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Last modified
7/29/2009 10:11:20 AM
Creation date
10/9/2006 4:38:41 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8283.200
Description
Colorado River Basin-Colorado River Computer Models-Colorado River Decision Support System-Ray
State
CO
Water Division
5
Date
8/25/1995
Title
Consumptive Use Modeling-Task Memorandum-Phase III-Analysis of the Bear Report Blaney-Criddle Crop Coefficients
Water Supply Pro - Doc Type
Report/Study
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<br />1.11)"1;\58 <br /> <br />NW8 <br /> <br />TAll.E I <br />GROWING 8IA.ON 'Oil COLOllADO NWS <br /> <br />AVERAGE DATU AVERAGE DATU <br />'OR ITART or 'OR END or <br />GROWING SIA.ON GROWING 8EASON <br /> <br />Gunn180n <br />8toamboat Springe <br />Moybed <br />aolta <br /> <br />MoyS <br />April SO <br />Ap,1111 <br />April' <br /> <br />811/tlmbe' , I <br />O.t..... . <br />O.t..... 12 <br /> <br />Oot.be, II <br /> <br />LINGTH Of <br />GROWING SIASON <br /> <br />1S4 <br />lit <br />17. <br />201 <br /> <br />The growing 8eason at Steamboat Springs and Maybell are .Imirar to the Bear River sites. <br />Gunnison's growing season Is ahorter and Datta's growing season la much longer. <br /> <br />The possible utilization of the Hill SCS-BC coefflclent8 was also analyzed using estimated Et similar <br />to thl methodology used to derive the Bear River coefficients. 0811y m8xlmum and minimum <br />temperatures at Gunnison, Steamboat Springs, Maybell and Oehl for the years 1971 through <br />1986 were used In the analysis. The analysis of evapotranspiration waa as followS: <br /> <br />1 . Monthly vlluea of potential crop evapotrenlplr8tlon using scs-ac was calculated <br />using crop coefficients for pasture grass from TR-21. (ETP _SCSBCI <br /> <br />2. Monthly values of potential crop evepotransplratlon u8ing HlII'a Kcm coefficients <br />and Etr as cllculated using the Iqultlon Etr - . a TMIN + b 0 TMAX + c 0 ElEV <br />+ d, which is dascribed in REFERENCE EVAPOTRANSPIRATION MAPS FOR <br />COLORADO. The coefficients a, b, c, and d are listed in Table 3 of the report. <br />(ETP _ETRI <br /> <br />3. Average monthly ratios of ETP_SCSBC divided by ETP_ETR were calculated.' <br /> <br />4. <br /> <br />The monthly ratio I were IdJusted upward by 8% to account for the use of NWS <br />temperature clatalnstead of temperature from agricultural altes. <br /> <br />;;:> <br /> <br />5. A second adjustment of 7% waa made to account for the use of the Penman <br />Monteith Instead of the 1972 Kimberly Penmln. <br /> <br />8. Corrected monthly SCS-BC coefficients calculated by dividing TR-21 pasture grasa <br />coefflcienta by the monthly ratios found In step 5. <br /> <br />7. The corrected SCS-8C coefficient. were compared to HIII'8 SCS-8C coefflclent8. <br />....'i <br />Tha basis for ste~ls that the temperature8 at a NWS.re commonly 3 to !5 degrees higher <br />than temperatures In Irrigated fields. Temperaturea In agricultur81 areaa were used to determine <br />the relationship describe in step 2~ Analysla of the Steamboat data found th8t if the temperatures <br />are lower by 3 or 5 decrees, Etr Is reduced by 8 to 11 % respectively. The conservative value of <br />6% waa used in this analysts. '"\ "'- ~;;c> <br />Cl(\,\'-'\ <br /> <br />The basia for step 4 Is that ASCE PRACTICE MANUAL 70, EVAPOTRANSPlRA TION AND <br />IRRIGA TION WA TER REQUIREMENT, Tabla 7.13, shows that In arid region8, leasonal estimltea <br /> <br />1Ul1.II\MEMO _ . '.211.811 <br /> <br />4 <br /> <br />A . In WAL Till <br /> <br />50'd ~OO'ON 05:~1 <br /> <br />56 5~ 6nl;t <br /> <br />~08~-19L-~O~-1:l31 <br /> <br />Jossl;t ~ Jalaa4~ .~.~ <br />
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