Bill Schintler
EF4
Target:
Mott, ND (60 miles WSW of Bismarck).
Timing:
Storm initiation 7 PM CDT.
Storm mode:
Multicell-storms which should remain below severe limits.
Discussion:
00Z analysis indicated deepening trough over the NWRN CONUS with several of pieces of energy embedded within it. A lead S/WV was translating through ERN MT with an area of convection associated with it, while a second feature was over ID. Return flow was established from TX through SD as a 20kt LLJ was transporting 8C H85 dewpoints towards the SD/ND border. A strong baroclinic zone extended along an OGA, FSD, to LSE line in NEB and MN with a shallow cool layer to its north. Up-wind soundings (SLC, RIW, and LKN) showed nearly dry-adiabatic lapse rates in the SFC-500mb layer, and differential advection of mid-level lapse rates of 8-8.5C/km on top of moisture from the south should result in modest MLCAPE’s of 1500J/kg by late afternoon tomorrow.
Sunday, the area should remain capped to SFC-based convection until late in the day as one or more outflow boundaries from a morning MCS over ND focuses the northward moving synoptic boundary and a compact vort max provides the necessary lift to overcome warm mid-levels. Moderate instability along with weak deep layer shear AOB 25 kts should result in primarily multicell storms. Overnight, the convection should grow into a large MCS and travel E through ND while producing heavy rain as a 40kt LLJ noses into the region.
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Mott, ND (60 miles WSW of Bismarck).
Timing:
Storm initiation 7 PM CDT.
Storm mode:
Multicell-storms which should remain below severe limits.
Discussion:
00Z analysis indicated deepening trough over the NWRN CONUS with several of pieces of energy embedded within it. A lead S/WV was translating through ERN MT with an area of convection associated with it, while a second feature was over ID. Return flow was established from TX through SD as a 20kt LLJ was transporting 8C H85 dewpoints towards the SD/ND border. A strong baroclinic zone extended along an OGA, FSD, to LSE line in NEB and MN with a shallow cool layer to its north. Up-wind soundings (SLC, RIW, and LKN) showed nearly dry-adiabatic lapse rates in the SFC-500mb layer, and differential advection of mid-level lapse rates of 8-8.5C/km on top of moisture from the south should result in modest MLCAPE’s of 1500J/kg by late afternoon tomorrow.
Sunday, the area should remain capped to SFC-based convection until late in the day as one or more outflow boundaries from a morning MCS over ND focuses the northward moving synoptic boundary and a compact vort max provides the necessary lift to overcome warm mid-levels. Moderate instability along with weak deep layer shear AOB 25 kts should result in primarily multicell storms. Overnight, the convection should grow into a large MCS and travel E through ND while producing heavy rain as a 40kt LLJ noses into the region.
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