GWP Formula:
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The GWP (Global Warming Potential) formula calculates the relative measure of how much heat a greenhouse gas traps in the atmosphere compared to carbon dioxide. It is a key metric for assessing the climate impact of different greenhouse gases.
The calculator uses the GWP formula:
Where:
Explanation: The formula compares the warming effect of a greenhouse gas to that of carbon dioxide over a specific time period, typically 100 years.
Details: GWP calculation is crucial for climate policy, emissions trading, and understanding the relative impact of different greenhouse gases on global warming. It helps prioritize mitigation efforts and set emission reduction targets.
Tips: Enter radiative efficiency in W/m²/ppb, lifetime in years, and CO2 reference values. All values must be positive numbers greater than zero for accurate calculation.
Q1: What is radiative efficiency?
A: Radiative efficiency measures how effectively a gas absorbs infrared radiation and contributes to the greenhouse effect, expressed in watts per square meter per parts per billion (W/m²/ppb).
Q2: Why is atmospheric lifetime important for GWP?
A: Atmospheric lifetime determines how long a greenhouse gas remains in the atmosphere and continues to contribute to warming. Longer-lived gases have higher GWPs.
Q3: What are typical CO2 reference values?
A: CO2 is used as the reference gas with a GWP of 1. The specific values used in calculations depend on the time horizon (usually 20, 100, or 500 years).
Q4: How does GWP vary for different greenhouse gases?
A: Different gases have vastly different GWPs. For example, methane has a GWP of about 28-36 over 100 years, while some fluorinated gases can have GWPs in the thousands.
Q5: What are the limitations of GWP?
A: GWP doesn't account for indirect effects, varies with time horizon, and may not fully capture the complex interactions between different greenhouse gases in the atmosphere.