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Using some of the available doppler radars, it is possible to 'see' bird migration. Two of the common radar modes used are Base Reflectivity and Radial Velocity. Below are two of the common images looped so you can easily see the radar images (the current image with be shown).
Below are two radar images from the National Weather Service's doppler radar that can show migration of birds, bats and insects. Further down is some more information on interpreting the images for yourself. Observing migration on radar can be fascinating - but I don't think it can ever beat actually being out there!
Base Velocity loop
Base Reflectivity loop
Interpreting the images
Below is some initial information on how it works and here is a link to the Radar Ornithology Laboratory at Clemson University, which goes into great detail about radar types and how to interpret the radar images.
How it works (short version)
Migrating Birds (from Clemson's BirdRad)
At its lowest scanning level a NEXRAD antenna is set at a 0.5 degree elevation angle.
Therefore, as a radar beam travels farther from the antenna, it scans higher altitudes.
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a NEXRAD Volume Coverage Pattern (VCP 21, precip mode) |
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Birds migrating at night are typically most dense around 1500 ft (~500 m) above the ground.
Some may fly higher, frequently to 15,000 ft. (especially in trans-gulf migration) and occasionally to 20000 ft.
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Typical distribution of migrants with altitude |
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When a radar beam scans this distribution of targets, reflectivity
value rapidly increases with distance from the station. As the radar
scans above the densest layers of the migration pulse,
the reflectivity value gradually declines. The following figure
represents a hypothetical snapshot of nocturnal migration. In this
snapshot the most dense bird migration occurs where the black dots are
most numerous. When the radar beam scans this area, the reflected
energy from birds
is 25-30 dBZ represented by the darkest green dots. Again, note the
relationship between reflectivity and altitude. From ground level up to
the most dense bird layer, the reflectivity
value increases rapidly; from the most dense bird layer to much higher
altitudes, the reflectivity value decreases gradually.
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Birds overflying a NEXRAD station and detected as different reflectivities. |
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Note that no reflectors were detected by the radar near to or far
from the NEXRAD. This results in a "doughnut-shaped" pattern on the
radar scan.
| Precipitation mode base reflectivity image of birds overflying POE Ft. Polk, Louisiana. |
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| dBZ |
Birds
/km3 |
| ND |
| 5 |
59 |
| 10 |
71 |
| 15 |
109 |
| 20 |
227 |
| 25 |
602 |
| 30 |
1788 |
| 35 |
| 40 |
| 45 |
| 50 |
| 55 |
| 60 |
| 65 |
| 70 |
| 75 |
|
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Base Ref 124nm
Elev=0.5 deg
1.16 km²/pixel
POE: Ft. Polk LA
31.16N 92.98W
04/22/99 17:41
Precip
VCP 32
Max: 43 dBz |
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The reflectors nearest the station are "ground clutter" caused by radar returns from objects on the ground such as trees, buildings and even vehicles.
Read more about Bird Migration and Radar at the Radar Ornithology Laboratory at Clemson University (CUROL) .
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