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- W2374268595 abstract "Polar low is an intense cyclone that develops over middle-or high-latitude oceans in winter. In this paper, a meso-α-scale polar low which occurred over the Japan Sea on December 4 2005 was investigated by using almost all available observational data,including the GOES(Geostationary Operational Environmental Satellite)-9 infrared satellite imagery,the FNL(Final Analyses) data and the latent heat flux data issued by NCEP(National Centers for Environmental Prediction). Firstly, the evolutionary process of this polar low was documented based upon the satellite imagery, and its whole life can be divided into four stages: initial, developing, mature and dissipation stages. Prior to the development of the polar low, there existed a strong baroclinic zone in the upper-atmosphere accompanied with stronger cold advection. On satellite image, the mature polar low had a spiral-shaped cloud bands and a clear eye structure. The eye area of the polar low was free of wind, and was accompanied with a stronger updraft near its center region. This polar low also had a warm core structure at its mature stage. The baroclinicity and the transports of sensible and latent heat fluxes from the ocean to the atmosphere seemed to be the major contributors for the polar low development." @default.
- W2374268595 created "2016-06-24" @default.
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- W2374268595 date "2008-01-01" @default.
- W2374268595 modified "2023-09-25" @default.
- W2374268595 title "A Case Study of a Polar Low over the Japan Sea on 4 December 2005" @default.
- W2374268595 hasPublicationYear "2008" @default.
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