Hallasan topographic map

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Hallasan

The occurrence of the highest temperature coincides with the formation position of the eddy, and when the wind is weak, the eddy forms in the middle mountain region. When the wind is weak, the warmth is accumulated in the middle layer, so the maximum temperature in the mid-mountainous area is higher than the maximum temperature of the low-altitude coastal area about 1–3 °C, and 4 °C or higher on the downwind side.

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