6 april 2013, 13:55 uur | Bericht
#392480
Notes severe weather en tornado's
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Max uvv = square root of 2 × CAPE
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BRN (Bulk Richardson Number) = CAPE / (0-6 km) Shear (500MB)
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Showalter (SWI) = used when elevated convection is most likely (cool season)
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EHI = (SR HEL × CAPE) /160,000
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SWEAT = 12(850Td) +20(TT-49) +2(V850) + (V500) +125(sin(dd500-dd850) + 0.2)
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Total Totals = (T850- T500) + (Td850 - T500)= vertical totals plus cross totals
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K index = (T850 -T500) + (Td850 - Tdd700)
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SR Helicity : determines amount of horizontal streamwise vorticity available for storm ingestion
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streamwise = parallel to storm inflow
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Important to look for thermal and dewpoint ridges (THETA-E)
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For tornado, inflow must be greater than 20 knots
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20 to 30% of mesocyclones produce tornadoes
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Tornado types: rope, needle, tube, wedge
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Look for differential advection; warm/ moist at surface, dry air in mid levels
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Severe weather hodograph: veering, strong sfc to 850 directional shear
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>100 J/kg negative buoyancy is significant
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Good match: BRN < 20 and CAPE >2,000 J/kg
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Strong cap when > 2 degrees Celsius
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Study depth of moisture, TT unreasonable when low level moisture is lacking
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KI used for heavy convective rain, values vary with location/season
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Instability enhanced by ... daytime heating, outflow boundaries
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Models generally have weak handle on return flow from Gulf, low level jet, convective rainfall, orography, mesoscale boundaries, and boundary conditions
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Large hail when freezing level >675 mb, high CAPE, supercell
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Synoptic scale uplift from either surface WAA or upper level divergence
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Fair weather cumulus: cumulus humulus, cumulus mediocrus
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T-storm warning when Hail > 3/4", wind > 58 mph, gate to gate shear > 90 knots
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Sounding types: Inverted V, goal post, Type C, wet microburst
Bron: Theweatherprediction
| Gewijzigd: 7 april 2013, 10:28 uur, door Ries
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