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Analysis
DW-D
2010.06.06
Weather Charts
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Gwangju Gwangsangu 5 p.m.
500 hPa
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Upper level cold core and low pressure system form some cut-off lows.
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A temperature of -20 degrees Celsius at 500hPa can be found to have very strong cold air.
850 hPa
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The 9 degrees Celsius line crosses the Korean Peninsula, so the temperature difference between 500hPa is 29 degrees .
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Low-level warm moist air exists.
Surface
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We can see the development of a strong low-pressure system over Korea. Rapid temperature gradient due to the folding phenomenon of the tropospheric surface can be seen, resulting in cold advection in Korea.
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