Eventdex · Funnel Cloud

AVON POINT TO WILLOWICK OH BEYOND 5NM OFFSHORE TO US/CANADIAN BORDER

1042240 · 41.797, -82.030

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The record

Everything the slot carries, as measured. Series arrays are drawn above and listed here in full.

Event typeevent_type	Waterspout
NOAA NCEI event IDncei_event_id	1,042,240
Episode IDepisode_id	171,691
Begin UTCbegin_utc	2022-08-17T10:18:00+00:00
End UTCend_utc	2022-08-17T10:18:00+00:00
Statestate	LAKE ERIE
County/zone typecz_type	Z
County/zone namecz_name	AVON POINT TO WILLOWICK OH BEYOND 5NM OFFSHORE TO US/CANADIAN BORDER
Latitudelat	41.797
Longitudelon	-82.030
End latitudeend_lat	41.797
End longitudeend_lon	-82.030
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	Social Media
Episode narrativeepisode_narrative	A weak lake-induced surface trough over Lake Erie was accompanied by a land breeze convergence zone in vicinity of the lake's major axis. Ascent accompanying the low-level convergence zone amidst large lake-induced CAPE led to the development of a broken line of lake-effect showers and thunderstorms. Low-level horizontal wind shear along the land breeze convergence zone generated surface-based vertical vorticity. One of the storm's updrafts ingested this surface-based vertical vorticity, stretched it to tornado-strength via low-level convergence at the updraft's base, and then the tornado-strength vertical vorticity was advected upward in the updraft, resulting in waterspout formation.
Event narrativeevent_narrative	Received a Twitter photo from a storm chaser in Erieau, Ontario showing a waterspout with a complete condensation funnel accompanying a lake-effect thunderstorm. This waterspout occurred about 24-nautical miles north of Avon Point.
Yearyear	2,022

Provenance

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Storage: spine