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A New Algorithm to Identify Errors
Caused by Migrating Birds in Profiler Winds
On August 15, 1996, a new Quality Control
(QC) algorithm was implemented on the hourly winds from the
NOAA Profiler Network (formerly called the Wind Profiler
Demonstration Network). The algorithm is designed to flag
winds that are suspect of being biased in wind velocity or
direction by migrating birds. The algorithm is applied only
at night, only below 4.5 km above mean sea level (below about
570 mb or 15,000 feet), and only during the spring and fall
migration periods. No change to any existing profiler display
software is expected. Winds suspected of being biased by
migrating birds are identified as failing QC. A more detailed
description follows, covering bird migration patterns, the
new QC algorithm, and the results of an experiment conducted
to determine the impact of birds to the wind profiler data,
and to evaluate the performance of the algorithm (Miller et
al., 1997).
Bird Migration Patterns
Different species of birds migrate at
different times of the year. Definite peak migration periods
occur at night during the spring and fall when low-level
winds are favorable for their direction of travel.
Specifically, they migrate northward during the spring using
the low-level southerly jet, and southward in the fall. Large
migrating geese are not a major problem to the profiler, as
might be expected. The birds that cause the greatest impact
to the profilers are small songbirds (passerines) that fly in
a dispersed pattern rather than a tight flock. They typically
start flying about 30 minutes after sunset and continue until
about 30 minutes before sunrise, flying at an altitude of
most favorable tailwinds (or very weak headwinds), generally
< 2-4 km above the ground. Their maximum height appears to
be limited by the ambient air temperature (>
-2oC). They typically fly at a lower maximum
altitude in the spring (using the nocturnal low-level
southerly jet) compared to the fall (when they fly at greater
heights, apparently in the warmer, deeper mixed layer). The
birds typically fly with an airspeed of about 8-15
ms-1(15-30 knots) (Wilczak et al., 1995).
Contamination of Wind Profiler
Data Caused by Birds
Wind profiling radars are designed to
measure the extremely weak signals from the clear air
throughout the troposphere and lower stratosphere. These weak
signals require a long averaging time (1-minute) in each of
the three fixed beam positions used by the profilers
(generally pointing toward the east, north, and vertical).
The reflected energy from a single bird flying through the
radar beam even for just a few seconds is much greater than
the clear-air signal averaged over the 1-minute dwell time.
Therefore, the profiler reports a velocity equal to the
flying speed of the bird(s) toward or away from the profiler
(most noted in the northward pointing beam). The existing
hourly consensus averaging algorithm (used for the past 10 +
years) effectively removes isolated (a few per hour)
erroneous velocity measurements before averaging the
remaining "good" points. Problems occur when consistent "bad"
data (in time) are competing with, or overwhelming, the
"good" wind data. In addition, because the birds produce
higher reflectivity than clear-air, they can also be detected
as they fly through the profiler's antenna sidelobes. This
causes differing velocity and spectral width components to be
measured and averaged together. However, the erroneous
positive and negative velocity measurements may average out
to nearly the correct background wind, while the wider than
normal spectral widths remain (a key element in the QC
algorithm). In order to measure the extent of the
contamination, data from four profilers in Kansas and
Oklahoma were compared with data from collocated rawinsondes
that were launched every 3 hours during the spring and fall
of 1994. The mean (additional) error attributed to the
migrating birds was found to be only about 2
ms-1(biased toward higher wind velocity), with
larger errors possible up to the airspeed of the birds (15
ms-1), although errors this large were rare. The
likelihood of bird caused errors > 8 ms-1was
only 5% during migration periods. In total, it was found that
during the spring and fall migration periods, only about 2%
of all the profiler wind data were being contaminated by
birds (when considering all wind measurements in height and
time). Although a small amount, the impact of these biased
(high) wind velocities were significant at times to numerical
model output and forecasts in the central plains of the
U.S.
The Bird Detection Algorithm
A check for bird contamination in the
hourly winds was devised by two meteorologists (F.M. Ralph
and D.W. van de Kamp), based on work reported in Wilczak et
al. (1995), and their personal observations. It is a simple
six-step test that is primarily based on identifying the
larger velocity variance signature thought to accompany the
backscattered radar returns from birds. The other steps in
the test are meant to reduce the likelihood of false alarms.
The check flags an hourly observation as contaminated if all
the following criteria are met:
-
The time of year is appropriate for
bird migration ("spring": 15 February - 15 June or "fall":
9 August - 30 November).
-
The time of day is appropriate
("night": 0200 - 1200 UTC during the spring, 0000 - 1300
UTC during the fall, i.e., local civil twilight following
sunset to local civil twilight preceding sunrise).
-
The height is appropriate (< 4500 m MSL).
-
The wind direction is favorable for
migration (90º- 270º in the spring,
0º- 90º or 270º-360º in the fall).
-
The velocity variance signature is
appropriate (average of the north, east and vertical beams > 1.4
m2/s2).
-
The increased velocity variance is not
a result of precipitation (magnitude of downward vertical
velocity < 0.8 ms-1(wider spectral widths
naturally occur during precipitation)).
The rawinsonde data were also used to
statistically evaluate the algorithm. The Probability of
Detection (POD) was generally good, successfully flagging
over 60% of the "identified" bird contaminated wind data.
(Bird contamination was defined by computing the standard
deviation of wind component velocity differences
(approximately 2 ms-1) during non-bird migration
periods, and using two times this standard deviation as the
threshold for identifying velocity contamination in the
spring and fall.) A rather high False Alarm Rate (FAR) of 44%
was noted. This appears to be due to the positive and
negative velocity errors (caused by birds in the sidelobes)
averaging out to near the true wind velocity, while the
spectral width average remains high and trips the bird
detection algorithm. Therefore, the FAR appears to be
somewhat fictitiously high. Further evaluation and
adjustments to the algorithm are expected.
An obvious change after the algorithm
became operational on August 15, was an increase in the
number of winds below 4.5 km being flagged as failing QC. Use
your best judgment to interpret these winds. For further
information, contact Doug van de Kamp at (303) 497-6309 or
vandekamp@fsl.noaa.gov, or the Profiler Control Center at
(303) 497-6033.
References
Miller, P.A., M.F. Barth, J.R. Smart, L.A. Benjamin, 1997:
The Extent of Bird Contamination in the Hourly Winds Measured
by the NOAA Profiler Network: Results Before and After
Implementation of the New Bird Contamination Quality Control
Check. Preprints, 1st Symposium on Integrated Observing
Systems, Long Beach, CA, Amer. Meteor. Soc., 138-144.
Wilczak, J.M., R.G. Strauch, F.M. Ralph, B.L. Weber, D.A.
Merritt, J.R. Jordan, D.E. Wolfe, L.K. Lewis, D.B. Wuertz,
J.E. Gaynor, S.A. McLaughlin, R.R. Rogers, A.C. Riddle, and
T.S. Dye, 1995: Contamination of Wind Profiler Data by
Migrating Birds: Characteristics of Corrupted Data and
Potential Solutions. J. Atmos. Oceanic Technol., 12, 449-467.
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