Title: EVALUATING METEOROLOGICAL MONITORING SITES USING SIGMA-THETA
1EVALUATING METEOROLOGICAL MONITORING SITESUSING
SIGMA-THETA
Kenneth G. WastrackDoyle E. PittmanTENNESSEE
VALLEY AUTHORITY
2Background
- A 2002 NUMUG presentation discussed using
Sigma-Theta to determine if trees and tower
structures were impacting wind data. - The Impact of Nearby Structures and Trees on
Sigma Theta Measurements, by Tom Bellinger - TVA used this approach to examine its
meteorological monitoring sites.
3Methodology
- TVA sigma measurements.
- Sigma-Y (replaced in 1989).
- Average of 12 5-minute WD Standard Deviations
- Hourly Sigma-Theta.
- Sigma-Theta based on 720 WD readings.
- 15-minute Sigma-Theta.
- RMS of 4 15-minute Sigma-Thetas.
- 15-minute Sigma-Thetas based on 180 WD readings
each. - Annual average of 15-minute Sigma-Thetas.
- Did not include cases with WS lt 5 mph.
- Sorted into 10 degree WD sectors.
- Used 25 degrees as arbitrary cut-off in analysis.
4Watts Bar Nuclear Plant15-Minute Sigma-Theta for
wind speeds 5 mph and greater(6-year average,
1997-2002)
- 10-meter values are generally less than 25
degrees. - Values above 25 degrees are due to identifiable
causes.
5Sequoyah Nuclear Plant15-Minute Sigma-Theta for
wind speeds 5 mph and greater(6-year average,
1997-2002)
- More cases with 10-meter values above 25 degrees.
- Values above 25 degrees still due to identifiable
causes.
6Browns Ferry Nuclear Plant15-Minute Sigma-Theta
for wind speeds 5 mph and greater(6-year
average, 1997-2002)
- Some high cases, but most are below 25 degrees.
- Most values above 25 degrees due to identifiable
causes.
7Browns Ferry Nuclear Plant15-Minute Sigma-Theta
for wind speeds 5 mph and greater(6-year
average, 1997-2002)
Why is there a dip in 10-meter Sigma-Theta? (Dip
is not consistent with obstructions.)
8Browns Ferry Nuclear Plant10-meter level -
15-Minute Sigma-Theta Recent History(wind speeds
5 mph and greater)
- Dip in Sigma-Theta is consistent over time.
- Dip is not due to a recent change.
9Browns Ferry Environs
0.5 mile
Browns Ferry Nuclear Plant
Meteorological Monitoring Site
Tennessee River (Wheeler Reservoir)
10Meteorological Monitoring Site
Warehouses Training Center
Trees
Target Range
Tennessee River (Wheeler Reservoir)
Except for a few isolated trees, everything meets
110 criteria.
11Browns Ferry Meteorological Monitoring
Site(looking south from tower)
Direction of Sigma-Theta Dip
Target Range Berm
12Effects of Changes
- Reason for dip in Sigma-Theta curve is not
apparent. - Need to examine changes.
- Has dip in curve always existed?
- If not, when did change occur?
13Browns Ferry Nuclear PlantHistory of Site
Changes Impacting Sigma-Theta Measurements
- March 1973 Start monitoring at permanent
meteorological tower. - October 1977 Clear trees to meet 110 height
criteria. - July 1989 Change sigma calculation methodology.
- April 1991 Complete new berms around target
range adjacent to meteorological tower site. - February 2000 Change orientation of wind sensor
mounting arm (old into WNW, new into ENE). - February 2001 Change to ultrasonic wind sensors
(included slight changes in wind sensor
elevations).
141997-2002 Average 10-meter Sigma-Theta(displayed
on polar coordinates)
Portion that corresponds to dip in line chart
curve.
15Effects of Cutting Trees to Meet 110
Criteria(before trees cut, some high sigma
values)
Trees before cutting
16Effects of Cutting Trees to Meet 110
Criteria(after trees cut, sigma values much
improved)
17Effects of Building Firing Range Berm(before
berm is built, some high sigmas in SW quadrant)
18Effects of Building Firing Range Berm(after berm
is built, sigmas increase in SW quadrant)
19Change in Wind Sensor Orientation (generally no
change, dip is present both before and after)
20Preliminary Results
- 1977-78 Changes in Sigma-Y after trees are cut
shows general improvement but does not indicate
possible dip. - 1989-93 Dip is not apparent both before and
after target range berm was built. - 1997-2002 Dip is present both before and after
change in sensor orientation.
Therefore, Sigma-Theta curve changed between 1993
and 1997.
21Change in Sigma-Theta Curve (Dip not present in
1992-1993. Dip present in 1997-1999)
22Further Analysis
- Dip appears to be related to narrow band of trees
adjacent to river. - At 1993 NUMUG meeting, TVA presentation indicated
that a temperature anomaly was partly due to the
horizontal extent of a terrain feature. - Identification and Implications of a Local
Temperature Anomaly, by Ken Wastrack Norris
Nielsen - Therefore, TVA examined not only the presence of
obstructions, but also their horizontal extent.
23Sigma-Theta and Distance from Tower (Sigma-Theta
scale on left, Distance scale on right)
24Sigma-Theta and Distance from Tower (Add actual
Sigma-Theta)
25Sigma-Theta and Distance from Tower (Add
reservoir, trees, and target range)
26Sigma-Theta and Distance from Tower (Show narrow
band of trees, Remove reservoir to simplify)
- Band of trees less than 100 meters wide.
27Sigma-Theta and Distance from Tower (Examine
portion of curve with dip)
- Dip is related to unobstructed narrow band of
trees.
28Sigma-Theta and Distance from Tower (What would
curve look like without target range?)
- Expected Sigma-Theta estimated based on tree band
width.
29Conclusions
- Dip in Sigma-Theta curve is due to an narrow band
of trees unobstructed by the target range. - Dip represents relatively unobstructed wind flow.
- Tree band is narrow behind target range, but
Sigma-Theta values are greater from direction of
target range. - Even though it meets obstruction criteria, berm
still impacts measurements.
30Remember Ruckert's Law.
There is nothing so small that it can't be blown
out of proportion.