CO2 Equivalent Calculators
0 calculators tagged with “CO2 Equivalent”
All Calculators
No calculators found for this topic.
CO₂e Formula
CO₂e = mass of GHG × GWP₁₀₀
GWP₁₀₀ values (IPCC AR6, 2021): CO₂ = 1 (reference); CH₄ (fossil) = 29.8; CH₄ (biogenic) = 27.9; N₂O = 273; HFC-134a = 1,530; SF₆ = 25,200.
Example: 10 kg CH₄ emission: CO₂e = 10 × 29.8 = 298 kg CO₂e. 1 kg N₂O: CO₂e = 1 × 273 = 273 kg CO₂e.
GWP Time Horizon
GWP depends on the time horizon used: GWP₂₀ (20-year): CH₄ = 82.5 — emphasizes near-term warming. GWP₁₀₀ (100-year): CH₄ = 29.8 — most commonly used in policy. GWP₅₀₀: lower CH₄ GWP (longer-lived gases like N₂O and CO₂ become relatively more important). Policy choice of GWP₁₀₀ vs. GWP₂₀ significantly affects how methane-heavy industries (natural gas, agriculture) compare to CO₂-heavy industries.
Sources by Gas
- CO₂: fossil fuel combustion (~75% of GHG), deforestation, cement production
- CH₄: natural gas leaks, rice paddies, ruminant livestock, landfills (~16%)
- N₂O: agricultural soils (fertilizer), livestock, wastewater (~6%)
- F-gases (HFCs, SF₆): refrigeration, electronics, power equipment (~2%)
Carbon Footprint
Personal, product, or organizational carbon footprint = Σ (activity × emission factor) in CO₂e. Global average personal footprint: ~4 t CO₂e/year; US average ~15 t; Paris Agreement compatible target: < 2.5 t by 2050.
Glossary
Frequently Asked Questions
CO₂ equivalent (CO₂e) expresses the warming effect of any greenhouse gas in terms of the equivalent mass of CO₂ that would produce the same warming over a specified time horizon (usually 100 years). It is needed because different GHGs have different warming efficiencies and atmospheric lifetimes: methane is ~30× more potent than CO₂ over 100 years but persists for ~12 years (vs. centuries for CO₂); nitrous oxide is ~273× more potent and persists for ~116 years. CO₂e allows all GHG emissions from different sources to be summed into a single comparable number for inventories, targets, and trading systems.
GWP₁₀₀ (IPCC AR6, 2021): CO₂ = 1 (by definition); methane CH₄ (fossil origin) = 29.8; methane CH₄ (biogenic/non-fossil) = 27.9; nitrous oxide N₂O = 273; HFC-134a = 1,530; HFC-32 = 771; SF₆ = 25,200; NF₃ = 17,400. To convert mass of gas to CO₂e: multiply by the GWP₁₀₀ value. Note: GWP values are updated with each IPCC assessment report as understanding of radiative forcing and atmospheric chemistry improves. Different values may appear in older documents (e.g., CH₄ GWP₁₀₀ was 25 in AR4, 28 in AR5, 29.8 in AR6).
Carbon footprint = Σ (activity data × emission factor) for all emission sources. Examples: Electricity: kWh used × grid emission factor (kg CO₂e/kWh). US average grid: ~0.42 kg CO₂e/kWh → 1,000 kWh = 420 kg CO₂e. Car driving: miles × fuel consumption × emission factor. Average US car: 0.404 kg CO₂e/mile → 10,000 miles/yr = 4,040 kg CO₂e. Flying: passenger-km × aviation emission factor (~0.133–0.255 kg CO₂e/pkm depending on class and contrail radiative forcing). Beef consumption: 1 kg beef ≈ 27–60 kg CO₂e (varies widely by production system). Sum all sources for total annual footprint in kg or tonnes CO₂e.
GWP at different time horizons reflects the cumulative warming effect over that period. GWP₂₀ (20-year): emphasizes near-term warming; methane GWP₂₀ ≈ 82.5 — much higher than GWP₁₀₀ because methane has strong near-term warming but is short-lived. GWP₁₀₀: the standard policy metric; methane GWP₁₀₀ ≈ 29.8. Policy implications: using GWP₂₀ makes methane-intensive industries (natural gas, agriculture, waste) appear far more harmful relative to CO₂-intensive industries (coal, cement). Climate scientists debate which horizon is more relevant: for meeting near-term temperature targets (1.5°C by 2050), GWP₂₀ may be more appropriate; for long-term warming commitment, GWP₁₀₀ is relevant. IPCC reports both but policy (UN Framework Convention, NDCs) predominantly uses GWP₁₀₀.