Descending reflectivity cores in supercell thunderstorms observed by mobile radars and in a high-resolution numerical simulation

Weather and Forecasting

Volumn 24, Issue 1, 2009, Pages 155-186

  Byko, Zack ^a   Markowski, Paul ^a,c   Richardson, Yvette ^a   Wurman, Josh ^b   Adlerman, Edwin ^c  

^a PENNSYLVANIA STATE UNIVERSITY   (United States)

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

^c NONE   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

CLOSE RANGE; DIFFERENT MECHANISMS; DOPPLER RADAR OBSERVATION; FORMATION MECHANISM; HIGH-RESOLUTION NUMERICAL SIMULATION; LOW LEVEL; LOW-LEVEL WINDS; MICROPHYSICS PARAMETERIZATION; MOBILE RADARS; OPERATIONAL FORECASTING; RADAR CHARACTERISTICS; RADAR ECHO; RADIAL VELOCITY; REAR-FLANK; SUPER CELL; SUPERCELL THUNDERSTORMS; THERMODYNAMIC FIELDS; THREE-DIMENSIONAL NUMERICAL SIMULATIONS; TORNADOGENESIS; WIND FIELD;

DOPPLER EFFECT; DOPPLER RADAR; RADAR; ROTATION; THREE DIMENSIONAL; THUNDERSTORMS;

REFLECTION;

CLIMATE MODELING; COMPUTER SIMULATION; DETECTION METHOD; DOPPLER RADAR; FORMATION MECHANISM; NUMERICAL MODEL; OBSERVATIONAL METHOD; PARAMETERIZATION; REFLECTIVITY; SUPERCELL; THERMODYNAMICS; THREE-DIMENSIONAL MODELING; THUNDERSTORM; TORNADO; WEATHER FORECASTING; WIND FIELD;

EID: 66049144960     PISSN: 08828156     EISSN: None     Source Type: Journal    
DOI: 10.1175/2008WAF2222116.1     Document Type: Article

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