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 | 482,670 |
| Episode IDepisode_id | 80,292 |
| Begin UTCbegin_utc | 2013-11-17T19:08:00+00:00 |
| End UTCend_utc | 2013-11-17T19:08:00+00:00 |
| Statestate | ILLINOIS |
| County/zone typecz_type | C |
| County/zone namecz_name | WILLIAMSON |
| Latitudelat | 37.730 |
| Longitudelon | -88.930 |
| End latitudeend_lat | 37.730 |
| End longitudeend_lon | -88.930 |
| 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 | Supercell thunderstorms developed along a pre-frontal low pressure trough over Missouri and then moved east across southern Illinois. Very strong wind fields coupled with moderate amounts of instability resulted in several supercell thunderstorms, some of which produced tornadoes. The storms moved through the warm sector of a low pressure system characterized by mixed-layer capes around 1000 j/kg. Southerly surface winds transported rich low-level moisture north of the Ohio River, with dew points in the mid 60's. Areas of partial sunshine immediately preceding the convection bolstered instability. The low level wind shear was very strong, with 0 to 1 km storm-relative helicity at or above 500. Strong southerly surface winds ahead of the storms gusted to around 45 mph from Mount Vernon to Carbondale during the midday hours. |
| Yearyear | 2,013 |
Provenance
This slot's source list is not carried on the manifest row; open the dossier below.
Storage: spine