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 unit mass pulse emission of a substance to that from CO₂.
The calculator uses the GWP formula:
Where:
Explanation: The calculator numerically integrates the radiative forcing curves using the trapezoidal rule and computes their ratio to determine GWP.
Details: GWP values are crucial for climate policy, emissions trading, and comparing the climate impacts of different greenhouse gases. They help prioritize mitigation efforts and assess the effectiveness of climate policies.
Tips: Enter comma-separated values for RF(t), RF_CO2(t), and corresponding time points. All arrays must have the same length and at least 2 values. The time values should be in consistent units (e.g., years).
Q1: What time horizon should I use for GWP calculation?
A: Common time horizons are 20, 100, and 500 years. The choice depends on the specific application and policy context.
Q2: How accurate is the trapezoidal integration method?
A: The trapezoidal rule provides good accuracy for most climate modeling applications, especially with sufficient data points.
Q3: What units should the radiative forcing values be in?
A: Radiative forcing is typically measured in watts per square meter (W/m²). The units must be consistent between RF(t) and RF_CO2(t).
Q4: Why is CO₂ used as the reference gas?
A: CO₂ is the most abundant anthropogenic greenhouse gas and serves as a convenient reference point for comparing other gases.
Q5: Can I calculate GWP for multiple gases simultaneously?
A: This calculator computes GWP for one gas relative to CO₂. For multiple gases, you would need to calculate each one separately.