什么是温度反演和陷阱烟雾/污染吗?- 江南体育网页版- - - - -地球科学堆江南电子竞技平台栈交换 最近30从www.hoelymoley.com 2023 - 07 - 08 - t18:54:05z //www.hoelymoley.com/feeds/question/5123 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/5123 6 什么是温度反演和陷阱烟雾/污染吗? reddit //www.hoelymoley.com/users/3087 2015 - 07 - 04 - t04:45:15z 2018 - 03 - 28 - t19:56:35z < p >正如标题说,我听说过这个词,但不知道它是如何工作的。< / p > //www.hoelymoley.com/questions/5123/-/5127 # 5127 1 看你回答的是什么温度反演和陷阱烟雾/污染吗? 看到你 //www.hoelymoley.com/users/3126 2015 - 07 - 04 - t14:01:48z 2015 - 07 - 06 - t15:33:57z < p >这是直接从< a href = " https://en.wikipedia.org/wiki/Inversion_(气象学)”rel =“nofollow”>维基百科< / >:< / p > < blockquote > < p >在气象、反演是一种偏离正常高度的大气性质的变化。它几乎总是指“逆温层”,即温度随高度的增加,或层(“逆温层”)在这样一个增加发生。< / p > < p >倒置等可能导致污染的烟雾被困靠近地面,可能对健康造成不良影响。倒置还可以抑制对流通过扮演一个“帽子”。如果这个帽坏了的几个原因,对流的水分可以爆发雷暴。众所周知逆温层可以导致冻雨在寒冷气候。< / p > < /引用> //www.hoelymoley.com/questions/5123/-/5128 # 5128 12 答案由丹尼尔Griscom逆温层是什么和它能陷阱烟雾/污染吗? 丹尼尔Griscom //www.hoelymoley.com/users/534 2015 - 07 - 04 - t14:08:02z 2015 - 07 - 04 - t14:08:02z < p >正常,温度普遍< a href = " https://en.wikipedia.org/wiki/Lapse_rate " > < / >随高度,和对流是有效的:本地暖空气上升,冷空气就会下降。< A href = " https://en.wikipedia.org/wiki/Inversion_(气象学)" >逆温层< / >是那里的空气温度<强> < / >强上升高度。这意味着空气对流不太有效,因为上面已经温暖,所以有更少的混合海拔之间的空气。< / p > < p >因为污染一般产生在地面上,温度反演可以陷阱在地面污染(如烟雾)。< / p > //www.hoelymoley.com/questions/5123/-/5142 # 5142 6 由凯西回答什么是温度反演和陷阱烟雾/污染吗? 凯西 //www.hoelymoley.com/users/64 2015 - 07 - 06 - t16:55:59z 2015 - 07 - 06 - t16:55:59z < p >为其他人所注意到的那样,逆温层是一层温度随高度增加。这叫做一个反转,因为正常的温度曲线随高度。< / p > < p >温度反演可以陷阱污染。因素影响这环境温度剖面,烟囱的高度或烟囱排出污染和污染物的温度,因为他们离开烟囱。< / p > < p >如果来自烟囱空气的温度比周围的温暖和漂浮污染物不太重,空气浮力和上升。即使在严重污染的情况下,那些沉重的颗粒倾向于烟囱附近的落在地上,地面污染环境而其余的东西的栈上涨。尤其明显在冬天煤栈栈附近的雪逐渐变成橙色。漂浮污染物将上升的空气由直到他们不再活跃,然后他们将稳定在高度找到平衡。< / p > < p >来演示,考虑以下两种情形。< / p >

enter image description here

This scenario has an environmental temperature profile based on a surface temperature of 20 C, a dewpoint around 8 C, no capping inversion and a well mixed boundary layer. The black line represents the temperature a parcel lifted from the surface would have. The pollutants are being emitted from a smokestack with a height around 300 m with a temperature around 22 C. I've also assumed no water vapor coming out of the smokestacks. In this case the air from the smokestack (red) is always warmer than the environment and it escapes the boundary layer and rises well above the surface. This pollution is not trapped.

enter image description here

This scenario has a capping inversion between 900 and 850 mb but is otherwise the same as the previous example (same surface temperature and dewpoint). The pollutants have the same properties as the first scenario. In this case, however, due to the temperature inversion there is a height where the environment becomes warmer than the pollutants. If the pollutant ties to rise any higher it will be negatively buoyant and will oscillate around the height of neutral buoyancy (see Brunt–Väisälä frequency). In this case the pollution will be trapped around 860 mb, which is around 1250 m. This isn't too close to the ground but in a well mixed boundary layer this pollution eventually will be mixed throughout the boundary layer. This pollution is trapped.

Both of these scenarios are on warm well-mixed days. Bigger problems tend to happen at night or early morning and in the cold season. In these cases deep inversions that start at the surface tend to form and if smokestacks are not very tall this can cause pollution to be trapped very close to the ground. This kind of temperature structure will cause the pollutant to spread out at low heights. In places where these type of inversions are frequent it is important that smokestacks are built tall enough to emit pollution above the inversion height. The picture below demonstrates how this kind of pollution trapping can look.

enter image description here Image by JohanTheGhost, wikimedia commons. https://commons.wikimedia.org/wiki/File:SmokeCeilingInLochcarron.jpg

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