].
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<h2>NOTES</h2>
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<ul>
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-<li> z0m can be alculated by i.eb.z0m or i.eb.z0m0 (grass-addons).
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+<li> z0m can be alculated by <em>i.eb.z0m</em> or <em>i.eb.z0m0</em> (GRASS Addons).
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<li> ea can be calculated with standard meteorological data.<br>
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eoTmin=0.6108*EXP(17.27*Tmin/(Tmin+237.3))<br>
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eoTmax=0.6108*EXP(17.27*Tmax/(Tmax+237.3))<br>
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@@ -33,13 +33,13 @@ in this code in [3].
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<h2>SEE ALSO</h2>
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+
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<em>
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-<a href=i.eb.soilheatflux.html>i.eb.soilheatflux</a>,
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-<a href=i.eb.hsebal01.html>i.eb.hsebal01</a>,
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-<a href=i.eb.evapfr.html>i.eb.evapfr</a>
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+<a href="i.eb.soilheatflux.html">i.eb.soilheatflux</a>,
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+<a href="i.eb.hsebal01.html">i.eb.hsebal01</a>,
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+<a href="i.eb.evapfr.html">i.eb.evapfr</a>
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</em>
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-
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<h2>REFERENCES</h2>
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<p>[1] Bastiaanssen, W.G.M., 1995.
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@@ -48,7 +48,7 @@ conditions. PhD thesis, Wageningen University, Wageningen, The Netherlands.
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(<a href="http://edepot.wur.nl/206553">PDF</a>)
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<p>[2] Chemin Y., Alexandridis T.A., 2001. Improving spatial resolution of ET
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-seasonal for irrigated rice in Zhanghe, China}''. Asian Journal of
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+seasonal for irrigated rice in Zhanghe, China. Asian Journal of
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Geoinformatics. 5(1):3-11,2004.
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<p>[3] Alexandridis T.K., Cherif I., Chemin Y., Silleos N.G., Stavrinos E.,
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