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This is the current revision of this page, as edited by Cewbot (talk | contribs) at 21:25, 18 February 2024 (Maintain {{WPBS}}: 6 WikiProject templates. Keep majority rating "Start" in {{WPBS}}. Remove 5 same ratings as {{WPBS}} in {{WikiProject Environment}}, {{WikiProject Climate change}}, {{WikiProject Biography}}, {{WikiProject United States}}, {{WikiProject Weather}}. Keep 1 different rating in {{WikiProject Isle of Man}}.). The present address (URL) is a permanent link to this version.

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WikiProject class rating

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This article was automatically assessed because at least one article was rated and this bot brought all the other ratings up to at least that level. BetacommandBot 16:28, 27 August 2007 (UTC)[reply]

The Helm Wind isn't a foehn

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I don't think that the Helm Wind can be properly classed as a foehn. The ridge over which the wind flows isn't high enough, and the air (coming from the east) is rarely moist enough, for the uplift to cause substantial precipitation over the high ground, something that's necessary for the foehn effect to occur. I'm not aware of any measurements showing an increase in temperature on the lee side compared to somewhere at a similar height on the upwind side. However if there's a meteorology book or paper that can be cited to say that I'm wrong, then I will of course withdraw my objection. JH (talk page) 19:12, 8 November 2011 (UTC)[reply]

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