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Observing actual evapotranspiration within a hilly watershed: case study of the Kamech site, Cap Bon peninsula, Tunisia

Research datakeyboard_double_arrow_right Dataset 30 Jun 2017Publisher:Zenodo

Authors: Zitouna-Chebbi, Rim; Prévot, Laurent; Chakhar, Amal; Marniche-Ben Abdallah, Manel; Jacob, Frédéric;

doi: 10.5281/zenodo.821526 , 10.5281/zenodo.821527

Observing actual evapotranspiration within a hilly watershed: case study of the Kamech site, Cap Bon peninsula, Tunisia

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Abstract

Surface-atmosphere flux data acquired by the Kamech flux tower (Environmental Research Observatory OMERE) between March 2010 and August 2013 A single data file (csv format) containing : quality controlled surface-atmosphere fluxes (friction velocity, sensible heat flux, latent heat flux) meteorological data required to gap fill them with REddyProc (incoming solar radiation, air temperature, air humidity) wind direction (sectors NW or S) More details (names of the variables, units) are given in the readme.first.txt file

The author's express their thanks to : (1) the Environmental Research Observatory OMERE (http://www.obs-omere.org); (2) the MISTRALS/SICMED program; (3) French National Research Agency (ANR) TRANSMED program through the ALMIRA project (contract ANR-12-TMED-0003) for their financial support provided for this study.

Related Organizations

University of Carthage
Tunisia

Keywords

Tunisia, eddy covariance, actual evapotranspiration, ORE OMERE, gap filling, hilly watershed

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