Weather maps have been scrutinized in order to document polar lows over the sea surrounding Norway. The study emphasizes the period 1978-1982, and 33 cases of gale-producing polar lows have been identified. The results are presented in frequency tables and one case study is shown. The polar lows were most frequent in December and January. In February. there were only two cases. The lows were observed in weather situations with wind from NE, N or NW in the Norwegian Sea. and/or the Barents Sea. and with synoptic scale cyclones somewhere between Iceland and Novaya Zemlya. Half of the tracks crossed the area between Bear Island and the coast of North Norway. The propagation speed was usually between 8 and 13 ms I over the sea. and between I5 a...
International audiencePolar low (PL) storms are an important feature of the wintertime subsynoptic-s...
In this study polar lows over the Nordic Seas for the period of 1995–2008 have been detected and stu...
International audiencePolar lows are mesoscale (between 200 and 600 km) and short-lived intense low ...
International audienceTo develop a 14-winter (October–April; 1999–2013) climatic description of pola...
To develop a 14-winter (October–April; 1999–2013) climatic description of polar low (PL) occurrence ...
Polar lows (PLs), mesoscale cyclones in high latitudes, impacting Norway are studied in this thesis....
A new climatology of polar lows over the Nordic and Barents seas for 14 seasons (1995/1996-2008/2009...
The study of the “polar low episode” over the northern parts of the Norwegian Sea and the Barents Se...
The large-scale atmospheric circulation during polar low events over the Nordic seas (the North Atla...
Polar lows are small, but extreme cyclones that develop in marine polar air mass. They feature one o...
The polar low in the Norwegian Sea on March 16-17 2008 has been studied using both weather analysis ...
Here we present an objective global climatology of polar lows. In order to obtain objective detectio...
Polar lows are generally short-lived but intense events that occur over cold ocean waters, poleward ...
The sparse observational network over the Arctic region makes severe storms such as polar lows (PLs)...
International audiencePolar low (PL) storms are an important feature of the wintertime subsynoptic-s...
In this study polar lows over the Nordic Seas for the period of 1995–2008 have been detected and stu...
International audiencePolar lows are mesoscale (between 200 and 600 km) and short-lived intense low ...
International audienceTo develop a 14-winter (October–April; 1999–2013) climatic description of pola...
To develop a 14-winter (October–April; 1999–2013) climatic description of polar low (PL) occurrence ...
Polar lows (PLs), mesoscale cyclones in high latitudes, impacting Norway are studied in this thesis....
A new climatology of polar lows over the Nordic and Barents seas for 14 seasons (1995/1996-2008/2009...
The study of the “polar low episode” over the northern parts of the Norwegian Sea and the Barents Se...
The large-scale atmospheric circulation during polar low events over the Nordic seas (the North Atla...
Polar lows are small, but extreme cyclones that develop in marine polar air mass. They feature one o...
The polar low in the Norwegian Sea on March 16-17 2008 has been studied using both weather analysis ...
Here we present an objective global climatology of polar lows. In order to obtain objective detectio...
Polar lows are generally short-lived but intense events that occur over cold ocean waters, poleward ...
The sparse observational network over the Arctic region makes severe storms such as polar lows (PLs)...
International audiencePolar low (PL) storms are an important feature of the wintertime subsynoptic-s...
In this study polar lows over the Nordic Seas for the period of 1995–2008 have been detected and stu...
International audiencePolar lows are mesoscale (between 200 and 600 km) and short-lived intense low ...