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 | 166,321 |
| Episode IDepisode_id | 27,956 |
| Begin UTCbegin_utc | 2009-04-11T21:00:00+00:00 |
| End UTCend_utc | 2009-04-11T21:04:00+00:00 |
| Statestate | NEW MEXICO |
| County/zone typecz_type | C |
| County/zone namecz_name | LEA |
| Latitudelat | 32.950 |
| Longitudelon | -103.434 |
| End latitudeend_lat | 32.950 |
| End longitudeend_lon | -103.434 |
| 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 | Law Enforcement |
| Episode narrativeepisode_narrative | On April 11, 2009, a surface high northeast of the region resulted in easterly upslope flow over most of the CWA. Meanwhile, a mid to upper level low near Southern California approached the area from the west. Although the deepest moisture was confined to the Gulf Coast (due to the previously mentioned surface high) there was enough moisture convergence along a stalled surface boundary and dryline. Most unstable CAPE values along these features of 1000 j/kg and 0-6 km bulk shear magnitudes of 60 kt allowed for severe storms to develop as the dynamics neared the area during the late afternoon and early evening hours. A Severe Thunderstorm Watch was issued from 1520-2300 local. |
| Event narrativeevent_narrative | It is unknown whether or not a tornado actually developed. |
| Yearyear | 2,009 |
Provenance
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Storage: spine