Correcting Propagation Effects in C-Band Polarimetric Radar Observations of Tropical Convection Using Differential Propagation Phase

By Lawrence D. Carey, S. Rutledge, D. Ahijevych, T. Keenan. 2000

179 citations recorded by the source corpus.

View Paper: https://www.semanticscholar.org/paper/d0b6201e1f4495b4a02f9a32d496e7c9e2f2df52

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In Atmospheric Science

Citations in the corpus

The 29 June 2000 Supercell Observed during STEPS. Part I: Kinematics and Microphysics (2005, methodology): “Specific differential phase (Kdp) was then calculated from the differential phase in the manner outlined in Hubbert and Bringi (1995) and Carey et al. (2000).”
Radar observations of the kinematic, microphysical, and precipitation characteristics of two MCSs in TRMM LBA (2002, methodology): “Prior to unfolding radial velocities, the S-Pol data were processed to eliminate ground clutter using thresholds in ρHV and ΨDP [Ryzhkov and Zrnic ́, 1998] and to calculate specific differential phase (KDP) from the total differential phase (ΨDP) data as described in Hubbert and Bringi [1995] and Ca”
Comparison of Advanced Radar Polarimetric Techniques for Operational Attenuation Correction at C Band (2008, unknown): “…technique (hereafter PDP), based on the relation between differential phase dp and cumulative attenuation Ahh, and cumulative differential attenuation Adp, respectively, has been proposed by Bringi et al. (1990) and evaluated by other authors (i.e., Carey et al. 2000; Gourley et al. 2007).”
The Need to Represent Raindrop Size Spectra as Normalized Gamma Distributions for the Interpretation of Polarization Radar Observations (2002, background): “5 are the curves proposed by Chandrasekar and Bringi (1988a) and Chandrasekar et al.”
Drop Shapes, Model Comparisons, and Calculations of Polarimetric Radar Parameters in Rain (2007, background): “…equivalent, for example, as can occur along the leading edge of severe convective cells or aloft due to “big drop” zones inferred for example by Ryzhkov and Zrnić (1995) and measured by Schuur et al. (2001) at S band, and inferred by Meischner et al. (1991) and Carey et al. (2000) at C band.”
The Relationship between Precipitation and Lightning in Tropical Island Convection: A C-Band Polarimetric Radar Study (2000, methodology): “Given the relatively small sample volume of disdrometers, the lack of information regarding the distribution of drops (cid:46) 5.4 mm, the C-pol observations of large Z dr (3–5 dB), and videosonde observations of drops up to 8 mm in diameter during MCTEX (Carey et al. 2000), we felt that it was nece”
T-matrix theory of electromagnetic scattering by particles and its applications: a comprehensive reference database (2004, background): “…(1996) Borrmann et al. (2000) Bringi and Seliga (1977a) Bringi and Seliga (1980) Bringi et al. (1998) Brogniez et al. (2003) Brooks et al. (2004) Carey et al. (2000) Chang et al. (2002) Cline et al. (1986) Crosta et al. (2003) Czekala (1998) Czekala and Simmer (1998) Czekala and Simmer (2002)…”
Correction of Radar Reflectivity and Differential Reflectivity for Rain Attenuation at X Band. Part I: Theoretical and Empirical Basis (2005, methodology): “This concept, based on a simple linear relation, has been adapted and modified for correction of attenuation at S and C bands by many researchers (Ryzhkov and Zrnic 1995; Smyth and Illingworth 1998; Carey et al. 2000; Testud et al. 2000; Bringi et al. 2001).”