Abstract
A synergistic analysis of the radar-only and combined radar-lidar observations across the three platforms was conducted. To align with well-calibrated CloudSat cloud profiling radar (CPR) (and HCR) reflectivity measurements, a constant 4.5 dB offset was applied to all M-WACR reflectivitives during the MARCUS. This brings M-WACR data into better agreement with both HCR and CPR reflectivity measurements and facilitates a more reliable cloud fraction (CF) comparison. The total CFs (CFTs) derived from the three radars show excellent agreement. All three radars detect large drizzle drops, but M-WACR and HCR excel at detecting smaller cloud droplets that are often missed by CPR. The underestimated CFs by CPR are due to increased attenuation of CPR measurements below 3 km, and the combined effects of attenuation and surface clutter below 1 km. Combining radar and lidar observations enhanced cloud detection by 20%–60%. The results from this study provide new insights for designing future cloud radar systems.
| Original language | English (US) |
|---|---|
| Article number | e2024GL112079 |
| Journal | Geophysical Research Letters |
| Volume | 52 |
| Issue number | 9 |
| DOIs | |
| State | Published - May 16 2025 |
Keywords
- CloudSat CALIPSO
- MARCUS
- SOCRATES
- Southern Ocean
- cloud microphysics
- radar lidar
ASJC Scopus subject areas
- Geophysics
- General Earth and Planetary Sciences
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