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forced channeling

Scope: climate
Papers: 1 | Mentions: 1

Local Knowledge Graph (37 entities)

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Definition

Mechanism where upper-level flow is channeled by valley sidewalls when convective boundary layer grows above ridge height, causing valley wind direction to align with upper-level flow

Publications (1)

article

The short life of upvalley wind in a high-altitude valley in the Colorado Rocky Mountains

2025Journal of Geophysical Research: Atmospherescentral

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