Wetlands & Drained Organic Soils Emission Factors
Peatlands and coastal wetlands hold some of the densest carbon stores on Earth. Left waterlogged they lock that carbon away; drain them for cropland, plantation or peat extraction and the exposed peat oxidises, turning a sink into a large, year-after-year source of CO₂, methane and nitrous oxide. Restoring the water table reverses most of the CO₂ loss — at the cost of more methane — and intact mangroves, marshes and seagrass keep banking “blue carbon” in their soils.
This page publishes the complete IPCC wetlands parameter set implemented in the GreenCalculus MasterBrain v2026.203 — 106 parameters covering the emission factors for drained and rewetted organic soils (CO₂, CH₄, N₂O and dissolved organic carbon) and the coastal blue-carbon biomass and soil parameters. It is a subset of the IPCC AFOLU Tier-1 emission factors dataset. These factors power the GreenCalculus Forestry & Coastal Removals calculator — see the methodology.
Draining peat soil is a large, ongoing annual emission: a hectare of drained boreal or temperate cropland loses about 29 t CO2 plus 13 kg N2O–N every year it stays drained. Rewetting turns the CO2 slightly negative but raises methane.
The IPCC wetlands model
The 2013 Wetlands Supplement treats organic soils by their water status. Drained soils emit CO₂ (peat oxidation), CH₄ (from ditches) and N₂O, plus dissolved organic carbon washed to water. Rewetted soils largely stop the CO₂ loss but emit more CH₄. Coastal wetlands are accounted like forests — a carbon stock in biomass and soil whose change on clearing or restoration is the emission or removal.
Annual emission = area × EF, summed per gas:
CO₂ = EFCO2–C × 44/12; N₂O = EFN2O–N × 44/28 × GWP; CH₄ CO₂e = EFCH4 × GWP. Rewetting nets a (usually negative) CO₂ factor against a positive CH₄ factor.
CO₂ factors are given as tonnes of CO₂–C (carbon) — multiply by 44/12 to get CO₂. N₂O factors are N₂O–N (nitrogen) — multiply by 44/28, then by the N₂O GWP (AR6 = 273). CH₄ is kg CH₄/ha/yr (biogenic GWP 27.9). A negative CO₂ factor (rewetted soils) is a removal. Drained-soil emissions recur every year the soil stays drained — they are not a one-off.
Drained organic soils
Draining a peatland exposes its stored carbon to oxidation, turning a natural sink into a large, sustained source. The emission factors give the annual CO₂ (as carbon), CH₄ from ditches, and N₂O per hectare, by land use and climate. CO₂ values are tonnes CO₂–C (multiply by 44/12); CH₄ is kg/ha/yr; N₂O is kg N₂O–N (multiply by 44/28), each then converted with a GWP.
Greenhouse-gas emission factors
| Parameter | Value | Unit |
|---|---|---|
| CH4 EF — Cropland drained (boreal_temperate) | 0 | kg CH4 per ha per yr |
| CO2 EF — Cropland drained (boreal_temperate) | 7.9 | tonnes CO2-C per ha per yr |
| N2O EF — Cropland drained (boreal_temperate) | 13 | kg N2O-N per ha per yr |
| N2O EF — Cropland drained except rice (tropical_subtropical) | 5 | kg N2O-N per ha per yr |
| CO2 EF — Cropland and fallow drained (tropical) | 14 | tonnes CO2-C per ha per yr |
| CO2 EF — Cropland drained, paddy rice (tropical) | 9.4 | tonnes CO2-C per ha per yr |
| CH4 EF — Cropland drained (tropical_subtropical) | 7 | kg CH4 per ha per yr |
| CH4 EF — Forest Land drained (temperate) | 2.5 | kg CH4 per ha per yr |
| CO2 EF — Forest Land drained (temperate) | 2.6 | tonnes CO2-C per ha per yr |
| N2O EF — Forest Land drained (temperate) | 2.8 | kg N2O-N per ha per yr |
| CO2 EF — Forest Land and cleared Forest Land (shrubland) drained (tropical) | 5.3 | tonnes CO2-C per ha per yr |
| CH4 EF — Forest Land and cleared Forest Land (shrubland) drained (tropical_subtropical) | 4.9 | kg CH4 per ha per yr |
| N2O EF — Forest Land and cleared Forest Land (shrubland) drained (tropical_subtropical) | 2.4 | kg N2O-N per ha per yr |
| CH4 EF — Forest Land drained nutrient-poor (boreal) | 7 | kg CH4 per ha per yr |
| CO2 EF — Forest Land drained nutrient-poor (boreal) | 0.25 | tonnes CO2-C per ha per yr |
| N2O EF — Forest Land drained nutrient-poor (boreal) | 0.22 | kg N2O-N per ha per yr |
| CH4 EF — Forest Land drained nutrient-rich (boreal) | 2 | kg CH4 per ha per yr |
| CO2 EF — Forest Land drained nutrient-rich (boreal) | 0.93 | tonnes CO2-C per ha per yr |
| N2O EF — Forest Land drained nutrient-rich (boreal) | 3.2 | kg N2O-N per ha per yr |
| CO2 EF — Forest Land drained shrubland nutrient-poor (boreal) | 0.37 | tonnes CO2-C per ha per yr |
| CH4 EF — Forest plantations drained (tropical_subtropical) | 2.7 | kg CH4 per ha per yr |
| CH4 EF — Grassland drained (boreal) | 1.4 | kg CH4 per ha per yr |
| CO2 EF — Grassland drained (boreal) | 5.7 | tonnes CO2-C per ha per yr |
| N2O EF — Grassland drained (boreal) | 9.5 | kg N2O-N per ha per yr |
| CH4 EF — Grassland deep-drained nutrient-rich (temperate) | 16 | kg CH4 per ha per yr |
| CO2 EF — Grassland deep-drained nutrient-rich (temperate) | 6.1 | tonnes CO2-C per ha per yr |
| N2O EF — Grassland deep-drained nutrient-rich (temperate) | 8.2 | kg N2O-N per ha per yr |
| CH4 EF — Grassland drained nutrient-poor (temperate) | 1.8 | kg CH4 per ha per yr |
| CO2 EF — Grassland drained nutrient-poor (temperate) | 5.3 | tonnes CO2-C per ha per yr |
| N2O EF — Grassland drained nutrient-poor (temperate) | 4.3 | kg N2O-N per ha per yr |
| CH4 EF — Grassland shallow-drained nutrient-rich (temperate) | 39 | kg CH4 per ha per yr |
| CO2 EF — Grassland shallow-drained nutrient-rich (temperate) | 3.6 | tonnes CO2-C per ha per yr |
| N2O EF — Grassland shallow-drained nutrient-rich (temperate) | 1.6 | kg N2O-N per ha per yr |
| CO2 EF — Grassland drained (tropical) | 9.6 | tonnes CO2-C per ha per yr |
| CH4 EF — Grassland drained (tropical_subtropical) | 7 | kg CH4 per ha per yr |
| N2O EF — Grassland drained (tropical_subtropical) | 5 | kg N2O-N per ha per yr |
| CH4 EF — Peat Extraction (boreal_temperate) | 6.1 | kg CH4 per ha per yr |
| CO2 EF — Peatland Managed for Extraction (boreal_temperate) | 2.8 | tonnes CO2-C per ha per yr |
| N2O EF — Peatland Managed for Extraction (boreal_temperate) | 0.3 | kg N2O-N per ha per yr |
| CO2 EF — Peatland Managed for Extraction (tropical) | 2 | tonnes CO2-C per ha per yr |
| N2O EF — Peatland Managed for Extraction (tropical_subtropical) | 3.6 | kg N2O-N per ha per yr |
| CO2 EF — Plantations drained, short rotations (acacia) (tropical) | 20 | tonnes CO2-C per ha per yr |
| CO2 EF — Plantations drained, oil palm (tropical) | 11 | tonnes CO2-C per ha per yr |
| CH4 EF — Plantation oil palm (tropical_subtropical) | 0 | kg CH4 per ha per yr |
| N2O EF — Plantation oil palm (tropical_subtropical) | 1.2 | kg N2O-N per ha per yr |
| CH4 EF — Plantation sago palm (tropical_subtropical) | 26.2 | kg CH4 per ha per yr |
| N2O EF — Plantation sago palm (tropical_subtropical) | 3.3 | kg N2O-N per ha per yr |
| CO2 EF — Plantations shallow-drained (sago palm) (tropical) | 1.5 | tonnes CO2-C per ha per yr |
| CO2 EF — Plantations drained, unknown or long rotations (tropical) | 15 | tonnes CO2-C per ha per yr |
| CH4 EF — Rice (tropical_subtropical) | 143.5 | kg CH4 per ha per yr |
| N2O EF — Rice (tropical_subtropical) | 0.4 | kg N2O-N per ha per yr |
Dissolved organic carbon (DOC)
| Parameter | Value | Unit |
|---|---|---|
| DOC flux natural — boreal | 0.08 | tonnes C per ha per yr (natural DOC flux) |
| EF DOC drained — boreal | 0.12 | tonnes C per ha per yr (DOC EF from drained organic soils) |
| Delta DOC drainage (global) | 0.6 | dimensionless (proportional increase from drainage) |
| Frac DOC CO2 (global) | 0.9 | dimensionless (fraction of DOC converted to CO2) |
| DOC flux natural — temperate | 0.21 | tonnes C per ha per yr (natural DOC flux) |
| EF DOC drained — temperate | 0.31 | tonnes C per ha per yr (DOC EF from drained organic soils) |
| DOC flux natural — tropical | 0.57 | tonnes C per ha per yr (natural DOC flux) |
| EF DOC drained — tropical | 0.82 | tonnes C per ha per yr (DOC EF from drained organic soils) |
Rewetted organic soils
Rewetting a drained peatland stops the CO₂ loss — the CO₂ factor turns slightly negative (a small removal) — but the returning anaerobic conditions raise methane. These factors give the trade-off by climate and nutrient status.
| Parameter | Value | Unit |
|---|---|---|
| CH4 EF rewetted — boreal poor | 41 | kg CH4 per ha per yr |
| CO2 EF rewetted — boreal poor | -0.34 | tonnes CO2-C per ha per yr |
| CH4 EF rewetted — boreal rich | 137 | kg CH4 per ha per yr |
| CO2 EF rewetted — boreal rich | -0.55 | tonnes CO2-C per ha per yr |
| CH4 EF rewetted — temperate poor | 92 | kg CH4 per ha per yr |
| CO2 EF rewetted — temperate poor | -0.23 | tonnes CO2-C per ha per yr |
| CH4 EF rewetted — temperate rich | 216 | kg CH4 per ha per yr |
| CO2 EF rewetted — temperate rich | 0.5 | tonnes CO2-C per ha per yr |
| CH4 EF rewetted — tropical all | 41 | kg CH4 per ha per yr |
| CO2 EF rewetted — tropical all | 0 | tonnes CO2-C per ha per yr |
Coastal wetlands (blue carbon)
Mangroves, tidal marshes and seagrass meadows — “blue carbon” ecosystems — store exceptional amounts of carbon in biomass and waterlogged soil. These parameters give the above-ground biomass stock and growth, carbon fraction, root-to-shoot ratio, dead wood and soil carbon used to estimate the carbon lost when they are cleared or the carbon gained when they are restored.
| Parameter | Value | Unit |
|---|---|---|
| AGB growth — mangrove Subtropical | 18.1 | tonnes dry matter per hectare per yr |
| AGB growth — mangrove Tropical Dry | 3.3 | tonnes dry matter per hectare per yr |
| AGB growth — mangrove Tropical Wet | 9.9 | tonnes dry matter per hectare per yr |
| AGB stock — mangrove Subtropical | 75 | tonnes dry matter per hectare |
| AGB stock — mangrove Tropical Dry | 92 | tonnes dry matter per hectare |
| AGB stock — mangrove Tropical Wet | 192 | tonnes dry matter per hectare |
| Carbon fraction — mangrove above-ground biomass | 45.1 | percent dry matter (carbon fraction of above-ground biomass) |
| Dead wood C stock — mangrove mature stand | 10.7 | tonnes C per hectare |
| Litter C stock — mangrove mature stand | 0.7 | tonnes C per hectare |
| Root-shoot ratio (R) — mangrove Subtropical | 0.96 | tonnes root d.m. per tonne shoot d.m. |
| Root-shoot ratio (R) — mangrove Tropical Dry | 0.29 | tonnes root d.m. per tonne shoot d.m. |
| Root-shoot ratio (R) — mangrove Tropical Wet | 0.49 | tonnes root d.m. per tonne shoot d.m. |
| Annual rewetting EF (EF_RESET) — Mangrove | -1.62 | tonnes CO2-C per ha per yr |
| Soil C stock — Mangrove (aggregated) | 386 | tonnes C per hectare |
| Soil C stock — Mangrove (mineral) | 286 | tonnes C per hectare |
| Soil C stock — Mangrove (organic) | 471 | tonnes C per hectare |
| Soil/sediment C accumulation rate — Mangrove, Subtropical | 1.62 | tonnes C per hectare per yr |
| Soil/sediment C accumulation rate — Mangrove, Tropical Dry | 1.62 | tonnes C per hectare per yr |
| Soil/sediment C accumulation rate — Mangrove, Tropical Wet | 1.62 | tonnes C per hectare per yr |
| Wood density — mangrove | 0.71 | tonnes per m3 (oven-dry wood density) |
| Root-shoot ratio (R) — seagrass Subtropical | 2.4 | tonnes root d.m. per tonne shoot d.m. |
| Root-shoot ratio (R) — seagrass Temperate | 1.3 | tonnes root d.m. per tonne shoot d.m. |
| Root-shoot ratio (R) — seagrass Tropical | 1.7 | tonnes root d.m. per tonne shoot d.m. |
| Annual rewetting EF (EF_RESET) — Seagrass meadow | 0.43 | tonnes CO2-C per ha per yr |
| Soil C stock — Seagrass meadow (mineral) | 108 | tonnes C per hectare |
| Soil/sediment C accumulation rate — Seagrass meadow | 0.43 | tonnes C per hectare per yr |
| Root-shoot ratio (R) — tidal marsh Mediterranean | 3.63 | tonnes root d.m. per tonne shoot d.m. |
| Root-shoot ratio (R) — tidal marsh Subtropical | 3.65 | tonnes root d.m. per tonne shoot d.m. |
| Root-shoot ratio (R) — tidal marsh Temperate | 2.11 | tonnes root d.m. per tonne shoot d.m. |
| Root-shoot ratio (R) — tidal marsh Temperate freshwater tidal | 1.15 | tonnes root d.m. per tonne shoot d.m. |
| Annual rewetting EF (EF_RESET) — Tidal marsh | 0.91 | tonnes CO2-C per ha per yr |
| Soil C stock — Tidal marsh (aggregated) | 255 | tonnes C per hectare |
| Soil C stock — Tidal marsh (aggregated organic+mineral, secondary value) | 255 | tonnes C per hectare |
| Soil C stock — Tidal marsh (mineral) | 226 | tonnes C per hectare |
| Soil C stock — Tidal marsh (organic) | 340 | tonnes C per hectare |
| Soil/sediment C accumulation rate — Tidal marsh | 0.91 | tonnes C per hectare per yr |
| Annual drainage EF (EF_FM) — tidal marshes and mangroves | 7.9 | tonnes CO2-C per ha per yr |
Application — formula & worked example
t CO₂e/ha/yr = EFCO2–C×44/12 + EFCH4×GWPCH4/1000 + EFN2O–N×44/28×GWPN2O/1000
Drained cropland on peat. One hectare of boreal/temperate cropland on drained organic soil: CO₂ EF 7.9 t CO₂–C → 7.9 × 44/12 = 29.0 t CO₂; N₂O EF 13 kg N₂O–N → 13 × 44/28 = 20.4 kg N₂O → ×273 = 5.6 t CO₂e; CH₄ negligible. Total ≈ 34.5 t CO₂e per hectare, every year the peat stays drained.
Rewetting the same land. Restoring the water table turns the CO₂ factor slightly negative (a small removal) but raises methane — for a boreal poor fen, CH₄ rises to ~41 kg/ha/yr (×27.9 ≈ 1.1 t CO₂e) against a CO₂ removal of about −1.2 t CO₂. The net lands near zero — a swing of roughly 34 t CO₂e/ha/yr versus leaving it drained, which is why peatland rewetting is such a high-leverage mitigation.
Framework requirements
Wetlands emissions are a Scope 1 emission (or removal) for the operation managing the land, and the Wetlands and organic-soil lines across the Agriculture and Land categories in national inventories.
| Framework | Role | Basis |
|---|---|---|
| IPCC 2006 National Inventories | Wetlands & organic soils (CRF 3B, 3D) | Parent framework (extended by the 2013 Supplement) |
| IPCC 2019 Refinement | Consolidated wetlands & organic-soil guidance | Refines the wetlands method |
| GHG Protocol Corporate Standard | Scope 1 (land management, drainage, restoration) | IPCC methods; GWP per latest assessment |
Common reporting errors
- Reporting CO₂–C as CO₂. The CO₂ factors are tonnes of carbon — multiply by 44/12 to get CO₂, or you understate by roughly two-thirds.
- Forgetting the 44/28 on N₂O. N₂O factors are N₂O–N (nitrogen); convert to N₂O before applying the GWP.
- Treating drained peat as a one-off. Drainage emissions recur every year the water table stays low — multiply by the number of years drained, not once.
- Ignoring the methane cost of rewetting. Rewetting stops the CO₂ loss but raises CH₄ — net the negative CO₂ factor against the positive CH₄ factor rather than claiming the CO₂ saving alone.
- Omitting ditch methane and DOC. Drained organic soils also emit CH₄ from drainage ditches and lose dissolved organic carbon to water — include both where the guidance requires.
- Confusing organic soils with mineral soils. These are peat (organic) soils; the mineral-soil carbon-stock-change factors in the land-use change dataset are a different method — don’t apply one to the other.
- Treating blue-carbon stocks as emissions. Coastal biomass and soil carbon are stocks; the emission or removal is the change on clearing or restoration.
- Using the wrong climate or land use. Factors vary strongly with climate zone, nutrient status and land use (cropland, plantation, peat extraction) — match them to the site.
Methodology, boundaries & uncertainty
What this dataset is. The IPCC wetlands parameter set — CO₂, CH₄, N₂O and dissolved-organic-carbon emission factors for drained and rewetted organic soils, and coastal blue-carbon biomass and soil parameters for mangroves, tidal marshes and seagrass — from the 2013 Supplement to the 2006 IPCC Guidelines: Wetlands, as implemented in the GreenCalculus MasterBrain. Part of the IPCC AFOLU Tier-1 dataset.
Boundary. Emissions and removals from organic (peat) soils under drainage and rewetting, and carbon stocks in coastal wetland ecosystems, reported in Scope 1. Mineral-soil carbon change is in the land-use change dataset; forest biomass in the forest-land dataset; managed-soils N₂O from mineral soils in the agricultural-soils dataset.
Rounding policy. Values are reproduced at IPCC precision. CO₂ and DOC factors are tonnes CO₂–C (or C) per hectare per year; CH₄ kg per hectare per year; N₂O kg N₂O–N per hectare per year; biomass stocks t dry matter or t C per hectare; ratios and fractions dimensionless.
Uncertainty. Wetland factors carry wide uncertainty — drainage CO₂ and CH₄ vary strongly with water-table depth, nutrient status and management, and coastal carbon stocks vary by region and species. Tier-1 defaults suit national and screening estimates; measured or region-specific values are expected where organic soils or coastal wetlands are a key category.
Applicability. Climate- and land-use-specific defaults; match the climate zone, nutrient status, land use and ecosystem, and use measured values where available.
Implementation & provenance chain
- Primary source — 2013 Supplement to the 2006 IPCC Guidelines for National Greenhouse Gas Inventories: Wetlands, Chapters 2 (drained inland organic soils), 3 (rewetted organic soils) and 4 (coastal wetlands).
- MasterBrain — each parameter is curated under a stable
afolu.wetlands.*key with its source reference and GHG scope/category; current version v2026.203 (2026-09-22). - REST & CSV — the
/afolu-wetlands-factorsendpoint projects these rows as JSON; the CSV button below serves the identical set. - Calculators — GreenCalculus land-sector tools read the same keys, so a published inventory and this page cannot diverge.
- Update plan — static reference; revalued on a new IPCC refinement to the wetlands method. Logged in the version history and bumps the dataset version.
Data access — REST API & CSV
The full 106-row dataset is available as a machine-readable REST endpoint and as a flat CSV download — the same rows shown above, versioned and citable.
Cache-Control: max-age=3600; X-GC-Version header signals dataset updates. /wp-json/greencalculus/v1/afolu-wetlands-factors
Click to generate ↓
Citation guidance
Cite the IPCC primary source. These factors are a subset of the GreenCalculus IPCC AFOLU Tier-1 dataset, which holds the citable DOI — cite the parent dataset, not a separate wetlands DOI.
IPCC (2014). 2013 Supplement to the 2006 IPCC Guidelines for National Greenhouse Gas Inventories: Wetlands (Hiraishi, T., et al., eds). Published by the IPCC, Switzerland.
IPCC 2013 Wetlands Supplement primary citation
Say, Jeremiah (2026). IPCC AFOLU Tier-1 emission factors (machine-readable). GreenCalculus. Zenodo. https://doi.org/10.5281/zenodo.20621658
Parent dataset DOI — includes the wetlands subset
Browse the full IPCC AFOLU Tier-1 emission factors dataset, of which this page is a part.
Frequently asked questions
Peat is partly-decomposed plant matter that has accumulated over thousands of years because waterlogging starves it of oxygen. Drain it and oxygen reaches the peat, so microbes resume decomposing it and release the stored carbon as CO₂ — year after year, for as long as the soil stays drained. That is why a single hectare of drained organic cropland can emit tens of tonnes of CO₂e annually, far more than most mineral-soil land uses.
CO₂–C is the mass of carbon in the emitted CO₂, not the mass of CO₂ itself. Because a CO₂ molecule (mass 44) contains one carbon atom (mass 12), you convert carbon mass to CO₂ mass by multiplying by 44/12 (≈ 3.667). The wetlands CO₂ factors are given in CO₂–C, so this conversion is essential before reporting.
Almost always, yes. Rewetting stops the large, sustained CO₂ loss from peat oxidation, and although the returning anaerobic conditions raise methane, the CO₂ saving is usually far larger than the methane penalty in CO₂e terms. Net the negative CO₂ factor against the positive CH₄ factor for the specific climate and nutrient status; for most drained peatlands the balance swings from tens of tonnes of CO₂e emitted per hectare per year to near zero.
Blue carbon is the carbon stored by coastal vegetated ecosystems — mangroves, tidal marshes and seagrass meadows. They accumulate carbon in both their biomass and, especially, their waterlogged soils, often at higher rates per hectare than terrestrial forest. The dataset provides the biomass stock and growth, carbon fraction, root-to-shoot ratio, dead wood and soil carbon needed to estimate the carbon lost when these ecosystems are cleared or the carbon gained when they are restored.
Apply the biogenic methane GWP (AR6 = 27.9) to CH₄ and the nitrous-oxide GWP (AR6 = 273) to N₂O, after converting N₂O–N to N₂O with 44/28. CO₂ needs no GWP but must be converted from CO₂–C with 44/12. Disclose whether you used AR5 or AR6, and keep it consistent across the whole inventory. See the IPCC AR6 GWP values dataset.
No. These are organic (peat) soils, whose carbon comes from the peat itself oxidising when drained — a direct emission factor per hectare per year. The agricultural-soils dataset covers mineral-soil carbon via reference stocks and stock-change factors, and managed-soils N₂O. They are different methods for different soil types; use the wetlands factors for organic soils.
The 2013 Supplement to the 2006 IPCC Guidelines for National Greenhouse Gas Inventories: Wetlands — a dedicated volume that filled the gaps in the 2006 Guidelines for drained and rewetted organic soils and coastal wetlands. Its methods were later consolidated into the 2019 Refinement. The factors on this page are the Tier-1 defaults from that Supplement.
No — it is a subset. The wetlands factors here are part of the GreenCalculus IPCC AFOLU Tier-1 emission factors dataset, which carries the single citable Zenodo DOI. This page presents the wetlands portion in full with its own machine-readable endpoint and CSV, but for citation you reference the parent AFOLU dataset DOI, not a separate wetlands DOI.
Version history
| Version | Date | MasterBrain | Summary |
|---|---|---|---|
| 1.0 | 2026-07-21 | v2026.59 | Initial publication. Complete IPCC 2013 Wetlands Supplement parameter set (106 parameters): drained and rewetted organic-soil emission factors (CO₂, CH₄, N₂O, DOC) and coastal blue-carbon biomass and soil parameters. Formula, worked example, framework mapping, 8-item FAQ, REST + CSV access. Subset of the IPCC AFOLU Tier-1 dataset. |
Explore the full AFOLU dataset
Wetlands is one part of the IPCC AFOLU Tier-1 emission factors — the parent dataset also covers enteric fermentation, manure management, agricultural soils, rice cultivation, land-use change, forest land and biomass burning, all with machine-readable access and the citable DOI.