GWP Formula:
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Global Warming Potential (GWP) is a measure of how much heat a greenhouse gas traps in the atmosphere over a specific time period, relative to carbon dioxide. It's calculated as the ratio of the time-integrated radiative forcing from a pulse emission of a gas to that of CO₂.
The calculator uses the GWP formula:
Where:
Explanation: The equation compares the cumulative radiative forcing of a greenhouse gas to that of CO₂ over a specified time period, typically 100 years.
Details: GWP is crucial for climate policy, emissions trading, and comparing the climate impact of different greenhouse gases. It helps prioritize mitigation efforts and evaluate the effectiveness of climate policies.
Tips: Enter the integrated radiative forcing value and integrated CO₂ value. Both values must be positive numbers representing the cumulative effect over the chosen time horizon.
Q1: What time horizons are typically used for GWP?
A: The most common time horizons are 20, 100, and 500 years, with 100 years being the standard for international climate agreements.
Q2: Why is CO₂ used as the reference gas?
A: CO₂ is used as the reference (GWP = 1) because it's the most abundant anthropogenic greenhouse gas and serves as a baseline for comparison.
Q3: How does GWP differ for various greenhouse gases?
A: Different gases have different GWPs based on their radiative efficiency and atmospheric lifetime. For example, methane has a GWP of about 28-36 over 100 years.
Q4: What are the limitations of GWP?
A: GWP doesn't account for indirect effects, changes in atmospheric chemistry, or different emission scenarios. It's a simplified metric for policy purposes.
Q5: How is GWP used in climate policy?
A: GWP is used to convert emissions of various greenhouse gases into CO₂ equivalents for emissions reporting, carbon trading, and policy target setting.