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Last modified
1/26/2010 2:55:42 PM
Creation date
10/12/2006 3:54:54 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8143.700
Description
John Martin Reservoir - Annual Operating Plans and Reports
State
CO
Basin
Arkansas
Water Division
2
Date
12/1/2003
Title
Annual Report of the Operations Secretary - Concerning the Operation of John Martin Reservoir - 2003
Water Supply Pro - Doc Type
Annual Report
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<br />I <br />'"I' <br />" <br /> <br />'.~;;~ <br />;::~1 <br /> <br />r} <br />;;,':;' <br />;~:':? <br /> <br />\>~ <br />.... "~' <br />..' <br />;....::$ <br /> <br />-:.:~:~~ <br />~'. ,.-, <br />{:.J <br /> <br />';".' <br /> <br />" <br /> <br />o <br />r-, <br />w <br />..... <br />....:J <br />-.J <br /> <br />Beginning on November 16, 2002 and pursuant to the provision of Section III (a.k.a. Article III) <br />of the 1980 Operating Plan, the storage of certain other inflow was also credited to the winter <br />water account. Storage into the winter water account continued to March 15, 2003, when the <br />distribution of 12,572 acre-feet occurred to the appropriate accounts pursuant to Section III D of <br />the Plan. This included a transfer of 23 76 a.f. of water into the transit loss account consisting of <br />676 a.f. to make up for deficits detemrined pursuant to Section II E (4) and 1700 a.f. to complete <br />the fill of the transit loss account. An explanation of this operation is documented in a letter to <br />the Assistant Operations Secretary, Mr. Mark Rude, dated March 19, 2003. <br /> <br />The division of inflow between conservation storage and the winter water accounts followed <br />established guidelines and resulted in an approximate overall 49 -to- 51 split (conservation to <br />winter water) [See Section 2 -Tables I and II]. The methodology for determining the <br />conservation storage to winter water ratio was consistent to the method utilized in prior years. <br />The base flow at the Arkansas River at Las Animas gage was detemrined during the period <br />November. 8th through November 14th with current meter measurements conducted by DWR on <br />November 12th and by USGS on November 14th. The base flow was detemrined to be 12.14 cfs. <br />During the period November 15th through November 18th computations were made to determine <br />the enhanced flow associated with arrival of winter water at the gage. Additional current meter <br />measurements were conducted on November 18th and November 20th by DWR and on November <br />22nd by the USGS. The enhanced flow during this initial transition period was determined to be <br />30 cfs and an initial ratio for winter water and conservation storage was set at 59.5% for winter <br />water (17.86/30) and 40.5% for conservation storage (12.14/30) for the flow through the <br />Arkansas River at Las Animas gage, <br /> <br />A significant operational change in the winter water program occurred November 17th when the <br />Fort Lyon Canal ceased diversions at the main canal headgate, resulting in an increased flow at <br />the Arkansas River at Las Animas gage two days later on November 19th. Therefore, a second <br />transition period was established over the period November 19th through November 21" and the <br />new enhanced flow was detemrined to be 59 cfs. This resulted in a winter water ratio of 79.4% <br />(46.86/59) and a conservation storage ratio of 20.6% (12.14/59). Since there were no further <br />operational changes that significantly affected the winter water ratio during the remainder of the <br />2002-2003 winter water program, these ratios were used until the end of the winter water storage <br />season on March 14, 2003, <br /> <br />For the period November 1, 2002 to April 1, 2003, conservation storage accumulated 11,867 <br />acre-feet. The winter water inflow accumulation to the conservation pool did depart from the <br />1950 to 1975 average historic winter storage amount of22,209 acre-feet. In the 2002 Operations <br />Secretary's Report documentation was provided as to the severity of the drought effects on 2002 <br />water supply as measured through the Arkansas River at Canon City gage. The reduced inflow to <br />Pueblo Reservoir and John Martin Reservoir due to the effect of the severe drought caused an <br />overall reduction in the Wmter Water storage program and conservation storage in John Martin <br />Reservoir, <br />
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