A mountain climber wears a goose-down jacket 3.8 cm thick with total surface area 0.95 m². The temperature at the surface of the clothing is -18°C and at the skin is 34°C. Determine the rate of heat flow by conduction through the jacket assuming (a) it is dry and the thermal conductivity k is that of goose down, and (b) the jacket is wet, so k is that of water and the jacket has matted to 0.50 cm thickness.
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20. Heat and Temperature
Heat Transfer
Problem 97
Textbook Question
(a) Using the solar constant, estimate the rate at which the whole Earth receives energy from the Sun. (b) Assume the Earth radiates an equal amount back into space (that is, the Earth is in equilibrium). Then, assuming the Earth is a perfect emitter, (∈ = 1.0) estimate its average surface temperature. [Hint: Discuss why you use area A = πr²E or A = 4πr²E in each part.]

1
Step 1: Understand the solar constant. The solar constant is the amount of solar energy received per unit area per second at the Earth's distance from the Sun. Denote it as S (approximately 1361 W/m²). To calculate the total energy received by the Earth, consider the cross-sectional area of the Earth that intercepts sunlight, which is a circle with area A = πr²_E, where r_E is the Earth's radius.
Step 2: Calculate the total power received by the Earth. Multiply the solar constant (S) by the cross-sectional area of the Earth (A = πr²_E). The formula is: P_received = S × πr²_E. This gives the total rate at which the Earth receives energy from the Sun.
Step 3: Recognize that the Earth is in thermal equilibrium. This means the Earth radiates energy back into space at the same rate it absorbs energy from the Sun. The total surface area of the Earth that radiates energy is the surface area of a sphere, A = 4πr²_E. Use this area for the radiation calculation.
Step 4: Use the Stefan-Boltzmann law to calculate the Earth's radiated power. The Stefan-Boltzmann law states that the power radiated per unit area by a blackbody is P/A = σT⁴, where σ is the Stefan-Boltzmann constant (5.67 × 10⁻⁸ W/m²·K⁴) and T is the temperature. The total power radiated by the Earth is P_radiated = σT⁴ × 4πr²_E.
Step 5: Set the power received equal to the power radiated to find the Earth's average surface temperature. Equate P_received = P_radiated, which gives S × πr²_E = σT⁴ × 4πr²_E. Simplify to solve for T: T = [(S / (4σ))]^(1/4). Substitute the known values for S and σ to calculate the Earth's average surface temperature.

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Key Concepts
Here are the essential concepts you must grasp in order to answer the question correctly.
Solar Constant
The solar constant is the amount of solar energy received per unit area at the top of Earth's atmosphere, approximately 1361 watts per square meter. This value is crucial for estimating the total energy Earth receives from the Sun, as it allows us to calculate the energy flux over the entire surface area of the Earth, which is essential for understanding Earth's energy balance.
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Equilibrium Temperature
The equilibrium temperature of the Earth is the temperature at which the energy received from the Sun equals the energy radiated back into space. This concept is based on the Stefan-Boltzmann law, which states that the power radiated by a black body is proportional to the fourth power of its temperature. In this context, it helps us estimate the average surface temperature of the Earth assuming it behaves as a perfect emitter.
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Surface Area Calculations
When calculating the energy received by the Earth, the surface area used is critical. The area A = πr²_E represents the cross-sectional area of the Earth facing the Sun, while A = 4πr²_E accounts for the total surface area of the Earth. Understanding which area to use in each part of the problem is essential for accurately determining the energy balance and the resulting temperature.
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