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The character 霭, with its traditional form 靄, is structured from the rain radical 雨 positioned above the component 謁, which historically functioned as a phonetic element, thereby associating the character with atmospheric conditions like mist or haze. The simplified form 霭 adapts this by replacing the bottom with 谒, the simplified counterpart of 謁, maintaining the same structural logic. Etymologically, the character has consistently referred to visible vapor or cloudiness in the air, and over time its semantic range extended to include literary connotations of a gentle, diffuse vapor or a soft, cloudy atmosphere in poetic contexts.
Etymology Hide