Final answer:
The yearly rate of change in the amount of CO₂ in the atmosphere increases by a factor of 1.06.
Step-by-step explanation:
The yearly rate of change in the amount of CO₂ in the atmosphere can be determined by finding the ratio of the amount of CO₂ in a given year to the amount of CO₂ in the previous year.
In this case, the function a_decade(t) = 315 * (1.06)⁽ᵗ⁾ represents the total amount of CO₂ in the atmosphere in parts per million (ppm) as a function of the elapsed time in decades, t, since CO₂ levels were first measured. To find the yearly rate of change, we need to find the ratio of a_decade(t+1) to a_decade(t), as t represents time in decades.
Let's calculate the ratio:
a_decade(t+1) / a_decade(t) = (315 * (1.06)⁽ᵗ⁺¹⁾) / (315 * (1.06)⁽ᵗ⁾)
Simplifying the expression:
a_decade(t+1) / a_decade(t) = 1.06
Therefore, every year, the amount of CO₂ in the atmosphere increases by a factor of 1.06.