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 | 646,327 |
| Episode IDepisode_id | 106,773 |
| Begin UTCbegin_utc | 2016-07-07T05:00:00+00:00 |
| End UTCend_utc | 2016-07-07T12:00:00+00:00 |
| Statestate | NEBRASKA |
| County/zone typecz_type | C |
| County/zone namecz_name | YORK |
| Latitudelat | 40.860 |
| Longitudelon | -97.594 |
| End latitudeend_lat | 40.860 |
| End longitudeend_lon | -97.594 |
| 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 | Mesonet |
| Episode narrativeepisode_narrative | Pockets of wind damage and/or strong winds occurred with bowing convective line segments on this Wednesday night. Isolated supercells developed over western Nebraska late in the afternoon, with multiple tornadoes, spotty wind damage, and large hail occurring. During the evening hours, cell coverage increased leading to multiple cell mergers. By 9 p.m. CST, this resulted in several lines segments that stretched from Yankton, SD to Broken Bow to McCook. Two small bow echoes tracked through south central Nebraska, from Interstate 80 south to the state line, and another across central Nebraska which affected Valley and Greeley Counties. After 11 p.m. CST, the outflow from extensive thunderstorms over northeast Nebraska sagged to Interstate 80, from York west to Grand Island where it intersected the comma head of the bow echo moving across southern Nebraska. An east-west oriented line of storms developed along Interstate 80. Cell training between 11:30 p.m. and 1 a.m. CST resulted in a swath of 2 to 3 inches of rain from eastern Hamilton County across central York County. The highest rainfall amount was 3.08 inches just east of the city of York. These bow echoes produced multiple measured gusts between 50 and 62 mph. Snapped tree limbs and blown over trees were most extensive in the city of Hastings and the towns of Greeley and Spalding.||A very weak cold front sagged into Nebraska the previous night and was located roughly along the southern state line at daybreak. As the day progressed, the front gradually lifted north as a warm front as low pressure over Wyoming deepened to 1000 mb. In the upper levels, the flow was zonal with the Westerlies confined to the northern third of the United States. A subtropical high was over Texas. 500 mb observations suggest there was a weak/subtle shortwave trough moving across the Central Plains, possibly aiding thunderstorm development. Just prior to thunderstorms moving into south central Nebraska, temperatures were in the middle 70s to lower 80s, and dewpoints ranged from the lower 60s west to the upper 60s east. Yet, mid-level lapse rates were very steep (8 degrees C/km), resulting in MLCAPE between 2000 and 4000 J/kg. Effective deep layer shear was around 50 kts. |
| Event narrativeevent_narrative | A total of 3.04 inches was measured since midnight. |
| Yearyear | 2,016 |
Provenance
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