斜压和正压波是什么?- 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 - 04 - 11 - t15:15:57z //www.hoelymoley.com/feeds/question/7165 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/7165 12 斜压和正压波是什么? Darkgod //www.hoelymoley.com/users/5084 2016 - 01 - 04 - t00:18:50z 2017 - 10 - 25 - t15:43:59z < p >我有一个基本的了解似乎斜压和正压是什么意思,但不能让我的头斜压波和正压波。< / p > //www.hoelymoley.com/questions/7165/-/7168 # 7168 7 回答等密度线振荡的斜压和正压波是什么? 等密度线振荡 //www.hoelymoley.com/users/200 2016 - 01 - 04 - t10:03:47z 2016 - 01 - 20 - t21:42:48z < p >正压流的流体密度\ρ取决于压力$ p $美元,即ρ= \ \ρ(p)美元。例如,常数密度、等温、等熵流动正压。斜压流流动不正压。在这种情况下,流体密度取决于压力和温度,盐度,组分浓度。沉重的坐在毗邻打火机液流体沉和上升,分别。< / p > < blockquote > < p >这些流斜压,压力破坏意义。< / p > < /引用> < p >考虑下面两个流体元素。在正压情况下,$ p $的等值线平行的等值线\ρ所以没有美元机制产生涡度。另一方面,在斜压的情况下,的等值线$ p $和$ \ρ美元不平行。后者安排产生涡度变化vec{ω\}\和流通美元因为净压力不再通过质心的液体元素。< / p >

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Seen another way, take a look at the vorticity equation with density variation:

$$\frac{D\vec{\omega}}{Dt} = (\vec{\omega}\cdot \nabla)\vec{u} + \frac{1}{\rho^2}(\nabla \rho \times \nabla p)$$

The cross term on the right hand side is the baroclinic torque. When it is zero the flow is barotropic whereas if it is nonzero the flow is baroclinic.

When applied to waves in the Ocean the result is that barotropic relates to waves propagating at the ocean surface. Baroclinic relates to waves propagating along density surfaces in the interior of the ocean (or internal waves).

One good example is the surface tide and the internal tide. As the surface tide (regular tide) sweeps around the main oceanic basins, it rubs against the ocean floor giving rise to internal tides. The former are called barotropic tides, whereas the latter are called baroclinic tides.


References:

P. Kundu, Fluid Mechanics

B. Sutherland, Internal Gravity waves

//www.hoelymoley.com/questions/7165/-/12539 # 12539 0 答案由user11328斜压和正压波是什么? user11328 //www.hoelymoley.com/users/11328 2017 - 10 - 25 - t15:43:59z 2017 - 10 - 25 - t15:43:59z < p >正压的定义是,密度只取决于压力。斜压的定义是密度可以依赖于其他变量。这本身并不是非常有用,对于理解斜压和正压流意味着什么。< / p > < p >在海洋环境中,水是不可压缩的,所以密度将几乎恒定的正压。因此没有分层海洋正压,和唯一的浪液可以支持与空气的界面。另一方面,如果流体斜压(取决于不恒定温度、密度和盐度),然后可以有内部重力波引起的密度在z方向的变化。< / p > < p >大气,空气相对可压缩。因此如果正压大气中,这意味着唯一的密度变化是由于压力。因此温度水平不变,没有热垂直风切变。这是一个合理的假设在热带地区比在情理之中。

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