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As steward of the lower Colorado River, LCRA carefully manages the water in the river and the Highland Lakes. But there are times — during a drought, for example — when there may not be enough water for everyone. The graphic below shows the current storage level in lakes Buchanan and Travis —
the only water supply reservoirs in the Highland Lakes chain. When the water in these lakes drops below specific “trigger points,” some users receive less water. |
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Enter numbers in the boxes to change total volume – and
learn below how this
may trigger action to curtail water to specific users.
Buchanan
feet above msl
(Enter number between 912, the lake’s level when empty, and 1,025, the top of Buchanan Dam.)
Travis
feet
above msl (Enter number between 502, the lake level when empty,
and 750, the top of Mansfield Dam.)
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Trigger points: How LCRA priortizes water during
droughts
LCRA's state-approved Water
Management Plan is designed to prioritize water during droughts based
on the combined storage of lakes Travis and Buchanan. The lower the water
drops, the stronger the actions required to limit water use. Below are
specifics:
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2.01 million acre-feet: Lakes
considered full. This translates to 681 feet above mean sea level (msl) for
Lake Travis, and 1,020 feet (msl) for Lake Buchanan.
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1.897 million acre-feet: When the
combined volume of the lakes falls below 94 percent of total capacity on either
Jan. 1 or July 1, customers with “interruptible” water contracts — such as golf
courses — are required to cease diversions. This does not affect large
irrigation operations downstream.
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1.7 million acre-feet: If at or below
this level on Jan 1, begin reducing releases for
Matagorda Bay and estuaries.
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1.6 million acre-feet: If reached at
any time during the year, request voluntary water conservation from all
customers.
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1.1 million acre-feet: If the shortage
intensifies so that the volume drops to less than 1.1 million acre-feet on Jan.
1, large irrigation operations downstream, including
rice irrigation districts, are required to reduce diversions of water.
Water also is curtailed for "instream flow" designed for environmental needs.
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900,000 acre-feet: If reached at any
time during the year, request mandatory conservation from all customers.
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600,000 acre-feet: Begin pro-rata
curtailment of firm water customers when Board declares a drought worse than
"drought of record."
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325,000 acre-feet: If at or below this
level on Jan. 1, cease all water to interruptible customers for the coming
year.
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200,000 acre-feet: If reached at any
time during the year, immediate and total cutoff of Highland Lakes’ water for
rice irrigation.
Terms to know
*Acre-foot: The amount of water required to cover an area of
one acre to a depth of one foot. One acre-foot of water is equal to almost
326,000 gallons.
Drought of record: The decade-long drought that affected
Central Texas from the late 1940s through the late 1950s. (See
LCRA history.) No other drought in recent history was as severe or as
sustained. LCRA and other organizations use it as a benchmark to compare recent
droughts and to prepare for future droughts.
Firm water: The amount of water lakes Buchanan and Travis could
supply during a repeat of the most severe drought on record. Most of this water
is committed for use by cities, industries, power plants and protection of
aquatic life.
Interruptible water: Water that is available for use on a
year-to-year basis, depending on how much water is stored in lakes Travis and
Buchanan. Interruptible water is subject to curtailment during water shortages.
Mean sea level (msl): A point of reference to measure lake
elevation. It refers to the elevation of the ocean halfway between high and low
tide. Lake elevations are measured in feet above mean sea level.
Learn more:
Overview: managing the water supply and state preferences |
Water Management Plan | What
happens in a drought? | Water
contracts
guarantee supplies even during severe drought (with pie chart graphic)
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Water conservation
Note on calculations: The volume of water
in the lakes shifts constantly
because of the build-up of sedimentation, changes in river channels and other
factors. The calculations above are based on the latest hydrological surveys
available.
Lake Buchanan’s volume is from an LCRA hydro survey in 1991 plus aerial
mapping in 1997 (based on
National Geodetic Vertical Datum of 1929). Lake
Travis’ is from an LCRA hydro survey in 1992-1993 and aerial mapping
in 1997 (NGVD 29).
-- Published Feb. 1, 2006
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