Continental polar air, commonly denoted as cP, forms over
chilly surfaces and may be very stable with little moisture whereas maritime polar air commonly denoted as
mP, forms over hotter water and is unstable with excessive moisture content.
Maritime polar air results in fog, drizzles and lengthy intervals
of gentle or reasonable rain because of the quantity of moisture it
carries. Current forecasts reveal that Glasgow weather in October
will expertise polar air in the latter half of the month in all probability bringing alongside winter showers attempting to reach up to
Edinburgh. The mountains standing in the way in which of this air expertise considerable snow and rain on their windward side
whereas the opposite facet sees the air finally grow to
be chilly fronts. The instability of the maritime
polar air varieties convections which lead to formations
of clouds causing frequent precipitation. It's a stable air mass that varieties over high latitudes and typically has low dew points
and temperatures. The imbalance between the temperatures on land during spring
and summer season and the newly hushing air gets corrected in autumn.

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