Radar and Atmospheric Science: A Collection of Essays in Honor of David Atlas
By R. Wakimoto, R. Srivastava. 2003
145 citations recorded by the source corpus.
Subfields: Atmospheric Science
View Paper: https://www.semanticscholar.org/paper/5189208078d5298cb0063aa6e4180f076e3d5156
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In Atmospheric Science
- Matthew R. Kumjian
- Guifu Zhang
- Alexander Khain
- Edward Brandes
- Qing Cao
- Terry Schuur
- Daniel Rosenfeld
- Alexander V. Ryzhkov
Citations in the corpus
- The Impact of Size Sorting on the Polarimetric Radar Variables (2012, methodology): “In nature, precipitation formation in continental deep convective storms is generally dominated by ice microphysical processes (e.g., Dye et al. 1974; Rosenfeld and Ulbrich 2003, among others).”
- Microphysics of Raindrop Size Spectra: Tropical Continental and Maritime Storms (2007, background): “Such an asymptotic bound is close to those found by a variety of investigators (BC; Bringi et al. 2002; Sauvageot and Lacaux 1995; Rosenfeld and Ulbrich 2003; Uijlenhoet et al. 2003).”
- Polarimetric Radar Estimators Based on a Constrained Gamma Drop Size Distribution Model (2004, methodology): “For a gamma DSD, the parameters N0, m, and D0 can be derived using A and b power-law coefficients as (Rosenfeld and Ulbrich 2003) 1/(12b)b 2.33 A 33.31G1 2[ ] b 2 1 N 5 , (11a)0 2.33b 610 G 1 2b 2 1 7 2 4.67b m 5 , and (11b) b 2 1 3.67 1 m 1/(4.671m)D 5 R mm. (11c)0 1/(4.671m)[33.31N G(4.67 1…”
- Polarimetric Radar Rain Estimation through Retrieval of Drop Size Distribution Using a Bayesian Approach (2010, methodology): “Long-term DSD measurements made in central Oklahoma by the two-dimensional video disdrometer (2DVD) are first used to construct a prior probability density function (PDF) of DSD parameters, which are estimated using truncated gamma fits to the second, fourth, and sixth moments of the distributions.”
- Aerosol impact on the dynamics and microphysics of deep convective clouds (2005, background): “Clouds of similar cloud top heights (i.e. similar cloud top temperatures) will precipitate differently under different aerosol conditions (Rosenfeld and Ulbrich 2003).”
- Simulations of Polarimetric Radar Signatures of a Supercell Storm Using a Two-Moment Bulk Microphysics Scheme (2010, background): “The graupel category originally included in the MY05 package is turned off to maintain consistency with our previous experiments (JXZS08 and JZX08).”