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<br />I <br />, <br /> <br />I <br />I <br />, <br />I <br />, <br />I <br />I <br />, <br />J <br />, <br />I <br />I <br />t <br />I <br />I <br />I <br />I <br /> <br />.' <br /> <br />drought by June 1934. This drought reached its greatest severity in March 1935 <br />with PDSI of -6.41. The severe to extreme drought extended from June 1934 <br />through 1937. Precipitation for the seven year period was approximately 87 <br />percent of normal. The annual river flow at the present John Martin Reservoir <br />site for the seven year period was approximately 38 percent of normal. The <br />annual river flow at the present Trinidad Lake site for the seven year period <br />was approximately 80 percent of normal. The 1934 Purgatoire River flow at the <br />Trinidad Lake site was 43 percent of normal and was the lowest for the seven year <br />period. Plate 3-2spows the PDSI for this period. <br /> <br />d. Drought of 1939-1940. This drought started off as a mild to moderate <br />drought and intensified to a severe drought. The severe drought extended from <br />October 1939 to December 1939 and leveled off to a mild to moderate drought <br />through March 1940. This drought reached its greatest severity in October 1939 <br />with a PDSI of -3.87. The annual rainfall for 1939 was approximately 69 percent <br />of normal. The annual river flow at the John Martin Reservoir site was five <br />percent of normal during the two year period. At the Trinidad Lake site, the <br />annual inflow for the two year period was 60 percent of normal. Plate 3-3 shows <br />the PDSI for this period. <br /> <br />e. Drought of 1950-1956. A moderate to extreme drought occurred during <br />this period. This drought reached its greatest severity in October 1956 with <br />a PDSI of -6.46. The lowest annual rainfall for this period of record was 1956 <br />with 10.88 inches. The precipitation for the seven year period was 85 percent <br />of normal. The annual inflow into John Martin Reservoir during this six year <br />period was approximately 50 percent of normal, except for 1955. The annual flow <br />at the Trinidad Lake site was approximately 56 percent of normal for the six year <br />period. Plate 3-4 shows the PDSI for this period. <br /> <br />f. Drought of 1963-1964. This drought intensified to an extreme drought <br />by May 1963 and extended through December 1963. This drought reached its <br />greatest severity in July 1963 with a PDSI of -6.51. Practically all of this <br />period was in the severe drought level, with precipitation at 81 percent of <br />normal. The annual inflow into John Martin Reservoir was 31 percent of normal <br />during this two year period. At the Trinidad Lake site the annual flow was 44 <br />percent of normal. Plate 3-5 shows the PDSI for this period. <br /> <br />g. Drought of 1974-1978. The annual inflow into John Martin Reservoir was <br />41 percent of normal during this period. At the Trinidad Lake site, the annual <br />inflow was 35 percent of normal. This drought started as mild to moderate and <br />intensified to a severe drought. This drought reached its greatest severity in <br />July 1976 with a PDSI of -3.70. The precipitation during the period was 87 <br />percent of normal. The low annual inflow was partially accounted for by below <br />average snowmelt runoff during the period. Plate 3-6 shows the PDSI for this <br />period. <br /> <br />h. Other Droughts. There were other droughts which have occurred in the <br />Basin, only the most severe were described above. The droughts, not described, <br />were generally moderate to mild and lasted only for a few months to a year at <br />a time. The PDSI for the period of record (1895 to 1987) is shown on Plate 3- <br />7. The observed annual inflow and outflow for John Martin Reservoir and Trinidad <br />Lake are shown on Plates 3-8 through 3-11. As seen on Plates 3-8 through 3-11, <br /> <br />3-3 <br />