2019-2020 Polar Cyclones Season

The 2017-18 Arctic cyclone season was an 11.

Polar Storm Angel
The BNWC began monitoring the southeastern Labrador Sea for possible polar or subpolar development on September 29. At 00:00 UTC on October 4, the disturbance developed into a subpolar depression, the first of the season, 11 days before the season officially began. The depression moved slowly northwestward, transitioning into a fully polar cyclone by 18:00 UTC that same day. The polar depression failed to strengthen as its forward speed increased the next day, and at 12:00 UTC on October 6, the depression degenerated into a polar wave. The polar wave became better organized on October 7 as winds increased to polar storm force, although the remnants did not have a well-defined circulation at that time. The polar wave's circulation became better defined the next day, and it is estimated that the wave developed into Polar Storm Angel at 00:00 UTC on October 9. However, operationally, BNWC restarted advisories on Polar Depression One at 03:00 UTC on October 9, while it was located over the Davis Strait. It was operationally named six hours later. Angel strengthened slightly, peaking with maximum sustained winds of 50 mph and a minimum pressure of 1003 mbar by 18:00 UTC on October 9. Angel then began to weaken shortly thereafter, and made landfall in Baffin Island as a polar storm with maximum sustained winds of 40 mph and a minimum pressure of 1006 mbar. After landfall, Angel began to weaken, becoming a polar depression by 00:00 UTC on October 11. Angel dissipated over Baffin Island at 12:00 UTC that same day.

Polar Storm Bell
A broad area of low pressure over the southwestern Hudson Bay acquired sufficient organization to be classified as Polar Storm Bell at 15:00 UTC on October 14. Bell began to strengthen shortly after formation, eventually strengthening to peak intensity just under polar cyclone strength with maximum sustained winds of 70 mph and a minimum pressure of 989 mb at 03:00 UTC on October 16. Bell weakened slightly before making landfall in the Nunavut Province of Canada around 11:30 UTC on October 16, with maximum sustained winds of 65 mph and a minimum pressure of 994 mb. Bell then began to rapidly weaken later that day as it moved north-northwestward inland. Bell degenerated into a remnant low at 03:00 UTC on October 17.

Weak Polar Cyclone Candle
A polar wave developed into Polar Depression Three at 15:00 UTC on October 31, located over the Southern Baffin Bay. Twelve hours later, the depression strengthened into Polar Storm Candle. Candle gradually became better organized the next day, nearing polar cyclone strength by 21:00 UTC on November 1. At 03:00 UTC on November 2, Candle strengthened into a weak polar cyclone, becoming the first polar cyclone of the season. Candle made landfall at 23:55 UTC that day, east of Savissivik, Greenland, as a weak polar cyclone with maximum sustained winds of 80 mph. Candle then weakened to a polar storm by 03:00 UTC on November 3. Candle further weakened to a polar depression by 21:00 UTC that day, degenerating into a remnant low by 03:00 UTC on November 4.

Moderate Polar Cyclone Donner
On November 7, the BNWC began to monitor a slow-moving polar wave over the Eastern Labrador Sea for possible development. The system quickly organized, becoming a polar depression by 22:30 UTC on November 9. At 03:00 UTC on November 10, the depression strengthened into a Polar Storm and was assigned the name Donner. Donner began quickly intensifying that same day, becoming a Weak Polar Cyclone by 03:00 UTC on November 11 and a Moderate Polar Cyclone 12 hours later. Donner then began to slowly weaken early the next day as it moved into a less favorable environment, transitioning into a post-polar cyclone by 09:00 UTC on November 13.

Severe Polar Cyclone Eggnog
A broad area of low pressure developed over the Southern Hudson Bay in mid-November eventually organized into Polar Storm Eggnog by 03:00 UTC on November 15. Eggnog struggled to strengthen after formation due to marginally favorable conditions and the broad nature of the system, unexpectedly weakening to a polar depression by 21:00 UTC that same day. Eggnog regained polar storm intensity by 03:00 UTC on November 17, and began to strengthen. Eggnog rapidly intensified into a Weak Polar Cyclone by 03:00 UTC on November 18, with maximum sustained winds of 75 mph and a minimum pressure of 983 mb. Eggnog subsequently made landfall in Southampton Island at this intensity, and weakened to a polar storm later that same day. Eggnog's intensity fluctuated for the next couple days before it began to strengthen once again on November 21, rapidly intensifying into a Moderate Polar Cyclone by 03:00 UTC on November 22. Rapid intensification continued and Eggnog became a Severe Polar Cyclone by 15:00 UTC that same day, making it the first major polar cyclone of the season. Eggnog eventually made landfall in Northwestern Greenland at 21:00 UTC on November 23 as a Severe Polar Cyclone. Steady weakening followed, and Eggnog became a remnant low by 03:00 UTC on November 25.

Polar Storm Fir
A small area of low pressure developed into Polar Storm Fir at 15:00 UTC on November 16, while located over the open Northern Atlantic. Struggling with very dry air and moderate wind shear, Fir was not able to strengthen at all, eventually weakening to a polar depression by 15:00 UTC the next day and becoming a remnant low six hours later.

Intense Polar Cyclone Gingerbread
A polar wave organized into Polar Depression Seven by 21:00 UTC on November 21 over the Labrador Sea. 18 hours later, it strengthened into Polar Storm Gingerbread. Gingerbread became a Weak Polar Cyclone by 15:00 UTC on November 23, and an Intense Polar Cyclone by 15:00 UTC on November 24, making it the second major polar cyclone of the season. Gingerbread peaked at this time with maximum sustained winds of 120 mph and a minimum pressure of 966 mbar. Gingerbread then steadily weakened, making landfall around 19:00 UTC on November 25 near Nuuk, Greenland as a Weak Polar Cyclone with maximum sustained winds of 85 mph and a minimum pressure of 974 mbar. Gingerbread rapidly weakened after landfall and dissipated by 21:00 UTC on November 26.

Weak Polar Cyclone Holly
The remnants of Polar Vortex Francine from the Alaskan basin degenerated into a remnant low on November 25. They emerged into the Hudson Bay early on November 27, and redeveloped into the eighth polar depression of the season by 15:00 UTC the next day. The depression was upgraded to Polar Storm Holly at 22:25 UTC based on radar data. Holly then unexpectedly rapidly intensified, becoming a Weak Polar Cyclone by 12:30 UTC the next day. Holly then intensified to its peak intensity with maximum sustained winds of 85 mph and a minimum pressure of 985 mbar by 15:00 UTC that same day. However, Holly began to turn to the south and weaken, falling below Polar Cyclone Status by 15:00 UTC on November 30. Holly continued to weaken, and made landfall in Polar Bear Provincial Park at 03:00 UTC on December 1 with maximum sustained winds of 45 mph. Holly rapidly weakened and dissipated 12 hours later.

Catastrophic Polar Cyclone Icicle
A polar wave developed into Polar Storm Icicle at 15:00 UTC on December 1 over the Labrador Sea. Icicle rapidly intensified into a Weak Polar Cyclone by 09:00 UTC on December 2, an Intense Polar Cyclone by 21:00 UTC, and a Severe Polar Cyclone by 03:00 UTC the next day. Icicle fluctuated in intensity for the next couple of days, before strengthening into a Catastrophic Polar Cyclone by 21:00 UTC on December 5.

Subpolar Storm Jolly
A non-polar area of low pressure rapidly developed in Subpolar Storm Jolly at 17:00 UTC on December 5.

Moderate Polar Cyclone Lantern
Polar Storm Lantern formed at 15:00 UTC on December 11 over the Hudson Bay.

Names Used
This season will use the same Christmas-themed naming list as the 2015-16 Arctic Cyclone Season, with the exception of North, which replaced the retired name Noel.

One storm, Thomas, crossed over from the Alaskan basin and retained its name.

Season effects
This is a table of all the cyclones that have formed in the 2017-18 Arctic cyclone season. Damage figures are denoted in millions of United States Dollars (USD). Death and damage totals also include totals when the cyclone was post-polar, a low, or a polar wave.

[[Category:Arctic cyclones]