A Distributed Benchmarking Framework for Actual ET Models

With the various types of actual ET models being developed in the last 20 years, it becomes necessary to inter-compare methods. Most of already published ETa models comparisons address few number of models, and small to medium areas (Chemin et al., 2010; Gao & Long, 2008; Garcia et al., 2007; Suleiman et al., 2008; Timmermans et al., 2007). With the large amount of remote sensing data covering the Earth, and the daily information available for the past ten years (i.e. Aqua/Terra-MODIS) for each pixel location, it becomes paramount to have a more complete comparison, in space and time. To address this new experimental requirement, a distributed computing framework was designed, and created. The design architecture was built from original satellite datasets to various levels of processing until reaching the requirement of various ETa models input dataset. Each input product is computed once and reused in all ETa models requiring such input. This permits standardization of inputs as much as possible to zero-in variations of models to the models internals/specificities.

[1]  George C. Zalidis,et al.  Integrated Methodology for Estimating Water Use in Mediterranean Agricultural Areas , 2009, Remote. Sens..

[2]  J. Norman,et al.  Remote sensing of surface energy fluxes at 101‐m pixel resolutions , 2003 .

[3]  Rp De Silva,et al.  A comparison of different models of estimating actual evapotranspiration from potential evapotranspiration in the dry zone of Sri Lanka , 1999 .

[4]  Wilfried Brutsaert,et al.  Aspects of bulk atmospheric boundary layer similarity under free‐convective conditions , 1999 .

[5]  Lalith Chandrapala,et al.  Satellite measurements supplemented with meteorological data to operationally estimate evaporation in Sri Lanka , 2003 .

[6]  A. Holtslag,et al.  A remote sensing surface energy balance algorithm for land (SEBAL)-1. Formulation , 1998 .

[7]  W. Brutsaert Evaporation into the atmosphere , 1982 .

[8]  A. Gieske Numerical modeling of heat and water vapor transport through the interfacial boundary layer into a turbulent atmosphere , 2007 .

[9]  W. Bastiaanssen Regionalization of surface flux densities and moisture indicators in composite terrain. A remote sensing approach under clear skies in Mediterranean climates. , 1995 .

[10]  Anthony Morse,et al.  Computing and Mapping of Evapotranspiration , 2005 .

[11]  Assefa M. Melesse,et al.  A Coupled Remote Sensing and Simplified Surface Energy Balance Approach to Estimate Actual Evapotranspiration from Irrigated Fields , 2007, Sensors (Basel, Switzerland).

[12]  Z. Su The Surface Energy Balance System (SEBS) for estimation of turbulent heat fluxes , 2002 .

[13]  Mark A. Friedl,et al.  Relationships among Remotely Sensed Data, Surface Energy Balance, and Area-Averaged Fluxes over Partially Vegetated Land Surfaces , 1996 .

[14]  Lalith Chandrapala,et al.  Evapotranspiration fluxes over mixed vegetation areas measured from large aperture scintillometer , 2003 .

[15]  J. C. Price,et al.  Land surface temperature measurements from the split window channels of the NOAA 7 Advanced Very High Resolution Radiometer , 1984 .

[16]  George H. Hargreaves,et al.  Reference Crop Evapotranspiration from Temperature , 1985 .

[17]  S. Idso,et al.  Analysis of an empirical model for soil heat flux under a growing wheat crop for estimating evaporation by an infrared-temperature based energy balance equation , 1987 .

[18]  Di Long,et al.  Intercomparison of remote sensing‐based models for estimation of evapotranspiration and accuracy assessment based on SWAT , 2008 .

[19]  Jawad T. Al-Bakri,et al.  Intercomparison of Evapotranspiration Estimates at the Different Ecological Zones in Jordan , 2008 .

[20]  L. S. Pereira,et al.  Crop evapotranspiration : guidelines for computing crop water requirements , 1998 .

[21]  Richard G. Allen,et al.  Satellite-Based Energy Balance for Mapping Evapotranspiration with Internalized Calibration (METRIC)—Model , 2007 .

[22]  J. Clevers,et al.  The robustness of canopy gap fraction estimates from red and near-infrared reflectances: A comparison of approaches , 1995 .

[23]  W. Bastiaanssen,et al.  A remote sensing surface energy balance algorithm for land (SEBAL). , 1998 .

[24]  Massimo Menenti,et al.  Estimation of sensible heat flux using the Surface Energy Balance System (SEBS) and ATSR measurements , 2003 .

[25]  Sergio Contreras,et al.  Comparison of Three Operative Models for Estimating the Surface Water Deficit using ASTER Reflective and Thermal Data , 2007, Sensors (Basel, Switzerland).

[26]  Albert A. M. Holtslag,et al.  Flux Parameterization over Land Surfaces for Atmospheric Models , 1991 .

[27]  Thomas Alexandridis,et al.  GRASS Image Processing Environment. Application to evapotranspiration Direct Readout , 2010 .

[28]  W. J. Massman,et al.  A model study of kBH−1 for vegetated surfaces using ‘localized near-field’ Lagrangian theory , 1999 .

[29]  Wilfried Brutsaert,et al.  Evaporation into the atmosphere : theory, history, and applications , 1982 .

[30]  C. Priestley,et al.  On the Assessment of Surface Heat Flux and Evaporation Using Large-Scale Parameters , 1972 .

[31]  George H. Hargreaves,et al.  Agricultural Benefits for Senegal River Basin , 1985 .

[32]  J. Norman,et al.  Source approach for estimating soil and vegetation energy fluxes in observations of directional radiometric surface temperature , 1995 .

[33]  William P. Kustas,et al.  An intercomparison of the Surface Energy Balance Algorithm for Land (SEBAL) and the Two-Source Energy Balance (TSEB) modeling schemes , 2007 .

[34]  Mark A. Friedl,et al.  Forward and inverse modeling of land surface energy balance using surface temperature measurements , 2002 .

[35]  Yann H. Chemin Remote Sensing Raster Programming , 2014 .

[36]  A. Monin,et al.  Basic laws of turbulent mixing in the surface layer of the atmosphere , 2009 .

[37]  Richard G. Allen,et al.  Estimating Reference Evapotranspiration Under Inaccurate Data Conditions , 2002 .

[38]  J. Norman,et al.  Evaluation of soil and vegetation heat flux predictions using a simple two-source model with radiometric temperatures for partial canopy cover , 1999 .

[39]  Li Jing,et al.  Estimation of daily evapotranspiration using a two‐layer remote sensing model , 2005 .

[40]  Peter A. Troch,et al.  Applications of quantitative remote sensing to hydrology , 2003 .