Refined Supercell and Tornado Forecast Parameters

By E. Rasmussen. 2003

264 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/f25e0a0ce8efea377491aa1b233cc4caa3b50afe

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. P. Groenemeijer
2. R. Davies-Jones
3. R. edwards
4. Richard L. Thompson
5. P. Markowski
6. T. Kühne
7. Lon Curtis
8. J. Hart

In Global and Planetary Change

1. P. Groenemeijer
2. R. edwards
3. Richard L. Thompson
4. R. Davies-Jones
5. T. Kühne
6. Lon Curtis
7. J. Hart
8. P. Markowski

Citations in the corpus

• A Climatology of Tornadoes in Europe: Results from the European Severe Weather Database (2014, background): “…wind shear in the lowest 1–2 km above ground level with significant tornadoes was first documented in peer-reviewed literature (Thompson et al. 2003; Rasmussen 2003; Craven and Brooks 2004) using Storm Data, after being hypothesized almost 80 years earlier by Van Everdingen (1925) when studying a…”
• Close Proximity Soundings within Supercell Environments Obtained from the Rapid Update Cycle (2003, methodology): “In agreement with Rasmussen (2003), 0–1-km EHI (using MLCAPE, the MLEHI) values were offset by about 1.5 quartiles between nontornadic and significantly tornadic supercells when applied to the RUC-2 close proximity soundings (Fig.”
• Midlevel Dry Intrusions as a Factor in Tornado Outbreaks Associated with Landfalling Tropical Cyclones from the Atlantic and Gulf of Mexico (2004, result): “A denser network of observation sites coupled with more frequent sonde 10 The findings are also consistent with updated findings reported by Rasmussen (2003). releases (both dropwindsonde and rawinsonde) would be an important step for both research and operational purposes.”
• An Efficient and Accurate Method for Computing the Wet-Bulb Temperature along Pseudoadiabats (2008, background): “…index, the height to which penetrative convection can reach, etc.] that identify environments that support various types of severe weather (e.g., Rasmussen 2003; Thompson et al. 2003) and that may factor in the forecast likelihood that a thunderstorm will produce a significant tornado…”
• Estimations of CIN and LFC Associated with Tornadic and Nontornadic Supercells (2004, unknown): “This revised EHI formulation (Rasmussen 2003), combining total MLCAPE and 0–1-km storm-Unauthenticated (1) It may be notable that mean 0–1-km MLEHI values in Fig.”