The hydrostatic equilibrium equation including temperature, T(z)

In summary, the problem deals with modeling the lower atmosphere of Venus and estimating the adiabatic lapse rate. The hydrostatic equilibrium equation is used to confirm the adiabatic lapse rate and includes the variation of temperature (T(z)) in its calculation. However, solving for T(z) and plugging it into the equation yields a seemingly useless result. Further clarification may be needed to fully understand the problem.
  • #1
ndgoodburn
1
0

Homework Statement


In this problem, you'll model the lower atmosphere of Venus. The atmospheric pressure reaches 1 bar (100 kPa) in the middle of the dense cloud deck, where T ~ 350 K. At the surface, the pressure is 90 bars (9000 kPa). From the surface to the 1 bar level, the temperature T(z) decreases at a rate of dT/dz = -8 K [itex]km^{-1}[/itex], close to the adiabatic lapse rate of -8 K [itex]km^{-1}[/itex].

(b)Write down the equation for hydrostatic equilibrium, including explicitly the variation T(z).

Homework Equations


We can estimate the adiabatic lapse rate with the approximation:
[itex]\frac{dT}{dz}|_{ad}=-\frac{g}{c_p}[/itex]

The equation for hydrostatic equilibrium:
[itex]\Delta P = -\rho \Delta z g[/itex]

The Attempt at a Solution


Part (a) asks me to confirm the adiabatic lapse rate for Venus, which is simple by plugging in g and cp.

Part (b) (asking for the hydrostatic equilibrium equation) is what is confusing me. I am specifically having trouble including T(z). I can find an expression for T(z) by integrating the adiabatic lapse rate approximation:

[itex]∫\frac{dT}{dz} dz|_{ad}=∫-\frac{g}{c_p} dz[/itex]

[itex]T(z)=T_0-\frac{g}{c_p}z[/itex]

I called the constant of integration T0 because that makes sense conceptually.

Now, what I tried was just solving T(z) for g and plugging it into the hydrostatic equilibrium equation because I'm just trying to find a way to include it, but that just yields

[itex]\Delta P=-\rho \Delta z \frac{c_p}{z}(T_0-T(z))[/itex]

which seems useless to me, because T(z) would quickly reduce out with a tiny bit of simplification.

Maybe someone can help by telling me if what I've done so far makes sense and if I should continue, or if I'm just missing something that would make it more clear. Thanks in advance!
 
Last edited:
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  • #2
ndgoodburn said:
[itex]\frac{dT}{dz}|_{ad}=-\frac{g}{c_p}[/itex]

The equation for hydrostatic equilibrium:
[itex]\Delta P = -\rho \Delta z g[/itex]
Just guessing here, but if [itex]\frac{dT}{dz}|_{ad}=-\frac{g}{c_p}[/itex] then can you not write [itex]\Delta T = -\frac{g\Delta z}{c_p} = \frac{g\Delta P}{c_p\rho} [/itex]?
 

Related to The hydrostatic equilibrium equation including temperature, T(z)

1. What is the hydrostatic equilibrium equation?

The hydrostatic equilibrium equation is a fundamental equation in fluid mechanics that describes the balance of forces acting on a fluid at rest. It states that the pressure gradient within a fluid is equal to the weight of the fluid per unit volume, and is essential for understanding atmospheric and oceanic dynamics.

2. How is temperature incorporated into the hydrostatic equilibrium equation?

In the hydrostatic equilibrium equation, temperature is included as a variable in the pressure term. This is because temperature affects the density of the fluid, which in turn affects the weight per unit volume. As temperature increases, the fluid expands and becomes less dense, resulting in a decrease in pressure.

3. What is the significance of the hydrostatic equilibrium equation in meteorology?

The hydrostatic equilibrium equation is crucial for understanding the structure and dynamics of Earth's atmosphere. It helps meteorologists predict changes in air pressure, which can lead to changes in weather patterns. It also plays a role in the formation of clouds, precipitation, and other atmospheric phenomena.

4. Can the hydrostatic equilibrium equation be applied to other fluids besides air and water?

Yes, the hydrostatic equilibrium equation can be applied to any fluid, as long as it is in a state of rest. This includes liquids, gases, and even plasmas. It is a fundamental equation in fluid mechanics and is used in various fields, including meteorology, oceanography, and engineering.

5. How does the hydrostatic equilibrium equation relate to the ideal gas law?

The hydrostatic equilibrium equation and the ideal gas law are closely related. The ideal gas law describes the relationship between pressure, volume, and temperature in a gas, while the hydrostatic equilibrium equation describes the balance of forces in a fluid. Both equations incorporate temperature as a variable and are essential for understanding the behavior of gases and fluids.

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