Abstract
Polar lows are subsynoptic-scale cyclones that develop poleward of the main polar front over the ocean. Polar lows are the most intense variety of a general classification of polar mesoscale cyclones. They are typically less than 1000 km in scale and last for just 12-48 h, although they can have associated surface wind speeds of over 30 m s-1 (60 knots). Their scale and brief life cycle make them difficult to observe and forecast, therefore a genuine maritime hazard. Their role in the climate system and their outlook in a changing climate are topics of current research.
Original language | English |
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Title of host publication | Encyclopedia of Atmospheric Sciences |
Subtitle of host publication | Second Edition |
Publisher | Elsevier |
Pages | 379-385 |
Number of pages | 7 |
ISBN (Electronic) | 9780123822260 |
ISBN (Print) | 9780123822253 |
DOIs | |
Publication status | Published - 2015 |
Keywords
- Air-sea heat fluxes
- Arctic instability lows
- Baroclinic instability
- CISK
- Comma clouds
- Convection
- Extratropical cyclones
- Hurricanes
- Mesoscale cyclones
- Nordic Seas
- Polar lows
- Polar mesocyclones
- Potential vorticity
- Vortices
- WISHE