WP10 - Performance, social and sustainability indicators

Presentations and Papers by P01-CSIC-Juan Miguel González-Aranda (WEBMASTER & Knowledge Manager) — last modified 2010-07-29 11:24

Folder for this Thematic Presentations

Working Documents by P01-CSIC-Juan Miguel González-Aranda (WEBMASTER & Knowledge Manager) — last modified 2010-07-29 11:24

Folder for "dynamic on-line draft" Working Documents to this Workgroup

Workgroup Documents Library by P01-CSIC-Juan Miguel González-Aranda (WEBMASTER & Knowledge Manager) — last modified 2010-07-29 11:24

Documents Library to this Workgroup

Rest of deliverables by P01-CSIC-Juan Miguel González-Aranda (WEBMASTER & Knowledge Manager) — last modified 2010-07-29 11:24

Free organisation of contents in this folder

WP10 Dialogue Board by P01-CSIC-Juan Miguel González-Aranda (WEBMASTER & Knowledge Manager) — last modified 2010-07-29 11:24

Work Package Fora, Chats, Conversations, ... and rest of Dialogue Instruments

Combining Satellite Remote Sensing Data with the FAO-56 Dual Approach for Water Use Mapping in Irrigated Wheat Fields of a Semi Arid Region by P41-CDRT-Prof. Ahmed Chehbouni — last modified 2010-11-03 18:08

The aim of this study was to combine the FAO-56 dual approach and remotely-sensed data for mapping water use (ETc) in irrigated wheat crops of a semi-arid region. The method is based on the relationships established between Normalized Difference Vegetation Index (NDVI) and crop biophysical variables such as basal crop coefficient, cover fraction and soil evaporation.

Evapotranspiration Partitioning from Sap Flow and Eddy Covariance Techniques for Olive Orchards in Semi-Arid Region by P41-CDRT-Prof. Ahmed Chehbouni — last modified 2010-11-03 18:08

La partition de l’évapotranspiration (ET) entre évaporation du sol et transpiration de la végétation (T) dans deux vergers de l’olivier irrigués différemment (goûte à goûte et gravitaire), a été faite en combinant les mesures de flux de la sève et de l’Eddy Covariance. La transpiration de l’écosystème a été dérivée à partir des mesures de flux de la sève en utilisant la surface occupée par l’arbre. Les résultats de mesure de flux de la sève ont montré que le flux de la sève : (1) diminue rapidement à travers la profondeur radiale du tronc; (2) est lié étroitement à l’évapotranspiration de référence (ET0).