Why Are Nights More Calm Compared To The Day?
More often than not, the wind dies down at night after a blustery day. Where does the wind go? Why are nights generally more calm than days?
The difference between calm nights and windy days is the sun. During the day, the sun warms the surface of the Earth, which in turn warms the atmosphere above it. But at sunset, the earth’s surface and the layers of the atmosphere directly above it cool faster than higher layers of the atmosphere. That creates a stable temperature pattern, with dense, cool air on the ground and less dense, warmer air above.
And that’s a little crazy, because normally the atmosphere gets cooler as you go up! But with cooler air sitting tight at ground level, the usual temperature pattern turns upside down for a few hundred feet above the ground. Known as a temperature inversion, this upside-down pattern acts as a barrier, dividing the cool, calm air on the ground from whatever’s happening above.
On many calm nights, the wind still blows far overhead, but a temperature inversion prevents it from coming down to earth.
At sunrise, everything changes.The sun warms the earth and the lower layers of the atmosphere, mixing everything up. Without the temperature inversion as a boundary, the winds gust down to the ground again, picking up the most speed on smooth landscapes with little resistance to wind.
為什么夜晚要比白天平靜?
大多數(shù)情況下,大風刮了一天以后會在夜晚時平息下來。風去了哪里呢?為什么夜晚通常會比白天更平靜呢?
平靜的夜晚與多風的白天之間的差異就在于太陽的影響。白天的時候,太陽照射會使地球表面溫度升高,進而會使大氣溫度也隨之上升。但日落時,地球表面和表面 上方的大氣溫度比高層大氣下降得更快。由此會產(chǎn)生一種穩(wěn)定的氣溫狀態(tài),地面空氣的密度大,溫度較低,而地面上方的空氣較為稀薄,溫度較高。
這聽起來有點不可思議,因為通常情況下,氣溫是隨著高度的增加而降低的。但是隨著冷空氣停留在地表,地表上方幾百英尺處的氣溫模式就會發(fā)生顛倒。這就是逆溫現(xiàn)象,這種倒置的氣溫模式就像是屏障一樣,使地表較冷而平靜的空氣從上層大氣中分離出來。
在許多個平靜的夜晚中,風依舊在我們頭頂上方遠遠吹過,但逆溫現(xiàn)象會阻止風吹向地面。
日出的時候,一切都變了。太陽的照射會使地球和低層大氣溫度升高,所有氣流都混合在一起。沒有了逆溫層作為阻隔物,風又會吹向地面,在幾乎不受阻力的情況下加速吹過平坦的地面。