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 | 422,500 |
| Episode IDepisode_id | 70,343 |
| Begin UTCbegin_utc | 2013-01-12T22:02:00+00:00 |
| End UTCend_utc | 2013-01-12T22:02:00+00:00 |
| Statestate | KENTUCKY |
| County/zone typecz_type | C |
| County/zone namecz_name | UNION |
| Latitudelat | 37.720 |
| Longitudelon | -87.820 |
| End latitudeend_lat | 37.720 |
| End longitudeend_lon | -87.820 |
| 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 | During the afternoon, a supercell thunderstorm developed along a quasi-stationary front that extended from southwest to northeast along the Lower Ohio River Valley. Deep and strong southwesterly wind flow stretched from Texas to the Great Lakes region ahead of an expansive upper-level trough over the western and central states. Several weak disturbances tracked northeastward, contributing to the development of the isolated supercell. Strong low and mid-level wind fields supported the formation of the supercell, which spawned an isolated EF-2 tornado in Livingston County.|Later on during the night, more storms developed in a region of strong warm advection near a low level jet in excess of 50 knots. Marginal instability developed as a surface warm front lifted northward. This round of storms produced heavy rain and some flash flooding. |
| Yearyear | 2,013 |
Provenance
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Storage: spine