Laserfiche WebLink
<br />I <br />I <br />t <br />J <br />I <br />I <br />t <br />I <br />J <br />I <br />I) <br /> <br />t <br />I <br />I <br />t <br />a <br />I <br />I <br />I <br /> <br />SECTION III . DROUGHT IDENTIFICATION <br /> <br />3-01. Historical. <br /> <br />a. General. . For the purpose of this plan a drought is defined as a <br />climatically induced water shortage. It is generally of wide areal coverage and <br />its impacts are usually over a large spectrum of interests. The information <br />contained here relates specifically to naturally developed historical shortages. <br />The development of an isolated shortage at a specific location caused by the <br />overuse of the resource. while in a normal climatic pattern, . is considered a man- <br />made event. Such shortages are not considered in this document and are tr~ated <br />through routine water management procedures and coordination channels. <br /> <br />The Corps projects in the Basin were designed to provide a dependable <br />irrigation water supply based on the period of record available during design. <br />A more detailed discussion on design of the conservation storage is provided in <br />paragraph 4-02b and 4-02c for John Martin Reservoir and Trinidad Lake, <br />respectively. <br /> <br />b. Experienced Droughts. Although droughts are naturally occurring events <br />in the Arkansas River Basin, little is known about their occurrence prior to the <br />last decade of the 19th century. Climatic records kept prior to this period are <br />not sufficient to show the nature of the droughts. <br /> <br />Generally, these records are sporadic and few in number. The Palmer <br />Drought Severity Index (PDSI) has been calculated for each month from historical <br />records. This index is used by the National Weather Service (NWS) as an <br />indicator of the severi ty of a drought. A more detailed discuss ion of this <br />indicator is included in paragraph 3-02. Plate 3-1 shows the climatic divisions <br />for the PDSI in Colorado. By using this measure of severity, droughts can be <br />categorized as mild, moderate, severe or extreme. The droughts in these <br />categories and their duration in months, are shown in Table 3-1. The drought <br />periods shown on Table 3-1 are for the Arkansas River Drainage (NWS Climatic <br />Division # 1) in Colorado. <br /> <br />.' <br /> <br /> rablo 3-1 <br /> Arkansas River DratnRge <br /> Hlat~rlcal Drou&ht Periods <br />DROUGHT PERIOD NUKBER OF HONTHS TOTAL HONTHS <br />IIAIII 11m "1IUIl MODUATI W1RI EXTREME <br />Au! 1900 May 1903 10 14 8 2 34 <br />Ju1 1931 Rov 19 37 3 20 19 33 75 <br />Jun 1939 AUK 1940 2 7 6 15 <br />Rov 1949 Har 1957 10 9 37 31 87 <br />Mar 1962 Mar 1965 3 6 9 19 37 <br />Mar ,1966 Apr 1969 19 13 5 37 <br />Jun 1971 Apr 1972 10 1 4 15 <br />Har 1974 Oct 1978 19 22 9 50 <br />Apr 1980 Apr 1982 -1 -1 -11 -l -1l <br />Total 79 97 108 87 371 <br /> <br />*8.8 T.ble 3-3 for description. of .lld to extre.. drou&ht. <br />3-1 <br />