The record
Everything the slot carries, as measured. Series arrays are drawn above and listed here in full.
| Event typeevent_type | Funnel Cloud |
|---|---|
| NOAA NCEI event IDncei_event_id | 167,593 |
| Episode IDepisode_id | 27,957 |
| Begin UTCbegin_utc | 2009-04-17T04:00:00+00:00 |
| End UTCend_utc | 2009-04-17T04:05:00+00:00 |
| Statestate | TEXAS |
| County/zone typecz_type | C |
| County/zone namecz_name | MITCHELL |
| Latitudelat | 32.400 |
| Longitudelon | -100.970 |
| End latitudeend_lat | 32.400 |
| End longitudeend_lon | -100.970 |
| Deaths directdeaths_direct | 0 |
| Deaths indirectdeaths_indirect | 0 |
| Injuries directinjuries_direct | 0 |
| Injuries indirectinjuries_indirect | 0 |
| Damage propertydamage_property | 0.00K |
| Damage cropsdamage_crops | 0.00K |
| Weather forecast office sourcewfo_source | Public |
| Episode narrativeepisode_narrative | A mid to upper level closed low was located over southwest Utah the day of the event. Near the surface, a quasi dryline was located from a line near the mountains of west Texas to the eastern NM/TX border. Dewpoints in the low to mid 50 F range resulted in moderate surface based instability east of the dryline during the early evening hours. The upper dynamics combined with the surface convergence along the dryline led to the development of severe weather as the deep layer shear increased with the approach of the aforementioned feature. There was also a brief window for tornadic storms as low level profiles became increasingly backed east of the dryline as height falls increased ahead of the upper trough just west of the region. A tornado watch was issued from 1642-2400 local. |
| Yearyear | 2,009 |
Provenance
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Storage: spine