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Question

Given the following information, calculate the dry adiabatic lapse rate in Jupiter’s atmosphere.

CompositionSpecific heatAcceleration
due to gravity
$\text{H}_2$$13000\ \text{J/kg/K}$$26\ \text{m/s}^2$

The correct answer is
2° C/km

Calculating Jupiter's Dry Adiabatic Lapse Rate

The dry adiabatic lapse rate ($\Gamma_d$) is the rate at which the temperature of a parcel of dry air decreases as it rises through the atmosphere under adiabatic conditions. It can be calculated using the acceleration due to gravity ($g$) and the specific heat capacity at constant pressure ($c_p$).

Formula for Dry Adiabatic Lapse Rate

The formula used is:

$ \Gamma_d = \frac{g}{c_p} $

Where:

  • $g$ = acceleration due to gravity
  • $c_p$ = specific heat capacity at constant pressure

This formula yields the lapse rate in Kelvin per meter (K/m).

Applying the Formula to Jupiter

We are given the following information for Jupiter:

  • Composition: $\text{H}_2$
  • Specific Heat ($c_p$): $13000 \ \text{J/kg/K}$
  • Acceleration due to gravity ($g$): $26 \ \text{m/s}^2$

Substitute these values into the formula:

$ \Gamma_d = \frac{26 \ \text{m/s}^2}{13000 \ \text{J/kg/K}} $

To perform the calculation, note the unit relationship: $1 \ \text{J} = 1 \ \text{kg} \cdot \text{m}^2/\text{s}^2$. Therefore, the units of $c_p$ are equivalent to $\text{m}^2/(\text{s}^2 \cdot \text{K})$.

$ \Gamma_d = \frac{26 \ \text{m/s}^2}{13000 \ \text{m}^2/(\text{s}^2 \cdot \text{K})} $

$ \Gamma_d = \frac{26}{13000} \ \text{K/m} $

$ \Gamma_d = 0.002 \ \text{K/m} $

Converting Units to °C/km

The question asks for the answer in degrees Celsius per kilometer (°C/km). We need to convert K/m to °C/km.

Unit Conversion Factors:

  • Temperature difference: $1 \ \text{K} = 1 \ \text{°C}$
  • Distance: $1 \ \text{km} = 1000 \ \text{m}$

Apply these conversion factors:

$ \Gamma_d = 0.002 \ \frac{\text{K}}{\text{m}} \times \frac{1 \ \text{°C}}{1 \ \text{K}} \times \frac{1000 \ \text{m}}{1 \ \text{km}} $

$ \Gamma_d = 0.002 \times 1000 \ \text{°C/km} $

$ \Gamma_d = 2 \ \text{°C/km} $

Conclusion

The dry adiabatic lapse rate in Jupiter's atmosphere, based on the given values, is 2 °C/km.

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Important Questions from Planetary Bodies

  1. The correct sequence of planets in order of increasing surface temperature is:
  2. Atmosphere of planet Mars is almost entirely made up of $\text{CO}_2$. But the surface temperature of Mars is less than that of the Earth because:
  3. Consider two planets A and B with radii $2r$ and $r$, respectively. Let their distances from the Sun be $d$ and $2d$, respectively. The solar constants for A ($F_{\text{SA}}$) and B ($F_{\text{SB}}$) are related by
  4. Consider two planets 'A' and 'B' with the following characteristics. The relationship between $T_1$ and $T_2$ is
    Distance from the SunRadius of the planetIncident Solar flux densityEquivalent temperature
    Planet A$d_1$$r_1$$F_1$$T_1$
    Planet B$d_2 = 4d_1$$r_2 = 2r_1$$F_2$$T_2$
  5. Venus is closer to the Sun than Earth, and therefore solar energy incident on Venus is higher than that on Earth. However, the effective radiating temperature of Venus is lower than that of the Earth, because
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