What is the structure of the short article in the clouds and mist of Mount Huangshan is a symbolic approach, the second natural paragraph uses the rhetorical devices of metaphor and simile image of the writing, the second paragraph reads as follows:

I've admired the secretive clouds and mist of Alishan, and witnessed the magical sea of clouds of Mount Taishan, but I've never seen such clouds and mist of Mount Huangshan. The clouds of Mount Huangshan are really white, white like a light veil, and as if just under the white snow, so clean, so moist, so crystal clear.

Huangshan's clouds and fog really strange ah, whenever the sunrise before the valley on the fog up clouds, covered in the sky, like the sea is not the sea, such as smoke is not smoke, and occasionally a wind, clouds and fog tumbling, changes in thousands. At this time, the strange peaks, strange rocks, ancient pines in the clouds and mist, this scenery is really called people breathtaking.

When the sun rises, all of a sudden, the sunlight, the clouds become colorful, colorful. Huangshan's clouds are really long ah, like a big curtain to the whole world are shrouded up like a white blanket, so you can not look east to see the end, to the west can not see the end, the momentum is quite spectacular.

Causes and patterns.

The formation of the sea of clouds has its reasons and laws. Mount Huangshan mountains and valleys low, lush forests, short sunshine, water is not easy to evaporate, and thus high humidity, water and gas. It is common to see wisps of light mist rising from the valley after rain.

An average of 250 days of fog throughout the year, it can be called the home of the clouds. Huangshan sea of clouds is formed by low clouds (cloud bottom height below 2500 meters) and ground fog. Low clouds are mainly stratocumulus, which is its characteristics. Between November and March every year, 97% of the sea of clouds in Mount Huangshan are formed by stratocumulus clouds, and only 3% are formed by stratocumulus clouds or fog. from June to September, there are light cumulus clouds and thick cumulus clouds formed by the sea of clouds, accounting for about 6% of the total sea of clouds in this period.