国产av不卡一区二区_欧美xxxx做受欧美_成年人看的毛片_亚洲第一天堂在线观看_亚洲午夜精品久久久中文影院av_8x8ⅹ国产精品一区二区二区_久久精品国产sm调教网站演员_亚洲av综合色区无码一二三区_成人免费激情视频_国产九九九视频

今天西北風(fēng)，明天又是東南風(fēng)，還有狂風(fēng)，微風(fēng)。風(fēng)當(dāng)然是天氣中很重要的一個組成部分，風(fēng)的產(chǎn)生是跟空氣的流動有直接關(guān)系的。

Air is set in motion by the Pressure Gradient Force (PGF)（氣壓梯度力）. This, as you well know, is a flow from high pressure to low pressure. In nature, regions of excess move toward regions of deficit. This comes from the second law of thermodynamics（熱力學(xué)） that states higher energy states move toward lower energy states. Nature is always trying to balance. The result of trying to balance and equalize pressure results in wind. The pressure gradient force acts on a horizontal plane.

What causes the pressure changes in the atmosphere? The primary reason is through the warming and cooling of air. The pressure exerted by a gas changes as it becomes denser or less. Since a cold air mass is denser and has a lower thickness than warm air, pressure decreases more rapidly with height in cold air than in warm air. When cold dense air is placed next to warm less dense air, wind results by nature trying to balance the pressure differences at each level in the atmosphere between the two air masses. This can occur on all scales of motion. Examples: On the planetary scale, temperature gradients create the polar jet stream（急流）; on the synoptic scale it creates jet streaks; on the mesoscale（中尺度） it creates sea breeze circulations and the low level jet; on the microscale it creates lake breezes.

（來源：theweatherprediction.com 英語點(diǎn)津 Helen 編輯）