Karif: Difference between revisions

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|Meaning=(Also spelled kharif.) A strong southwest [[wind]] on the southern shore of the Gulf of Aden,  especially at Berbera, Somaliland, during the [[southwest monsoon]].
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|Explanation=It sets in at about 10 [[File:ams2001glos-Kex01.gif|link=|ams2001glos-Kex01]] [[local time]] and continues until about noon on the following day,  reaching its greatest strength, averaging 11 m s<sup>-1</sup> (25 mph) in July and August, about 8 [[File:ams2001glos-Kex02.gif|link=|ams2001glos-Kex02]] It  resembles a [[land breeze]], but on a much larger [[scale]] than the [[normal]] land breeze, owing to the  rugged [[topography]] and consequent great depth of the layer of cooled air.
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== karif ==
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<div class="definition"><div class="short_definition">(Also spelled kharif.) A strong southwest [[wind]] on the southern shore of the Gulf of Aden,  especially at Berbera, Somaliland, during the [[southwest monsoon]].</div><br/> <div class="paragraph">It sets in at about 10 <div class="inline-formula">[[File:ams2001glos-Kex01.gif|link=|ams2001glos-Kex01]]</div> [[local time]] and continues until about noon on the following day,  reaching its greatest strength, averaging 11 m s<sup>-1</sup> (25 mph) in July and August, about 8 <div class="inline-formula">[[File:ams2001glos-Kex02.gif|link=|ams2001glos-Kex02]]</div> It  resembles a [[land breeze]], but on a much larger [[scale]] than the [[normal]] land breeze, owing to the  rugged [[topography]] and consequent great depth of the layer of cooled air.</div><br/> </div>
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Latest revision as of 12:00, 26 March 2024

(Also spelled kharif.) A strong southwest wind on the southern shore of the Gulf of Aden, especially at Berbera, Somaliland, during the southwest monsoon.

It sets in at about 10 ams2001glos-Kex01 local time and continues until about noon on the following day, reaching its greatest strength, averaging 11 m s-1 (25 mph) in July and August, about 8 ams2001glos-Kex02 It resembles a land breeze, but on a much larger scale than the normal land breeze, owing to the rugged topography and consequent great depth of the layer of cooled air.

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