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Physical Process

Derecho Formation

Atmospheric and Climatic Processes

Derecho formation is the process by which a fast-moving, bowed line of severe thunderstorms, a bow echo, organizes and sustains itself long enough to drive a widespread, damaging straight-line windstorm along a path at least 400 kilometres long. It is fed by a rear-inflow jet of dry air that plunges to the surface behind the storm line and fans outward, and it is distinguished from an ordinary squall line mainly by its sheer duration and reach, sometimes cutting a swath of hurricane-force wind damage across several U.S. states in a single afternoon and evening. This description is adapted from Wikipedia contributors under CC BY-SA 4.0; changes were made. https://creativecommons.org/licenses/by-sa/4.0/

Facts
Process Type
Atmospheric Circulation 1
Timescale
A single event lasts several hours as it tracks along its path. 1
Timescale
Timescale (category)
Hours 1
Connections

Caused By

Source Derecho Formation (Wikipedia)
Sources
1. Derecho Formation (Wikipedia)
Wikimedia Foundation
  • Lead section
    A derecho (/dəˈɹeɪ.t͡ʃoʊ/ , from Spanish: derecho [deˈɾetʃo], 'straight') is a widespread, long-lived, straight-line wind storm that is associated with a fast-moving complex of severe thunderstorms referred to as a mesoscale convective system.
  • In Category: Physical Processes
  • Caused By: Thunderstorm Formation
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