The record
Everything the slot carries, as measured. Series arrays are drawn above and listed here in full.
| Event typeevent_type | Excessive Heat |
|---|---|
| NOAA NCEI event IDncei_event_id | 338,679 |
| Episode IDepisode_id | 56,470 |
| Begin UTCbegin_utc | 2011-07-09T20:30:00+00:00 |
| End UTCend_utc | 2011-08-01T05:59:00+00:00 |
| Statestate | OKLAHOMA |
| County/zone typecz_type | Z |
| County/zone namecz_name | MCINTOSH |
| 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 | Official NWS Observations |
| Episode narrativeepisode_narrative | A strong ridge of high pressure in the middle and upper atmosphere redeveloped across the south central United States in mid July resulting in strong subsidence over the region. High temperatures climbed to above 100 degrees on all but two days during the remainder of the month at the Tulsa International Airport and July 2011 went down as the second warmest July on record for that area since records began in 1905. Numerous record temperatures were exceeded this month across eastern Oklahoma. This heat combined with fairly high relative humidity values resulted in afternoon heat index values, or apparent temperatures, in the 105 to 115 degree range. Very little relief was realized during the overnight period as temperatures only fell into the upper 70s to mid 80s. This period of excessive heat continued into August. |
| Yearyear | 2,011 |
Provenance
This slot's source list is not carried on the manifest row; open the dossier below.
Storage: spine