The record
Everything the slot carries, as measured. Series arrays are drawn above and listed here in full.
| Event typeevent_type | Heavy Rain |
|---|---|
| NOAA NCEI event IDncei_event_id | 407,234 |
| Episode IDepisode_id | 67,874 |
| Begin UTCbegin_utc | 2012-09-08T00:20:00+00:00 |
| End UTCend_utc | 2012-09-08T00:50:00+00:00 |
| Statestate | ILLINOIS |
| County/zone typecz_type | C |
| County/zone namecz_name | PERRY |
| Latitudelat | 38.152 |
| Longitudelon | -89.380 |
| End latitudeend_lat | 38.152 |
| End longitudeend_lon | -89.380 |
| 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 | Trained Spotter |
| Episode narrativeepisode_narrative | Damaging winds were the primary type of severe weather as an extensive squall line crossed southern Illinois. Thunderstorms were organized into bowing line segments that produced damaging winds as they moved rapidly east at 50 to 60 mph. The storms occurred along and ahead of a cold front that trailed south from a low pressure center near St. Louis. Isolated severe thunderstorm cells developed ahead of the quasi-linear convective system. Moderate instability existed ahead of the line of storms, with capes from 1500 to 2500 j/kg. Wind shear remained more than adequate for organization of the storms, with winds veering vertically in the lowest 3 km. |
| Event narrativeevent_narrative | One inch of rain was measured in 30 minutes. |
| Yearyear | 2,012 |
Provenance
This slot's source list is not carried on the manifest row; open the dossier below.
Storage: spine