A few selected METARs:
Detroit, MI: KDTW 211353Z 20027G41KT 3SM +TSRA SQ OVC035CB 23/18 A2994 RMK AO2 LTG DSNT SW-N RAB49 TSB52 SLP133 OCNL LTGIC ALQDS AND OHD TS ALQDS AND OHD MOV NE T02330183 PNO $
Kitchener, ON: CYKF 211623Z AUTO 28032G71KT 220V290 3/4SM +TSRA BR SQ SCT022 BKN036 BKN046 OVC086 18/17 A3000 RMK LTNG DIST ALQDS PRESRR SLP161 DENSITY ALT 1500FT
Ottawa, ON: CYOW 211952Z 28038G65KT 1/4SM R07/P6000FT/U R32/4000VP6000FT/D +TSRA OVC050CB 20/17 A2992 RMK RA5CB3 NOTE WIND SPEED PRESRR SLP135 DENSITY ALT 1100FT
Quebec, QC: CYQB 212305Z 25036G54KT 210V290 3/4SM R06/1800V2200FT/N +TSRA OVC013CB 21/19 A2985 RMK CB8 PRESRR SLP110 DENSITY ALT 1200FT
It appears to be a serial derecho whose winds were greatly aided by strong winds aloft. Derechos are not so uncommon in southern Ontario, but are quite rare in Quebec. Quebec probably has not had a derecho since July 4-5, 1999 (which was one of the farthest north progressive derechos recorded).
| Source: SPC |
With strong instability meeting up with a quasi-stationary front and WSW flow at mid-levels parallel to the front, the environment was at least somewhat conducive for derechos, based on Johns and Hirt (1987). A lack of height falls or a true mid-level dry intrusion as well as the mid-level flow being slightly more backed than with most derechos were possible negative factors though.
| Source: SPC |
Derechos are almost never easy to predict, especially given their rarity in this area, and this one was no exception. Even the 12z HRRR and NAM 3-km (convectively-allowing models) from that morning failed to show anything severe:
| Source: weather.us |
Reality is shown below:
| Source: weather.us |
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