Question

Suppose that the concentration of infrared-absorbing gases in earth's atmosphere were to double, effectively creating a second "blanket" to warm the surface. Estimate the equilibrium surface temperature of the earth that would result from this catastrophe. (Hint: First show that the lower atmospheric blanket is warmer than the upper one by a factor of $2^{1/4}$. The surface is warmer than the lower blanket by a smaller factor.)

Short answer

$\text{The temperature of the lower atmosphere blanket is}303\mathrm{K}\text{.}$

Step-by-step solution

Step 1. Given information

The below figure shows two blankets of the earth's atmosphere for receiving the energy from the sun.

In the above figure the upper blanket must send one unit of the infrared energy for every unit of energy absorbed from the sun.

Step 2. Calculating the temperature of the upper blanket

Let the$30\%$of the solar light is reflected. So, the temperature of the upper blanket is

$T_{\text{upper}}={\left(\frac{(0.7)\text{solar constant}}{4\sigma }\right)}^{1/4}$

where, $\sigma$is the Stefan Boltzmann constant.

$\text{Putting}1370\mathrm{W}/{\mathrm{m}}^2\text{for the solar constant and}5.67\times {10}^{-8}\mathrm{W}/{\mathrm{m}}^2{\mathrm{K}}^4\text{for}\sigma \text{.}$

$T_{\text{upper}}={\left(\frac{(0.70)\left(1370\mathrm{W}/{\mathrm{m}}^2\right)}{4\left(5.67\times {10}^{-8}\mathrm{W}/{\mathrm{m}}^2{\mathrm{K}}^4\right)}\right)}^{\frac{1}{4}}$

$=255\mathrm{K}$

So, the temperature of the upper blanket$255K$.

Step 3. Calculating the temperature of the lower blanket

The temperature of the lower blanket is

$T_{\text{lower}}={\left(\frac{2(0.7)\text{solar constant}}{4\sigma }\right)}^{1/4}$

$=(2{)}^{1/4}{\left(\frac{(0.7)\text{solar constant}}{4\sigma }\right)}^{1/4}$

$\text{Putting}{T}_{\text{upper}}\text{for}{\left(\frac{(0.7)\text{solar constant}}{4\sigma }\right)}^{1/4}$we get

$T_{\text{lower}}=2^{1/4}{T}_{\text{upper}}$

So, the temperature of the lower atmosphere blanket is$2^{1/4}$times of the temperature of the upper atmosphere.

$T_{\text{lower}}=2^{1/4}(255\mathrm{K})$

$=303\mathrm{K}$

$\text{Hence, the temperature of the lower atmosphere blanket is}303\mathrm{K}$.

Step 4. Calculating the equilibrium surface temperature of the earth 

The temperature of the earth is

$T_{\text{ground}}={\left(\frac{3(0.7)\text{solar constant}}{4\sigma }\right)}^{1/4}$

$=(3{)}^{1/4}{\left(\frac{(0.7)\text{solar constant}}{4\sigma }\right)}^{1/4}$

Putting $T_{\text{upper}}\text{for}{\left(\frac{(0.7)\text{solar constant}}{4\sigma }\right)}^{1/4}$

$T_{\text{ground}}=3^{1/4}{T}_{\text{upper}}$

$T_{\text{ground}}=3^{\frac{1}{4}}(255\mathrm{K})$

$=335.6\mathrm{K}$

$=(335.6-273.15)°\mathrm{C}$

$=62°\mathrm{C}$

$\text{Hence, the equilibrium surface temperature of the earth is}62°\mathrm{C}\text{.}$