The 29 June 2000 Supercell Observed during STEPS. Part I: Kinematics and Microphysics

By Sarah A. Tessendorf, K. Wiens. 2005

147 citations recorded by the source corpus.

Subfields: Astronomy and Astrophysics, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/73aa393ec61860d72c33c93d305e8a1ee1785b50

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Citations in the corpus

The global lightning-induced nitrogen oxides source (2007, background): “7 shows a lightning discharge observed by the VHF New Mexico Tech Lightning Mapping Array (LMA, see Table 7) (Noble et al., 2004; Thomas et al., 2004; Wiens et al., 2005) during the Severe Thunderstorm Electrification and Precipitation Study (STEPS) (Lang et al.”
Understanding Hail in the Earth System (2020, background): “11 of 49 serves as a conduit for such a pathway (e.g., Tessendorf et al., 2005).”
Aerosol Effects on Intensity of Landfalling Hurricanes as Seen from Simulations with the WRF Model with Spectral Bin Microphysics (2010, background): “An increase in lightning rate indicates invigoration of convection (stronger updrafts with increasingly larger volumes of graupel or small hail/frozen drops aloft) and an increase in the probability of heavier rainfall (e.g., Lhermitte and Krehbiel 1979; Wiens et al. 2005; Fierro et al. 2007).”
A Robust C-Band Hydrometeor Identification Algorithm and Application to a Long-Term Polarimetric Radar Dataset (2013, methodology): “Simulated S-band values were compared with a number of sources (Straka et al. 2000; Tessendorf et al. 2005) and were thus determined to be physically representative of hail, lending confidence to the microphysical parameters used in the simulations.”
Simulated Electrification of a Small Thunderstorm with Two-Moment Bulk Microphysics (2010, methodology): “The conclusions are consistent with observations of IC lightning in a lower dipole (e.g., Qie et al. 2005; Wiens et al. 2005) and the variation of time from initiation to return stroke in 2 CG lighting reported by Coleman et al. (2008).”
An Overview of Lightning Locating Systems: History, Techniques, and Data Uses, With an In-Depth Look at the U.S. NLDN (2009, background): “Severe storms, however, produce much higher rates of cloud lightning than CG flashes, with some storms producing no CG flashes at all [5]–[7].”
Numerically Simulated Electrification and Lightning of the 29 June 2000 STEPS Supercell Storm (2006, background): “During this period, the Doppler-derived maximum updraft speed was near 50 m s (cid:2) 1 (Tessendorf et al. 2005) as the storm intensified, assumed a supercell structure, and increased in size.”
A Theory-Based Hydrometeor Identification Algorithm for X-Band Polarimetric Radars (2009, methodology): “Additionally, the Colorado State University (CSU) Radar Meteorology Group hy-drometeor identiﬁcation algorithm (CSUHID; discussed in Tessendorf et al. 2005) was used as a baseline for comparison with the S-band scattering simulations.”
Theory and Observations of Controls on Lightning Flash Size Spectra (2013, methodology): “Many studies (Wiens et al. 2005; MacGorman et al. 2008) have used thresholds within the range Murphy (2006) indicated was less stable, but found those counts to compare favorably with counts obtained through painstaking manual, interactive analysis.”