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Results <br />As shown in Table 1, a good linear correlation was found between temperature stations, therefore <br />linear regression was used to fill missing temperature values in the temperature data set. A linear <br />relationship was not clear for precipitation and frost date data. Figures 1 and 2 show examples of <br />the poor precipitation relationships found between Alamosa and Del Norte climate stations and <br />between Center and Alamosa climate stations. Figures 3 through 6 show examples of the poor <br />spring and fall frost date relationships found between Alamosa and Del Norte climate stations <br />and between Center and Alamosa climate stations, therefore, tstool was used to fill missing <br />precipitation values with average monthly values for the period of record, and fill missing frost <br />date values with average frost date values for the period of record. <br />Figure 1 <br />Alamosa vs Del Norte Precipitation <br />1950-1997 April through October Data <br />A <br />0 <br />E 3 <br />A <br />a <br />y = 0.5323x + 0.217 <br />' RZ = 0.5083 <br />., .. <br />~.; :.. <br />.: _'. <br />.:, .., <br />0.5 1 1.5 2 2.5 3 3.5 4 4.5 <br />Del Norte <br />appendD_cropcu.doc D-4 of D-9 10/28/99 <br />