Global warming potential of different greenhouse gases ($CO_2$, $CH_4$, $N_2O$, etc) is determined by their: P: ability to absorb infrared radiation Q: concentration in the atmosphere R: residence time in the atmosphere S: source of origin (whether natural, or anthropogenic)
The Global Warming Potential (GWP) quantifies how effectively a greenhouse gas traps heat compared to carbon dioxide ($CO_2$) over a specific time period. Several factors determine this potential:
Based on the definition and factors influencing GWP, the ability to absorb infrared radiation (P), concentration in the atmosphere (Q), and residence time (R) are the key determinants. Therefore, the correct option includes P, Q, and R.
The table below lists potential environmental conditions in future climates, related to atmospheric carbon dioxide concentrations ($CO_2$) and mean annual temperature (MAT).
The table also lists potential outcomes with respect to whether conditions will favour grasses with C3 or C4 photosynthetic pathways.
Assuming no other changes in environmental conditions, match the options in the two columns.
| Environmental conditions | Outcomes |
| (P) Increased $CO_2$, no change in MAT | (i) C3 performs better than C4 |
| (Q) No change in $CO_2$, increased MAT | (ii) C4 performs better than C3 |
| (iii) C3 and C4 perform equally |