Laserfiche WebLink
<br />. <br /> <br />3. EvapOration rates for each month for . <br />all reservoirs <br />4. Maximum and minimum reservoir <br />CODSttaints <br />s. Maximum and mlnlmllm outlet <br />JintifMinDa <br /> <br />6.., IDitiaL reservoir content and saIiu.ity . <br /> <br />Demand Data <br /> <br />Var,iDg: IeveIs of basiIl cIcvelopmeat may be. . <br />st;nIlWl. by modifying, the ".....-d. data b8se.. <br />The d-d data base contains characteristics <br />of each d...."...d aJId allows for a breakdown CJf <br />a "_and into 10 ~ IISCrL SiJlce theIe may <br />beup to 10 lI_d~ per radr. it is possible.ta . <br />bave as IIIlIDY as 100 users per rcacl1. The de- <br />IIIIDd data base is not input to the model. di- <br />rectly but. is input to the- SMDID (SimuIar:ion <br />MocId ~"1DpUt Data) (ll'08r3m.. With the.. .. <br />, 1I__d data base as input. SMDID generates , <br />the II.....-d data for ~ SMDID not only <br />~. the d-cl data' but also produces. . <br />"'........ri~, of projectccl dep1edon. by water u* <br />(L~. iirigation.. M&I. power, etc.). State. and <br />basin. These ,,'......-;a prOvide a useful for- ' <br />mat: for ck-nnf!lt1:iJlg, the level of development <br />.mDdeJecJ by a panicuIar nUl of CRSM.... <br /> <br />Hydrology Data: <br /> <br />The hydrology data. inplit to CRSM is gener- <br />ated by rnnnillg the pl()l5Iam. MHYDRO with <br />the hydrology data base aJId control data as in- <br />put. The hydrology data base contains. c:aI.c:u- <br />Iated uatUral tIow and salt and uatUral, reach <br />gains and losses of flow and salt from 1906 to <br />1978;uatUral is defined for this purpose as <br />historical data adjusted for human develop- <br />ment. 'Ibis adjU"tl11eUt is made to estimate <br /> <br />. <br /> <br />, . <br /> <br />" <br /> <br />what the flows would be without present dcvel- <br />opmalt on the river; The data for this data <br />base were developed from historical stream- <br />~. records. "r;mMoio~ records. cropped <br />'1 a.......... cak:uIatcd evaporation from resez:- <br />voirs. and recorded diversions and return. <br />flows. The data base has been developed for <br />. ,thePerlods 19Q6.1978 and will be extended peri., <br />. odically. The: program,MHYDRO not only <br />geacrateS: the hydiology data for CRSM but <br />also may produc:c- tables.. correlations. plots. <br />and other reports at the option of the user; <br />MHYDRO also performs the updating of the <br />hydrology data base. <br /> <br />. <br />With most appiil:ations of the CRSS, it is Un- . <br />portaJit to evaluate the rcadion of the system to .', <br />hiP and low runoff periods coupled with dif- <br />. ferent periods of dcvelopmc:Dt.. 'Ibis evaluation. <br />is ~.....t1y performed. by .....Jrn,g several runs.. ' <br />With each nm. the bqinnillg year of the hydrol- <br />ogy is shifted aheid ''u'' years. For examp~ iC <br />the model nUlwcreto be from 1981 to 2030 and <br />''u'' was set equal to S. the first nUl would begin <br />with 1981 using the 1906 hydrology, 1982 using <br />the 1901 hydrology, etc. The second nUl would <br />begin with 1981 using the 1911 hydrology and so ' <br />OIL !lhifing the bcginnll1g year by ''u''. years <br />each nUl and placing the earlier years to the tail <br />eDCl of the hydrology allows for 73 divided by It <br />model l1lDS to be evaluated. <br /> <br />-. <br /> <br />.' <br /> <br />Tapedit (OUtput Snmmary <br />Program) . <br /> <br />The- TAPEDIT program was developed to save <br />both manpower and computer resources. With <br />TAPEDIT, the user may select certain param- <br />eters to be summarized in either tabular or <br /> <br />10 <br />