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Also, that the centripetal force component $\frac{v^2}{r}$ is a proxy for all the dynamical forces (rotational, turbulence, etc.) This equation is the hydrostatic equation, which describes a change of atmospheric pressure with height.We could integrate both sides to get the altitude dependence of From Equation 2.20, the atmospheric pressure falls off exponentially with height at a rate given by the scale height. Start here for a quick overview of the site

Using the Ideal Gas Law, we can replace ρ and get the equation for dry air: d p d z = − g p R d T o r d p p = − g R d T d z = − M g R * T d z This equation is not rendering properly due to an incompatible browser. We can sum these three forces together and set them equal to 0 since the parcel's at rest. I pulled this equation out of 'Physics, Formation and Evolution of Rotating Stars', A. Maeder.The centripetal force is an aggregate of real forces.

<< /S /GoTo /D (slide.13) >> 64 0 obj endobj 22 0 obj endobj 65 0 obj Learn more about Stack Overflow the company

The formula above is trying to make a ballpark estimate of these non-thermal contributions to the mass estimate given that pure HE is an increasingly unreliable assumption.This is incorrect for (at least) the reason given by Sebastian Rise above. 39 0 obj

endobj endobj There is no simple formula and the one you have postulated is manifestly incorrect, since it assumes spherical symmetry when there will be an axis of rotation. In fact, we can use the isothermal and adiabatic gas laws to explain most of the observable features of the atmosphere.

The real forces at work here are the gravitational force inward and the pressure gradient force outward. I could also make the argument that $E = \frac{1}{2}mv^2$ is incorrect, but it is a useful approximation.

The smallest object that appears to have an equilibrium shape is the icy moon Solid bodies have irregular surfaces, but local irregularities may be consistent with global equilibrium. << /S /GoTo /D (slide.5) >>

The smallest body confirmed to be in hydrostatic equilibrium is the dwarf planet Ceres, which is icy, at 945 km, whereas the largest body known to not be in hydrostatic equilibrium is the Moon, which is rocky, at 3,474 km.

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95 0 obj () << /S /GoTo /D (slide.7) >> 54 0 obj endobj endobj Now, define the quantity (what is g(r)?) 104 0 obj endobj

() Dividing by Consider an air parcel at rest. Hydrostatic paradox deals with the pressure of a liquid at all points of the same horizontal level (depth).

endobj At 40 km, the pressure is only a few tenths of a percent of the surface pressure. << /S /GoTo /D (slide.17) >>

Hydrostatic Pressure Derivation. By using our site, you acknowledge that you have read and understand our Physics Stack Exchange is a question and answer site for active researchers, academics and students of physics.

123 0 obj 112 0 obj 139 0 obj [adsenseyu1] Formula no. 138 0 obj << /S /GoTo /D (slide.19) >>

The two videos below show how to use the formula no.

I first encountered it in Schwartzchild's book---all the data in which is massively dated now, but the basic physics is there and it is relatively inexpensive.For the purposes of the questions you've been asking it doesn't matter. The best answers are voted up and rise to the top << /S /GoTo /D (slide.5) >> xڕUKs�0��W�(�Ԫ���c�I�IOI�erp��`l���+0t This sum equals zero if the fluid's velocity is constant. 108 0 obj $$ \frac{1}{\rho} \nabla P = -\nabla \Psi -r^2 \sin^2 \theta \nabla \Omega $$

endobj endobj Preliminaries: the hydrostatic equation 42 0 obj Using the formula of pressure: 50 0 obj QED.

endobj << /S /GoTo /D (slide.20) >> The formula is a 'ballpark' estimate.To subscribe to this RSS feed, copy and paste this URL into your RSS reader. Where $wm_p$ is the mean molecular weight times the mass of a proton, $\rho_X(r)$ is the density of gas at radius $r$, and $T(r)$ and $v(r)$ and $M(r)$ are the temperature, velocity and mass (respectively) at the same radius.Is there a canonical expression for the accelerations in this kind of body or is the idea of hydrostatic equilibrium invalidated with a rotating body?The equation you have written cannot be correct, even approximately, except in cases where rotation is unimportant.If rotation of the gas is important, that rotation occurs around an axis. endobj

98 0 obj so that we have What balances this gravitational force? endobj 135 0 obj << /S /GoTo /D (slide.18) >> 84 0 obj This force balance is called a hydrostatic equilibrium. $$ \frac{1}{\rho} \nabla P = -\nabla \Psi $$In general then, the pressure gradient is no longer in the radial direction, however the isobars are still equipotentials.An alternative approximation is to consider "shellular rotation", where $\Omega$ is constant along isobars. () () endobj endobj << /S /GoTo /D (slide.21) >>

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$$\frac{1}{\varrho}\frac{dp}{dr}= -\frac{GM_r}{r^2}$$This is valid for stars with no fast radial motions. Of course the formula depends on $\Phi$, as does the version without rotation.OK, I'll try my comment in a different way then: what am I missing? 72 0 obj

<< /S /GoTo /D (slide.13) >> << /S /GoTo /D (slide.3) >> 62 0 obj

endobj Formula for Hydrostatic Pressure.

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hydrostatic equilibrium formula