The pretornadic phase of the Goshen County, Wyoming, supercell of 5 June 2009 intercepted by VORTEX2. Part I: Evolution of kinematic and surface thermodynamic fields

Monthly Weather Review

Volumn 140, Issue 9, 2012, Pages 2887-2915

  Markowski, Paul ^a   Richardson, Yvette ^a   Marquis, James ^a   Wurman, Joshua ^b   Kosiba, Karen ^b   Robinson, Paul ^b   Dowell, David ^c   Rasmussen, Erik ^d   Davies Jones, Robert ^e  

^a PENNSYLVANIA STATE UNIVERSITY   (United States)

^b Center for Severe Weather Research Colorado   (United States)

^c NOAA EARTH SYSTEM RESEARCH LABORATORY   (United States)

^d Rasmussen Systems   (United States)

^e NATIONAL SEVERE STORMS LABORATORY   (United States)

Author keywords

Convective storms; Tornadogenesis

Indexed keywords

CONVECTIVE STORMS; COUNTER-ROTATING VORTICES; ECHO REGIONS; POTENTIAL TEMPERATURE; PRESSURE GRADIENT FORCE; RADAR DATA; REAR-FLANK; SUPER CELL; SURFACE THERMODYNAMICS; TORNADOGENESIS; VERTICAL VORTICITY; VORTEX LINES; WEATHER SURVEILLANCE RADAR-1988 DOPPLER; WYOMING;

STORMS; VORTICITY;

VORTEX FLOW;

CONVECTIVE SYSTEM; DOPPLER RADAR; OUTFLOW; PRESSURE GRADIENT; STORM; SUPERCELL; THERMODYNAMICS; TORNADO; VORTEX FLOW; VORTICITY;

GOSHEN COUNTY; UNITED STATES; WYOMING;

EID: 84867946528     PISSN: 00270644     EISSN: 15200493     Source Type: Journal    
DOI: 10.1175/MWR-D-11-00336.1     Document Type: Article

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