Evaluation of a simple approach for crop 1 evapotranspiration partitioning and 2 analysis of the water budget distribution for 3 several crop species

16 17 Climate variability and climate change induce important intra-and inter-annual variability of 18 precipitation that significantly alters the hydrologic cycle. The surface water budgets and the plant or 19 ecosystem water use efficiency (WUE) are in turn modified. Obtaining greater insight into how 20 climatic variability and agricultural practices affect water budgets and regarding their components in 21 croplands is, thus, important for adapting crop management and limiting water losses. Therefore, the 22 principal objectives of this study are: 23 1) to assess the contribution of different components to the agro-ecosystem water budget and 24 2) to evaluate how agricultural practices and climate modify the components of the surface 25 water budget. 26 To achieve these goals, we tested a new method for partitioning evapotranspiration (ETR), 27 measured by means of an eddy-covariance method, into soil evaporation (E) and plant transpiration 28 (TR) based on marginal distribution sampling (MDS). The partitioning method proposed requires 29 continuous flux recording and measurements of soil temperature and humidity close to the surface, 30 global radiation above the canopy and assessment of leaf area index dynamics. This method is well 31 suited for crops because it requires a dataset including long bare-soil periods alternating with 32 vegetated periods for accurate partitioning estimation. 33 We compared these estimations with calibrated simulations of the ICARE-SVAT double source 34 mechanistic model.The results showed good agreement between the two partitioning methods, 35 demonstrating that MDS is a convenient, simple and robust tool for estimating E with reasonable 36 associated uncertainties. During the growing season, the proportion of E in ETR was approximately 37 one-third and varied mainly with crop leaf area. When calculated on an annual time scale, the 38 proportion of E in ETR reached more than 50%, depending on the crop leaf area and on the duration 39 and distribution of bare soil within the year. 40