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“焚风”顾名思义,就是火一样的风,是山区特有的天气现象。在山岭的一侧是高气压,另一侧是低气压,空气会从高压区向低压区移动。空气在移动途中遇山受阻,被迫上升,气压降低,空气膨胀,温度也就随之降低。空气每上升100米,气温就下降0.6℃,当空气上升到一定高度时,水汽遇冷凝结,形成雨雪落下。空气到达山
As the name implies, “fog wind” is a wind like fire and is a unique weather phenomenon in mountainous areas. On one side of the mountain, there is high pressure, and on the other side, low pressure. Air moves from the high pressure zone to the low pressure zone. When the air is blocked in the middle of the road, it is forced to rise, the air pressure decreases, the air expands, and the temperature decreases. As soon as the air rises by 100 meters, the temperature drops by 0.6 degrees Celsius. When the air rises to a certain height, the water vapor condenses and forms rain and snow. Air reaches the mountain