Step 1: Initial Conditions and Rate of Reduction
In 2020, the emissions are 40 Giga tons, and 50% of this is retained in the atmosphere. Thus, the amount of CO\(_2\) that stays in the atmosphere from the emissions in 2020 is:
\[
40 \times 0.5 = 20 \, \text{Giga tons}.
\]
In 2021, the emissions are reduced to 39 Giga tons, and 50% of this is retained in the atmosphere:
\[
39 \times 0.5 = 19.5 \, \text{Giga tons}.
\]
Similarly, in 2022, the emissions are reduced to 38 Giga tons, and half of this is retained:
\[
38 \times 0.5 = 19 \, \text{Giga tons}.
\]
Step 2: Cumulative Effect of Emissions
The amount of CO\(_2\) in the atmosphere increases each year by the retained emissions. If the emissions continue to decrease by 1 Giga ton each year starting from 2021, the accumulated emissions from all the years will continue to contribute to the increase in CO\(_2\) concentration in the atmosphere.
The total retained emissions can be calculated cumulatively:
\[
\text{Total retained emissions} = 20 + 19.5 + 19 + \dots.
\]
Since emissions are being reduced each year, it will take time for the contributions to reduce sufficiently for the total emissions to stop rising. In this case, by the year 2060, the emissions will have reduced enough that the total amount of CO\(_2\) in the atmosphere due to anthropogenic emissions will stop rising, assuming that all emissions are retained.
Thus, the year when the CO\(_2\) concentration in the atmosphere stops rising due to anthropogenic emissions is around 2060.
Final Answer: \[ \boxed{2060}. \]
The value of the determinant 
is: