evapotranspiration (et) in the lower walker river basin, west- central nevada by kip k. allander, j....
TRANSCRIPT
![Page 1: Evapotranspiration (ET) in the Lower Walker River Basin, West- Central Nevada By Kip K. Allander, J. LaRue Smith, Michael J. Johnson, U.S. Geological Survey,](https://reader035.vdocuments.mx/reader035/viewer/2022062518/56649e715503460f94b702d3/html5/thumbnails/1.jpg)
Evapotranspiration (ET) in the Lower Walker River
Basin, West-Central Nevada
ByKip K. Allander, J. LaRue Smith,
Michael J. Johnson, U.S. Geological Survey, Nevada Water Science Center
and Robert PattisonU.S. Department of Agriculture, Agricultural Research
Service
Nevada Water Resources Nevada Water Resources AssociationAssociation
2006 Annual Conference; Mesquite, 2006 Annual Conference; Mesquite, NVNV
February 23, 2006February 23, 2006
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Overview
• Objective• Study Design
– ET Network– Scaling up of ET
• Results– ET at Walker
Lake– ET at Saltcedar– ET summary
Main area of interest for ET study
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Objective
The primary objective of the ET component of the Walker River Basin project is to estimate ET losses from . . .
Natural Vegetation,
Agricultural Vegetation,
and from open-water surfaces.
Photo by Jim CromptonPhoto by Jim Crompton
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Study Design
• 8 ET Stations• 5 are Bowen-ratio
method• 3 are Eddy-
covariancemethod (3D)
RAWS Dead Camel Site
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Quantifying ET across the Study Area
• Create map of ET units– Airborne imagery– Lidar
This image is an example of an ET unit map obtained from Laczniak and others, 2001, Ground-water discharge determined from estimates of ET, Death Valley Regional Flow System, NV and CA: USGS WRIR 01-4195, p. 23.
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Imagery (infrared)
• Color infrared imagery will be used to classify vegetation based on its relative vigor and soil conditions.
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Imagery (natural color)• Natural color imagery will be used to define the
extent of riparian and phreatophytic vegetation.
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Lidar• Lidar imagery will be used to estimate
vegetation density and canopy height.
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Results – Evaporation (E) from Walker Lake
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Measured E on Walker Lake
Water Year 2005
Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep Oct
Eva
po
rati
on
(m
m)
0
2
4
6
8
10
12
14
Daily EData gaps
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E compared with Net Radiation on Walker Lake
Water Year 2005
Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep Oct
Evap
ora
tio
n (
mm
)
0
2
4
6
8
10
12
14
Mean
Da
ily
Ne
t R
ad
iati
on
(W
/m2 )
-50
0
50
100
150
200
250
300Daily ENet RadiationData gaps
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RAWS – Dead Camel Site
Photo obtained from Photo obtained from http://www.wrcc.dri.edu/wraws/pictures/ndea/200509/ndea.ST3.jpg
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E at Walker Lake compared with RAWS solar radiation
Water Year 2005
Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep Oct
Eva
po
rati
on
(m
m)
0
2
4
6
8
10
12
14
Dai
ly S
ola
r R
adia
tio
n (
kW-h
r/m
2)
0
2
4
6
8
10
12
Daily E RAWS Solar Radiation
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Relation between E at Walker Lake and RAWS solar radiation
y = 0.0548x2 + 0.5356x
R2 = 0.6533
0
2
4
6
8
10
12
14
0 2 4 6 8 10 12
Daily Solar Radiation (x) kW-hr/m^2
Dai
ly E
vapo
ratio
n (y
) in
mm
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Total E for Water Year (WY) 2005
Water Year 2005
Oct Nov Dec Jan Feb Mar Apr May Jun Jul Aug Sep Oct
Ev
ap
ora
tio
n (
mm
)
0
2
4
6
8
10
12
14
Daily EEstimated daily E
Total E, WY 2005 = 1,814 mm or 6.0 ft*
* Provisional data has not received final approval and is subject to change with further review
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Results – ET from Walker Lake
• Preliminary estimate of ET for WY 2005 was 6.0 ft*, up from previous estimates of 4.1 ft.
• Surface area of Walker Lake in June 2005 was 32,000 acres.
• Estimated water volume evaporated from Walker Lake in WY2005 was 191,000 acre-ft*.
• ~ 50% increase over previous estimates.• If relation between lake ET and RAWS solar
radiation data holds, may be able to estimate annual ET back to 1999.
* Provisional data has not received final approval and is subject to change with further review
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Results – Saltcedar site
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Saltcedar site• Site underwent substantial defoliation due
to introduction of a biologic control agent: Saltcedar Leaf Beetle (Diorhabda elongata)
• Changed characteristics and ET rate for large stand of Saltcedar
Photo by Robert Pattison Photo by Robert Pattison
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Date 2005
Mar Apr May Jun Jul Aug Sep Oct Nov
ET
(m
m)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
Leaf
Cov
er (
%)
0
20
40
60
80
100
SaltcedarSaltcedar Leaf Cover
Measured ET at SaltcedarRed line represents a “Conceptual ET Curve” for a vegetation with shallow depth to ground water, such as is the case with this site. This conceptual curve is intended to demonstrate seasonal variability more than seasonal magnitude.
Error bars represent standard error
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Comparison with Saltgrass ET
Date 2005
Mar Apr May Jun Jul Aug Sep Oct Nov
ET
(m
m)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
Leaf
Cov
er (
%)
0
20
40
60
80
100
SaltcedarSaltgrassSaltcedar Leaf Cover
Period used in regression
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Relation between ET at Saltcedar and Saltgrass
y = 0.7985x + 0.7609
R2 = 0.5962
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
0.0 0.5 1.0 1.5 2.0 2.5
Saltgrass ET (mm)
Sal
tced
ar E
T (
mm
)
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Saltgrass ET normalized to Saltcedar ET
Date 2005
Mar Apr May Jun Jul Aug Sep Oct Nov
ET
(m
m)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
Leaf
Cov
er (
%)
0
20
40
60
80
100
SaltcedarNormalized SaltgrassSaltcedar Leaf Cover
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Reduction of ET using Saltgrass comparison
Date 2005
Mar May Jul Sep Nov
ET
(m
m)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
Lea
f C
ove
r (%
)
0
20
40
60
80
100
SaltcedarNormalized SaltgrassSaltcedar Leaf Cover
203 mm*
57 mm*
This is a 22% reduction in ET*
* Provisional data has not received final approval and is subject to change with further review
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Comparison with Willow ET
Date 2005
Mar Apr May Jun Jul Aug Sep Oct Nov
ET
(m
m)
0
2
4
6
8
10
12
Leaf
Cov
er (
%)
0
20
40
60
80
100
SaltcedarWillowSaltcedar Leaf Cover
Period used in regression
![Page 25: Evapotranspiration (ET) in the Lower Walker River Basin, West- Central Nevada By Kip K. Allander, J. LaRue Smith, Michael J. Johnson, U.S. Geological Survey,](https://reader035.vdocuments.mx/reader035/viewer/2022062518/56649e715503460f94b702d3/html5/thumbnails/25.jpg)
Relation between ET at Saltcedar and Willow
y = -0.0015x + 1.8512(mean difference is 1.85 mm/day)
0.00
0.50
1.00
1.50
2.00
2.50
3.00
3.50
0.00 2.00 4.00 6.00 8.00 10.00
Willow ET (mm)
Sal
tced
ar E
T (
mm
)
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Reduction of ET using Willow comparison
Date 2005
Mar Apr May Jun Jul Aug Sep Oct Nov
ET
(m
m)
0.0
0.5
1.0
1.5
2.0
2.5
3.0
3.5
Le
af C
ove
r (%
)
0
20
40
60
80
100
SaltcedarNormalized WillowSaltcedar Leaf Cover
203 mm*
58 mm*
This is a 22% reduction in ET*
* Provisional data has not received final approval and is subject to change with further review
![Page 27: Evapotranspiration (ET) in the Lower Walker River Basin, West- Central Nevada By Kip K. Allander, J. LaRue Smith, Michael J. Johnson, U.S. Geological Survey,](https://reader035.vdocuments.mx/reader035/viewer/2022062518/56649e715503460f94b702d3/html5/thumbnails/27.jpg)
Results – Saltcedar site
• Saltcedar underwent substantial defoliation and associated reduction of ET due to introduction of biologic agent.
• ET rate may have been reduced by more than 20%, but a reduction even greater than this is likely.
• Saltcedar ET rates of 4.0 ft/yr have been observed in Southern Nevada.
• Actual pre-Saltcedar Beetle ET rates from Saltcedar in study area are undetermined at this time.
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ET Station
Wa
lke
r L
ak
e
Wil
low
Alf
alf
a B
11
Alf
alf
a B
01
Sa
ltg
ras
s
Sa
ltc
ed
ar
Ra
bb
itb
rus
h
Gre
as
ew
oo
d
ET
(in
ch
es
)
0
20
40
60
80
2005 Growing Season2005 Water Year
Results – ET Summary6.0 ft*
3.5 ft* 3.3 ft*2.8 ft*
0.7 ft* 0.7 ft*0.4 ft* 0.4 ft*
* Provisional data has not received final approval and is subject to change with further review
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Summary
• Open water has the greatest ET rates, followed by Willows and then Alfalfa.
• E from Walker Lake for 2005 water year was nearly 6 ft*, almost 2 ft greater than previous estimates.
• Estimated volume evaporated from Walker Lake is approximately 50%* greater than previous estimates.
• ET rates in Saltcedar were reduced by more than 20%* with newly introduced biologic control, but a reduction even greater than this is likely.
* Provisional data has not received final approval and is subject to change with further review
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http://nevada.usgs.gov/walker/