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2010.06.06

Weather Charts

  • Gwangju Gwangsangu 5 p.m.

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500 hPa

  • Upper level cold core and low pressure system form some cut-off lows.

  • A temperature of -20 degrees Celsius at 500hPa can be found to have very strong cold air.

850 hPa

  • The 9 degrees Celsius line crosses the Korean Peninsula, so the temperature difference between 500hPa is 29 degrees .

  • Low-level warm moist air exists.

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Surface

  • 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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