Differential absorption radar techniques: Water vapor retrievals

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Abstract

Two radar pulses sent at different frequencies near the 183ĝ€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 500ĝ€m by ĝ1/4 ĝ€1ĝ€km vertical and horizontal resolution and a minimum detectable signal and radar precision of ĝ'30 and 0.16ĝ€dBZ, respectively, can estimate total column water vapor with an expected precision of around 0.03ĝ€cm, with potential biases smaller than 0.26ĝ€cm most of the time, even under rainy conditions. The expected precision for water vapor profiles was found to be around 89ĝ€% on average, with potential biases smaller than 77ĝ€% most of the time when the profile is being retrieved close to surface but smaller than 38ĝ€% above 3ĝ€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.

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APA

Millán, L., Lebsock, M., Livesey, N., & Tanelli, S. (2016). Differential absorption radar techniques: Water vapor retrievals. Atmospheric Measurement Techniques, 9(6), 2633–2646. https://doi.org/10.5194/amt-9-2633-2016

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