Step 1: Understanding the Concept:
Global Warming Potential (GWP) is a relative measure of how much heat a greenhouse gas traps in the atmosphere compared to a reference gas, typically carbon dioxide (\( \text{CO}_2 \)).
GWP values are calculated over a specific time horizon (usually 100 years) and depend on the gas's infrared absorption capacity and its atmospheric lifetime.
Step 2: Detailed Explanation:
Let us compare the 100-year GWP values of the greenhouse gases listed in the options, as established by the Intergovernmental Panel on Climate Change (IPCC):
Carbon Dioxide (\( \text{CO}_2 \)): This is the baseline reference gas. By definition, its GWP is assigned a value of \( 1 \).
Methane (\( \text{CH}_4 \)): Methane is a potent short-lived greenhouse gas. Over a 100-year timescale, it has a GWP of approximately \( 28 \text{ to } 36 \).
This means that releasing one ton of methane has the same warming effect as releasing about 30 tons of carbon dioxide.
Nitrous Oxide (\( \text{N}_2\text{O} \)): Nitrous oxide is a long-lived greenhouse gas with a high capacity to absorb heat. Its GWP is approximately \( 265 \text{ to } 298 \).
Sulfur Hexafluoride (\( \text{SF}_6 \)): This is an extremely stable, synthetic fluorinated gas used in electrical equipment.
Because of its very long atmospheric lifetime and strong infrared absorption, it has a GWP of approximately \( 23,500 \).
Arranging these gases in descending order of their Global Warming Potential:
\[ \text{SF}_6 \ (23,500) > \text{N}_2\text{O} \ (\sim 273) > \text{CH}_4 \ (\sim 30) > \text{CO}_2 \ (1) \]
This matches the sequence shown in Option (B).
Step 3: Final Answer:
The correct sequence in descending order of Global Warming Potential is $\text{SF}_6 > \text{N}_2\text{O} > \text{CH}_4 > \text{CO}_2$.