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Alamosa and other stations. The best filling basis was determined as reflected by the largest <br />goodness of fit parameter (r~ -correlation coefficient squared) and the completeness of data for <br />the 1950-1997 period. Regressions were made on all data values as one set rather than <br />performing separate regressions for each month. Table 1 shows the goodness of fit coefficients <br />(r~) as well as the independent station used for filling. <br />All temperature station regression command files where combined to create one TSTOOL <br />command file named rgtempfillallcom, shown in Exhibit A. <br />Table 1 <br />Temperature Station Filling Parameters <br /> <br />Station to be Filled Station used as Basis for <br />Filling <br />rZ- <br /> <br />Name NWS <br />No. <br />Name NWS <br />No. Goodness <br />of Fit tstool Command File <br />names <br />Alamosa WSO AP 130 Del Norte 2184 .9915 Alamosacom <br />Blanca 776 Alamosafill 130 .9954 Blancacom <br />Center 4 SSW 1458 Alamosafill 130 .9893 Centercom <br />Del Norte 2184 Alamosa 130 .9915 Delnortecom <br />Great Sand Dunes Nat 3541 Alamosafill 130 .9885 Sanddunescom <br />Hermit 7 ESE 3951 Alamosa 130 .9513 Hermitcom <br />Manassa 5322 Alamosafill 130 .9914 Manassacom <br />Monte Vista 2 W 5706 Alamosafill 130 .9889 Montevistacom <br />Sa uache 7337 Alamosafill 130 .9883 Sa uachecom <br />Summaries <br />Table 2 shows historic summary information for each weather station including the period of <br />record and number of missing temperature, precipitation, and frost date values for the period <br />1974 through 1996. Table 3 shows the regression equations used to fill temperature stations. <br />appendD_cropcu.doc D-2 of D-9 10/28/99 <br />