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 | 588,639 |
| Episode IDepisode_id | 97,901 |
| Begin UTCbegin_utc | 2015-07-07T10:00:00+00:00 |
| End UTCend_utc | 2015-07-07T12:30:00+00:00 |
| Statestate | KENTUCKY |
| County/zone typecz_type | C |
| County/zone namecz_name | CRITTENDEN |
| Latitudelat | 37.410 |
| Longitudelon | -88.038 |
| End latitudeend_lat | 37.410 |
| End longitudeend_lon | -88.038 |
| 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 | Fire Department/Rescue |
| Episode narrativeepisode_narrative | An early morning thunderstorm complex rapidly developed over the Lower Ohio Valley ahead of a weak mid-level shortwave trough. The complex evolved into a broad zone of convection along and south of a stationary front that extended from central Missouri through central Illinois. Three-hour rainfall amounts were from one to three inches, with isolated higher rates. The convection was focused along the nose of a low-level jet in a very moist air mass, with precipitable water values in the 2 to 2.25 inch range. Unidirectional wind flow from the surface to 500 mb resulted in little net movement of the convection. Although the best instability resided further south in the warm/moist sector, there was enough buoyancy in place to maintain convection. The front settled southward across western Kentucky by late afternoon, providing a focus for renewed convective complexes. |
| Event narrativeevent_narrative | Creeks and streams rose past bankfull. |
| Yearyear | 2,015 |
Provenance
This slot's source list is not carried on the manifest row; open the dossier below.
Storage: spine