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<br />ET unless other monitored fields were within about a mile, then the neighboring fields <br />were served by one atmometer. <br /> <br />. <br /> <br />Crop cuttings were taken at multiple locations within most of the fields where in"igation <br />applications were being monitored. Soil water salinity was estimated at locations near <br />the cuttings using EM-38 surveys within these fields. The crop yield at each location was <br />divided by the maximum measured yield in the respective study regions for each <br />respective crop to estimate relative crop yield. The goal was to obtain data that would <br />allow us to develop relationships between soil salinity and crop yield. <br /> <br />A related effort that is not being conducted using CWCB funds is the development of the <br />use of remote sensing techniques to estimate crop ET. ET can be estimated using satellite <br />imagery by applying an energy balance approach. This approach uses the thermal <br />info1l11ation from the infrared band as well as the crop reflectance (NDVI). The Colorado <br />State University research group has developed and implemented a remote sensing <br />algorithm for estimating ET called RESET (Remote Sensing of ET) which takes into <br />account spatial and temporal variability using an energy balance approach. RESET can <br />estimate the actual crop ET at the time when the satellite image was taken. The goal of <br />this research is to estimate how much ET is reduced due to soil water salinity in the <br />Arkansas River Valley. This work is being partially supported by the United States <br />Bureau of Reclamation, the Colorado Agricultural Experiment Station, and the Colorado <br />Cooperative Extension. <br /> <br />H-I Model Review by Consultants <br /> <br />. <br /> <br />The objective of this project is to have changes to the H-I Model code and calibration <br />made by the State Engineer's Office reviewed by additional experts from Hydrosphere <br />Resource Consultants and Helton & Williamsen in order to have the revised model ready <br />for presentation to Special Master Arthur Littleworth and to have expert reports prepared <br />by the additional experts who will provide testimony to the Special Master. <br /> <br />Changes to the H-I Model to be used to quantify the depletions to usable Stateline flows <br />for the period 1997-2004 that are currently being reviewed by the Special Master were <br />completed in January, 2006. Following that completion, the H-I Model was recalibrated <br />by experts for both Colorado and Kansas. Hydrosphere Resource Consultants perfonned <br />all analysis comparing the calibration statistics produced for the Colorado calibration and <br />the Kansas calibration of the H-I Model. Both Hydrosphere Resource Consultants and _ <br />Helton & Williamsen assisted the State Engineer's Office in an evaluation of the H-I <br />Model code to determine the cause of differences between the model results produced by <br />the Colorado calibration and the Kansas calibration. Helton & Williamsen assisted the <br />State Engineer's Office in preparing the "Report to the Special Master Concerning <br />Oi fferences Between the Colorado and Kansas Calibrations of the Hydrologic <br />Institutional Model" which was submitted in June, 2006. <br /> <br />Ie <br />