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Satellite image of a “Polar Low” observed in the Arctic Sea on 06 04 2007, framed in red. Greenland appears clearly at the top left, covered with clouds.

Understanding Polar Lows Using Satellite Imagery

During winter, small cyclones – typically 200 to 600 km in diameter – develop in subarctic regions over areas free of sea ice. The most intense cyclones are called polar lows. These severe storms usually form when polar air is transported over maritime areas. This cold and dry air destabilises the lowest layers of the atmosphere when it arrives over relatively warm waters, creating a polar low.

Short-term forecasting of polar lows remains challenging, because they develop very rapidly, in areas with very few observations. The understanding of the formation of polar lows has been substantially improved with the advent of satellite observations in the late seventies.

Retreating sea ice exposes new ocean areas to extreme weather systems such as polar lows. Climate change could therefore potentially change where and when polar lows will occur in the future.

During the winter, small-scale cyclones, typically 200 to 600 km, develop on Arctic-free ice seas. The most intense of them are called Polar Lows. These severe low pressure systems usually form along the sea ice along warm ocean currents as a result of intrusions of polar air masses. Indeed, the icy and dry air coming either from the pack ice or from continents covered with ice destabilizes the lower layers of the troposphere when it circulates over the relatively hot open seas.

Considerable advances in knowledge of the structure, physics of polar lows came from satellite observation. But their short-term forecasting is still a challenge. Climate change could also change both regions and times of occurrence.

Why are we interested in the Polar Lows ?

These systems are associated with strong surface winds with very often gusts that can be very violent. The conditions at sea during the passage of a Polar Low can be dangerous with strong waves, brutal snowfall and blizzard.

The Polar Lows, characterized by a rather small spatial and temporal extension, can be triggered extremely rapidly, making them particularly difficult to predict, and dissipate shortly after reaching the ribs.

These extreme weather events represent a real risk to the region’s maritime and coastal activities, including shipping, fishing and offshore oil and gas platforms.

POLAR LOWS