Abstract
AbstractPolar lows (PLs) are small‐scale and intense low‐pressure systems that form at high latitudes in both hemispheres. Due to their limited spatial scale and brief lifetimes, weather and climate models are often unable to resolve these systems. One way to overcome this problem is to define a suitable proxy for PLs, with which the likelihood of PL formation can be assessed even in coarse‐resolution datasets. This study draws on previous studies and an empirical database of 63 PLs to quantify the respective influences of low‐level static stability and upper‐level forcing on PL formation, as both of these factors are known to favour PL development. Little redundancy between the two parameters is found. After defining threshold values for the two parameters, climatological properties of favourable conditions for PLs are computed for the North Atlantic, the North‐West Pacific and the Southern Hemisphere. The low‐level static stability, which is strongly modified during marine cold‐air outbreaks, puts important constraints on where PLs can form, while the upper‐level forcing determines whether or not they will form. As a result of the climatologically lower tropopause in the Labrador Sea region, favourable conditions for PLs occur more often there than in the Nordic Seas, which has long been believed to be the main PL region in the Northern Hemisphere (NH). In the Southern Hemisphere, favourable conditions for PLs occur substantially less often than in the NH. The PL index defined here is suitable for other climatological studies and PL forecasting. Copyright © 2011 Royal Meteorological Society
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