Alberta low: Difference between revisions

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|Display title=Alberta low
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|Meaning=A [[low]] that originates centered on the eastern slope of the Canadian Rockies in the  province of Alberta, Canada.
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|Explanation=Formerly, it was thought that such lows actually originated (more or less independently) over  this location. It is now recognized that depressions moving inland from the Pacific are the actual  parent systems. Alberta lows appear as these systems enhance, or are enhanced by, the [[dynamic trough|dynamic  trough]] that is a typical, almost semipermanent, feature of this region. <br/>''See'' [[Colorado low]], [[Alberta clipper|Alberta  clipper]].
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== Alberta low ==
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<div class="definition"><div class="short_definition">A [[low]] that originates centered on the eastern slope of the Canadian Rockies in the  province of Alberta, Canada.</div><br/> <div class="paragraph">Formerly, it was thought that such lows actually originated (more or less independently) over  this location. It is now recognized that depressions moving inland from the Pacific are the actual  parent systems. Alberta lows appear as these systems enhance, or are enhanced by, the [[dynamic trough|dynamic  trough]] that is a typical, almost semipermanent, feature of this region. <br/>''See'' [[Colorado low]], [[Alberta clipper|Alberta  clipper]].</div><br/> </div>
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Latest revision as of 21:15, 13 January 2024

A low that originates centered on the eastern slope of the Canadian Rockies in the province of Alberta, Canada.

Formerly, it was thought that such lows actually originated (more or less independently) over this location. It is now recognized that depressions moving inland from the Pacific are the actual parent systems. Alberta lows appear as these systems enhance, or are enhanced by, the dynamic trough that is a typical, almost semipermanent, feature of this region.
See Colorado low, Alberta clipper.


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