Differential absorption radar techniques: water vapor retrievals
Two radar pulses sent at different frequencies near the 183 GHz water vapor line can be used to determine total column water vapor and water vapor profiles (within clouds or precipitation) exploiting the differential absorption on and off the line. We assess these water vapor measurements by applyin...
Main Authors: | , , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-06-01
|
Series: | Atmospheric Measurement Techniques |
Online Access: | http://www.atmos-meas-tech.net/9/2633/2016/amt-9-2633-2016.pdf |
Summary: | Two radar pulses sent at different frequencies near the 183 GHz water vapor
line can be used to determine total column water vapor and water vapor
profiles (within clouds or precipitation) exploiting the differential
absorption on and off the line. We assess these water vapor measurements by
applying a radar instrument simulator to CloudSat pixels and then running
end-to-end retrieval simulations. These end-to-end retrievals enable us to
fully characterize not only the expected precision but also their potential
biases, allowing us to select radar tones that maximize the water vapor
signal minimizing potential errors due to spectral variations in the target
extinction properties. A hypothetical CloudSat-like instrument with 500 m by
∼ 1 km vertical and horizontal resolution and a minimum detectable
signal and radar precision of −30 and 0.16 dBZ, respectively, can estimate
total column water vapor with an expected precision of around 0.03 cm, with
potential biases smaller than 0.26 cm most of the time, even under rainy
conditions. The expected precision for water vapor profiles was found to be around 89 % on average, with potential biases smaller than 77 % most of the time when the profile is being retrieved close to surface but
smaller than 38 % above 3 km. By using either horizontal or vertical
averaging, the precision will improve vastly, with the measurements still
retaining a considerably high vertical and/or horizontal resolution. |
---|---|
ISSN: | 1867-1381 1867-8548 |