Investigation of the impact of Microphysics Options on Idealized WRF Supercell

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INVESTIGATION OF THE IMPACT OF MICROPHYSICS OPTIONS ON IDEALIZED WRF SUPERCELL Catrin M. Mills Sara T. Strey-Mellema

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Investigation of the impact of Microphysics Options on Idealized WRF Supercell. Catrin M. Mills Sara T. Strey- Mellema. Microphysics. Kessler: Warm rain – no ice Idealized microphysics (read- simple) Time-split rainfall Thompson: Replacement of Thompson et al. (2007) - PowerPoint PPT Presentation

Transcript of Investigation of the impact of Microphysics Options on Idealized WRF Supercell

Page 1: Investigation of the impact of Microphysics Options on Idealized WRF  Supercell

INVESTIGATION OF THE IMPACT OF MICROPHYSICS OPTIONS ON IDEALIZED WRF SUPERCELLCatrin M. MillsSara T. Strey-Mellema

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MICROPHYSICS Kessler:

Warm rain – no ice Idealized microphysics (read- simple) Time-split rainfall

Thompson: Replacement of Thompson et al. (2007) 6-class microphysics with graupel with ice and rain number

concentrations (rather than idealized) predicted (double-moment ice) Time-split fall terms

Millbrandt: New in Version 3.2 7-class microphysics with separate graupel and hail Number concentrations predicted for all six species water/ice species (double-moment) – 12 Time-split fall terms

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HYPOTHESIS The microphysics scheme that best

represents ice particles will have the strongest updrafts and strongest mesocyclone

Model studies have shown that simulating ice effects storm dynamics, such that vertical vorticity is enhanced throughout the storm

We expect that the more sophisticated schemes are necessary in generating cold pools that can generate horizontal vorticity and downdrafts that can tilt it into the vertical

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ADVECTION TERM: THOMPSON VS. KESSLER

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DIVERGENCE TERM: THOMPSON VS. KESSLER

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TILTING TERM: THOMPSON VS. KESSLER

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ADVECTION TERM: THOMPSON VS. KESSLER

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W- WIND

kessler thompson millbrandt