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WSP06317
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Last modified
1/26/2010 2:22:12 PM
Creation date
10/12/2006 1:33:39 AM
Metadata
Fields
Template:
Water Supply Protection
File Number
8056
Description
Drought Preparedness
State
CO
Basin
Statewide
Date
6/1/1996
Author
Drought Study Team
Title
Severe Sustained Drought - Managing the Colorado River System in Times of Water Shortage
Water Supply Pro - Doc Type
Report/Study
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<br />6, <br /> <br />T' <br /> <br />0030iJ2 <br /> <br />COLORADO WATER <br /> <br />June 1996 <br /> <br />., <br /> <br />. Studies of potential environmental impacts of different <br />hydrologic scenarios; <br /> <br />DROUGHT SCENARIOS <br /> <br />The initial step was to select a representative SSD, and for this <br />study a hydrologic measure as a basic indicator of drought <br />was chosen - river nows relative to long~tenn averages. <br />However. the hydrologic measure was derived from tree ring <br />srudies of long-tenn climatic behavior. <br /> <br />The hydrologic analysis commenced with an estimated <br />measure of native flows at Lees Ferry, just below Glen <br />Canyon Dam in northeastern Arizona. where convention and <br />iaw divides the Colorado into Upper and Lower Basins, <br /> <br />. Economic projections of water-reiated benefits and costs <br />of such scenarios; <br /> <br />Explorations of the social impacts of drought in the basin <br />states; and <br /> <br />. A gaming experiment in changing rules for managing <br />thesystem as the drought progresses. <br /> <br />The study was conducted <br />by an interdisciplinary team <br />from the Universities of <br />Arizona, California, <br />Colorado, Nevada and <br />Wyoming, plus faculty at <br />Colorado State and Utah <br />State Universities and the <br />consulting finn <br />Hydrosphere, Inc" based in <br />Boulder, Colorado. <br /> <br />Included on the team were <br />engineerlhydrologists, tree <br />ring scientists, attorneys, <br />environmental scientists, <br />economists, sociologists <br />and public administration <br />specialists, The study <br />group was overseen by a <br />consonium of the Water <br />Research Institutes in the <br />Colorado River Basin <br />states, with major funding <br />provided by the U.s, <br />Interior Department and the <br />V,S, Anny Corps of <br />Engineers, <br /> <br />OBJECTIVES <br /> <br />25 <br /> <br />20 <br /> <br />~ 15 <br /><I: <br />~ <br />~ <br />:l <br />~1O <br /> <br />o <br /> <br />Figu re 2. <br /> <br />The representative 38- <br />year drought period <br />adopted for this study <br />was patterned after (but <br />not identical to ) the most <br />severe and long-Ia~ting <br />dry period identified by <br />tree ring srudies, the <br />period for the years 1579 <br />to 1616, <br /> <br />Colorado River Rearranged Severe Drought <br />and Recovery Period. <br /> <br />.... <br /> <br />Analysis period including drought <br />and recovery 1579 to 1616 <br /> <br />~ <br /> <br />5 <br /> <br /> <br />I. Colorado River <br />Basin Severe Drought <br /> <br /> <br />Drought scenarios were <br />defined in tenns of <br />aggregate annual flows <br />(in million acre-feet), <br />The scenarios included: <br /> <br />.... ~ The period 1579-1600 is <br />the most severe sustained <br />Rearranged flows drought that occurred in <br />tree ring reconstruction of <br />Lees Ferry streamflow, It <br />1580 1590 1600 1610 1620 is characterized by a 22- <br />year mean streamflow of <br />Year 11.1 maf with mean <br />streamflow over the first <br />17 years of only [0.5 <br />maf. compared [0 mean <br />recorded native streamflow of 15.2 mat). This drought is <br />estimated to have a return period between 400 to 700 years. <br /> <br /> <br />Taking the present-day configuration of the storage and <br />diversion structures and [he economic conditions in the <br />Basin as the base-point, Phase II objectives were: <br /> <br />. <br /> <br />2. Colorado Drought in Historic Record <br /> <br />The period 1943 to 1964 is the most severe drought that <br />occurred in the observed Lees Ferry streamflow record dating <br />to 1906, II is characterized by a 22-year mean flow of 13.4 <br />maf(eompared to the observed mean 'of 15.2 mat), The return <br />period is estimated to be between 50 and 100 years, regardless <br />of uncenainty in tree ring reconstructions of streamflow. <br /> <br />To assess the hydrologic impacts of a Severe Sustained <br />Drought (SSD); <br /> <br />. <br /> <br />To forecas[ [he economic, social and environmental <br />impacts on the southwestern U.S,; and <br /> <br />To assess po[ential altema[ive institutional arrangemen[s <br />for coping with an SSD, <br />
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