In order to understand
what is presented in this paper, you need to understand some background
information on the LA Aqueduct and more specifically the Mono Basin
Project.
The Mono Basin Project was developed to bring and obtain more water
for the city of Los Angles that was growing rapidly and needed more
water. The city of LA applied for permits to divert water from Lee Vining,
Walker, Parker, and Rush Creeks. By diverting this water it allowed
LA to supply water for 500,000 more people. They had one giant thing
standing in their way though, the Mono Craters. They decided to build
an 11-mile tunnel that went under the Mono Craters. Once completed it
increased LA’s water supply by 35% up to 300 million gallons per
day.
MONO LAKE
In 1941 Los Angles started diverting water from Mono Lake’s tributaries,
about 350 miles south of LA. As Mono Lake became deprived of its freshwater
sources the lake level began to drop, and almost halved.
The current volume of Mono Lake is 2.6 million acre-feet at 6382.8 ft.
This current year so far the runoff of snow and rain is slowly becoming
a dry/normal season. So far this year the total is 99,800 acre-feet
of runoff, the average is 122,124 acre-feet.
Below is a graph showing the snow pack for Mammoth Pass, which does
feed into creek and streams and other sources that feed into Mono Lake.
The snow pack helps in what was mentioned before in run-off.
Another contributing factor to the dry runoff so far
is precipitation. Below is chart showing the percent of normal precipitation
to date.
Precipitation percentage of normal
to current date
SNOW SURVEYS
About 65% of the water comes from the
Sierra Nevada Mountains runoff. Accurate measures of the snow are very
important to LA in order to be able to forecast each year’s water
supply. Each winter Department of Water and Power (DWP) trek it up into
the Sierra’s to measure the depth and water content in the snow
at certain specific points and over periods of many years forecasters
can accurately predict the amount of runoff each year.
STREAMS DIVERTED by the LA AQUEDUCT
Lee Vining Creek is the second
largest stream in the Mono Basin, carrying about 33% of the total runoff.
It’s a 47 square mile watershed that starts at 13,053 ft. at the
foot of Mt. Dana in the Ansel Adams Wilderness. Before the dams where
built peak stream lows would reach as high as 650 cfs at the height
of snowmelt.
Figure shows stream flows from 10/1935 till 12/79
http://waterdata.usgs.gov/nwis/discharge/?site_no=10287900
Each year has a different stream
flow then the year before. Really high peaks on the chart show years
that had a very high stream flow, example 1943. When the peaks are much
lower the year is having a low flow year. This could be the result of
a lot of things. For example, low snowfall, not much rain, maybe LA
diverted some of the water and at the point these readings were taking
they were lower than the structure that diverts the water.
In 1941 diversions from Lee Vining creek into the aqueduct began. After
1971 high runoff stopped and irrigation ended, causing the stream to
dry up. From below Hwy 395 vegetation declined and was severely affected
all the way to Mono Lake. Up until 1969 the stream was basically dry,
until a flood caused widening of the stream.
As of 1989 there was a loss of 50% of what existed before 1941. Currently
there are various measures are being used to restore the creek to the
way it was before 1941.
Rush creek is the largest stream in the Mono Basin carrying about 41%
of the total runoff. It’s a 141 square mile watershed that begins
Mt. Lyell at about 13,000 ft. also in the Ansel Adams Wilderness. Each
year the stream provides an average of 59,200 acre-feet of runoff. Before
the damn was built peak stream flows would reach 1100 cfs.
As you can see from the chart below that has changed since the aqueduct
was put in.
Figure shows stream flows from 10/1969 till 9/1990
http://waterdata.usgs.gov/nwis/discharge/?site_no=10287290
From 1947-1951 there was
very low runoff and below Hwy 395 pine trees died. Low releases continued
again in the early 1960’s causing a loss of vegetation. With the
vegetation dying extreme floods scoured the channels and removed large
amounts of live and dead vegetation and topsoil in 1967 and 1969. By
this time Mono Lake had dropped 28 feet, and Rush Creek’s floodplain
had dropped in order to reach this lower lake level.
The third creek is Parker Creek, which carries 6% of the total of the
Mono Basin runoff. Its 12 square mile watershed begins at 13,000 ft.
at the foot of Kuna Peak in the Ansel Adams Wilderness. The average
runoff each year is 9100 acre-feet and at peak snowmelt flows can reach
90 cfs.
Figure shows daily, measured, and estimated stream
flow from 10/1945 till 9/2000
http://waterdata.usgs.gov/nwis/discharge/?site_no=01101000
Lee Vining crosses Parker Creek above irrigated land.
Since 1947 LA has diverted almost all of the water in Parker Creek into
the aqueduct. This caused the creek to dry up below the conduit. When
it began to dry up this caused a loss of vegetation and aquatic habitat.
Gravel was then pushed into the dry channel by CalTrans, which formed
a feature know as “Parker Plug,” which was removed in 1990,
marking the start of the Parker Creek restoration project. (p. 3C-25,
Mono Basin EIR, 1993)
As of 1989 there were 49 acres of woody vegetation, 9 acres less than
before 1941 conditions. In 1990 water flowed down Parker Creek again
due to a court order.
The last creek to be diverted is Walker Creek. Walker Creek carries
4% of the total Mono Basin Runoff. An average of 5400 acre-feet of runoff
each year flows, and during peak snowmelt average peak flows could reach
70 cfs.
Figure shows stream flow from 8/1965 till 9/1981
http://waterdata.usgs.gov/nwis/discharge/?site_no=11390660
Since 1947 LA diverted virtually
all of the water in Walker Creek. This caused the stream to dry up below
the conduit causing a loss of vegetation and aquatic habitat. Currently
there are 7 acres less than pre-1947 conditions. In 1990 water started
flowing down the stream again as a result of a court order.
Figure shows creeks, lakes, and conduits.
http://web.ladwp.com/~wsoweb/Aqueduct/realtime/monorealtime.htm
Since 1941 LA has been diverting water via the aqueduct. This is not
the only place that they have taken water from. For about 50 years LA
diverted water uncontested, until people started to realize what exactly
was happening to the environment around. By people stepping up and starting
to take action the LA Aqueduct has been ordered to return Mono Lake
back to a set depth and to return the streams to set court orders.
WORKS SITED
http://www.monobasinresearch.org
http://www.laaqueduct.com
http://www.usgs.gov
http://waterdata.usgs.gov