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 | 541,955 |
| Episode IDepisode_id | 90,232 |
| Begin UTCbegin_utc | 2014-10-13T22:54:00+00:00 |
| End UTCend_utc | 2014-10-13T22:54:00+00:00 |
| Statestate | INDIANA |
| County/zone typecz_type | C |
| County/zone namecz_name | VANDERBURGH |
| Latitudelat | 37.966 |
| Longitudelon | -87.579 |
| End latitudeend_lat | 37.966 |
| End longitudeend_lon | -87.579 |
| 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 | A broken squall line oriented from north to south moved slowly eastward across southwest Indiana. Individual storm cells within the line raced north-northeast at 50 to 65 mph. Storm development was fostered by modest solar heating as surface dew points climbed into the mid and upper 60's. Low level confluence ahead of a slow-moving surface low over southern Missouri aided the intensification of the squall line. Strengthening wind fields associated with an upper level trough approaching from the southern Plains contributed to isolated tornadoes with the longer-lived storms. Strong low-level winds, around 50 knots at 1 kilometer above the ground, enhanced the risk of mesovortices and isolated tornadoes within the squall line despite a dearth of instability. |
| Event narrativeevent_narrative | A funnel cloud was reported over the Ohio River. |
| Yearyear | 2,014 |
Provenance
This slot's source list is not carried on the manifest row; open the dossier below.
Storage: spine