离心力是如何确定流体运动方程在地球的旋转参考系?- 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 - t22:37:16z //www.hoelymoley.com/feeds/question/24600 https://creativecommons.org/licenses/by-sa/4.0/rdf //www.hoelymoley.com/q/24600 3 离心力是如何确定流体运动方程在地球的旋转参考系? MichaelW //www.hoelymoley.com/users/21047 2022 - 12 - 08 - t08:18:57z 2022 - 12 - 08 - t10:52:52z < p >我已经花费几天时间如下:在我的一个气象脚本的动量守恒方程给出了地球的旋转参考系:< / p > < p > < a href = " https://i.stack.imgur.com/GctmI.png " rel = " nofollow noreferrer " > < img src = " https://i.stack.imgur.com/GctmI.png " alt = "在这里输入图像描述" / > < / > < / p > < p >橙色的明显的力量,其他的是显而易见的。< / p > < p >我想知道为什么没有离心力,然而,明显的在一个旋转系统应该是科氏力和离心力的总和。< / p > < p >来了解更多关于这些方程的推导我仔细研究了这个视频:< a href = " https://www.youtube.com/watch?v=nljud2UiWUk&list=PL_cuIb7hx5lg_zHfUVsUrw6I66U4jq8Dq" rel="nofollow noreferrer">https://www.youtube.com/watch?v=nljud2UiWUk&list=PL_cuIb7hx5lg_zHfUVsUrw6I66U4jq8Dq

At it's end, the equations are written down:

enter image description here

First I'm surprised that there are "curvature" forces: In my opinion they are nothing else but the centrifugal forces, but usually the total acceleration a' seen in a rotating system is written down as

$$\vec a' = -\vec \omega \times \left(\vec \omega \times \vec r' \right) - 2 \cdot \vec \omega \times \vec v' \tag{1}$$

First term is called usually "centrifugal force" while the right term is the Coriolis force. But when I consider motion with (zonal) velocity u (along the east) on the equator, the total centrifugal force in radial direction z would be

$$a_z = \frac{(u+\omega R)^2}{R} = \omega^2R+u^2/R+2 \omega \cdot u \tag{2}$$

because the total tangential speed is the sum of earth's rotation and zonal speed.

Now I wonder, where the quadratic term would be derived from equation (1). I see only the first and third term arising from (1) but not the middle...

It seems a bit, that the u,v,w-driven part of what I call "centrifugal force" is absorbed into the Coriolis force and when we speak about centrifugal force only the static part of it (u=v=0) is regarded.

However, when this is the case, there is still one missing thing: when u=v=w=0 we have a point at rest in earth's reference frame. At a given northern latitude $\phi$ there is clearly a centrifugal force which doesn't point in pure z-direction but also has a y-component, pointing south:

$$F_y = \Omega^2 R \cos(\phi) \sin(\phi)$$

so I would expect this as a "static" part of the second equations for $Dv/dt$.

However, in neither in the first image (my script) nor in the second one (the video) such component is identified: everything is proportional to u,v,w without a static component.

Even worse, in the first image (taken from my lecture) the centrifugal forces are missing completely.

Final questions in particular:

  1. How do quadratic terms arise from (1)?
  2. Where have centrifugal components gone to in the first image? It drives me nuts...
  3. Why "curvature force" when everywhere else (in my physics textbooks) total force is split just into centrifugal and Coriolis? Is there a new basic force "curvature" which I have overseen previously or is is just a matter of definition of whether we assign some mathematically arising components to "Coriolis" or "centrifugal"?
  4. Could it be, that centrifugal force is just the "static" centrifugal force due to earth's rotation and the other components are distributed along linear and quadratic terms, where the quadratic terms are called "curvature forces" and the linear ones "Coriolis". Something here is not consistent with my textbook knowledge I learned in the past.
//www.hoelymoley.com/questions/24600/-/24601 # 24601 3 答案由大卫Hammen离心力是如何确定的流体运动方程在地球的旋转参考系? 大卫Hammen //www.hoelymoley.com/users/239 2022 - 12 - 08 - t10:52:52z 2022 - 12 - 08 - t10:52:52z < blockquote > < p >我想知道为什么没有离心力,然而,明显的在一个旋转系统应该是科氏力和离心力的总和。< / p > < /引用> < p >有一个离心加速度方程。我们称之为“gravity"躺在意义上是一个重力加速度和离心加速度。在技术意义上,我们称之为“gravity"是自由落体的身体在海平面的加速度作为参照系中观察到固定的地球旋转。离心加速度烤成< span class = " math-container”> g < / span >美元。< / p > < p >这意味着离心加速度存在于你的方程。特别是,它是在你的方程(3)< span class = " math-container " > g < / span >美元。如果一个< span class = " math-container”> g < / span >美元作为一个常数,< span class = " math-container " > $ g_0 = 9.80665 \ \ {m} / \文本{年代}^ 2美元< / span >(可能是一个坏主意),这是重力和离心力加速度约巴黎的纬度。我们称之为< span class = " math-container”> g < / span >美元随纬度和高度椭球,加上本地的小扰动。喜马拉雅山附近(重力可以相当复杂,如果一个想成为非常精确。)< / p > < p >一个相当简单的近似,占纬度(但不是高度)是Somigliana引力公式,< span class = " math-container " > $ $ g = g_文本{eq}}{\ \压裂{1 + \ kappa \罪^ 2 \φ}{\√6{单电子^ 2 \罪^ 2 \φ}}$ $ < / span >, < span class = " math-container " >美元g_{\文本{eq}} = 9.7803267714 \ \ {m} / \文本{年代}^ 2 $ < / span >是重力加速度在赤道(包括离心加速度),< span class = " math-container " > \ k = 0.00193185138639美元< / span >,它反映了观测重力在赤道和两极之间的区别,< span class = " math-container " > $ e ^ 2 = 0.00669437999013 $ < / span >是偏心的平方图的地球,和<跨类= " math-container " > \φ< / span >美元是大地纬度。< / p > < p >随高度变化(“自由空气correction")成线性比例在地球大气层的减少<跨类= " math-container " > 3.086美元\ \{μm} /文本\文本{年代}^ 2 $ < / span >每米的海拔。 If you are using $g$ as a constant, you are essentially ignoring both the latitude and altitude corrections. Centrifugal acceleration is baked in. If you are using the Somigliana formula (or some other approximation of gravitation at sea level as a function of latitude), centrifugal acceleration is once again baked in.

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