Case Study of a Tornado in China with Large Eddy Simulation

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Case Study of a Tornado in China with Large Eddy Simulation Dan Yao Zhiyong Meng Peking University Summer 2015 Meeting of Fuqing’s Group Penn State University 17th August 2015, State College, PA

Accumulated Precipitation (mm) 21 July 2012 Beijing Tornado Accumulated Precipitation (mm) Beijing Narrow damage swath & Surface convergence 460 Damage Survey (Meng and Yao 2014, Weather and Forecasting)

Storm & Tornado by CM1 Tornadogenesis Re-intensification Maturity updraft cold pool cloud vorticity Maturity Demise t+15’ t+20’ cloud: 0.1 g/kg cloud water mixing ratio updraft: 15 m s-1 vertical velocity cold pool: -1 K potential temperature perturbation vorticity: 0.1 & 0.15 s-1

Vorticity Development 15 m s-1 0.1 s-1 10 m s-1 0.05 s-1 Vertical Velocity Vertical Vorticity top-down 1. Weaker rotation developed top-down 2. Rotation intensified touching the ground 3. Stronger rotation grew bottom-up bottom-up intensified

Vorticity Replacement #1 & Tornadogenesis #2 & Re-intensification #3 & Tornado Demise Low-level downdraft occluded into the lower part of the tornado, though the midlevel updraft was intensified, not weakened. (Yao and Meng 2015, in preparation)

vorticity replacement vorticity replacement Mechanisms at a Glance Tornadogenesis Maintenance Tornado Demise Suction Suction Suction Top-down Occlusion Downdraft Bottom-up #1 #1 #2 #2 #3 Intensified when touching the ground Successful vorticity replacement Unsuccessful vorticity replacement

DRC Captured by CM1 DRC: descending reflectivity core 3D Isosurfaces of Reflectivity Observed Simulated DRC: descending reflectivity core Not the funnel cloud. Mechanisms unclear.

DRC & Tornadogenesis Next-step interests: Impact of DRC on the intensification of near-surface rotation.

Skeleton of My PhD Thesis Part I: Observational Facts (Finished) Damage survey Radar analysis Sounding analysis Part II: Simulated Features (Finished) From genesis to maintenance & demise in comparison to observations Development of vertical vorticity w.r.t. tornadogenesis Replacement of near-surface vorticity w.r.t. maintenance & demise Part III: Dynamical Analyses (To be finished here) Impact of the DRC on the intensification of near-surface rotation Formation mechanism of the DRC in the Beijing tornado (Collaborate with Profs. Paul Markowski & Yvette Richardson)