General features of polar lows over the Japan Sea and the Northwestern Pacific |
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Authors: | Fu Gang Liu Qin-yu Wu Zeng-mao |
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Institution: | (1) College of Physical and Environmental Oceanography, Ocean University of Qingdao, 266003 Qingdao, China |
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Abstract: | This study of general features of occurrence frequencies, spatial distribution of locations, life-time and cloud patterns
of polar lows over the Japan Sea and the neighboring Northwestern Pacific in winter of 1995/1996 based on observation and
satellite satellite data showed that polar lows develop most frequently in mid-winter over the Japan Sea (35–45°N) and the
Northwestern Pacific (30–50°N). They rarely form over the Eurasian Continent. Polar lows over the Northwestern Pacific are
usually longlived (2–3 days). But polar lows over the Japan Sea are relatively short-lived (1–2 days), because the east-west
width of the Japan Sea is relatively narrow and polar lows tend to decay after their passing over the Japan Islands.
Generally speaking, polar lows over the Japan Sea are characterized by tight, spital (or comma) cloud patterns on satellite
images. It was observed that polar lows over the Japan Sea have a typically spiral cloud band with clear “eye” at their mature
stage. In winter, because of the effect of the warm Tsushima Current, the annual mean SST of the Japan Sea is 5–9°C higher
than that of the same latitude oceans. The large sea-air temperature difference sustained over the Japan Sea provides favorable
condition for polar formation. The general features of polar lows over the Japan Sea are compared with those of other areas
where polar lows often occur. |
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Keywords: | polar lows the Japan Sea satellite data spiral cloud band |
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