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Last reviewed September 2026
Authored by Jeremiah Say

Founder and Lead Systems Architect of GreenCalculus. Translates GHG Protocol methodology into high-precision JavaScript calculation engines. Architect of the MasterBrain data layer covering 16,686 sourced emission factors, aligned with IPCC AR6 and the GHG Protocol Corporate Standard.

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Wetlands & Drained Organic Soils Emission Factors

Wetlands and drained organic soils emission factors dataset: IPCC 2013 Wetlands Supplement — carbon dioxide, methane, nitrous oxide and dissolved-organic-carbon emission factors for drained and rewetted organic soils, plus coastal blue-carbon biomass and soil parameters for mangroves, tidal marshes and seagrass, 106 parameters. A subset of the IPCC AFOLU Tier-1 dataset. Source lineage from the IPCC Wetlands Supplement through the GreenCalculus MasterBrain and REST API/CSV to your wetlands carbon total.
MB v2026.203 · updated 22 Sep 2026

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.

Quick Answer

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.

SourceIPCC 2013 Wetlands Suppl.
Metrict CO₂–C / ha / yr
Parameters106 · 3 states
GC ImplementationMasterBrain v2026.203
Part ofAFOLU dataset (DOI)

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.

The calculation

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.

Read the units before you multiply

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

Drained organic soil emission factors (CO₂, CH₄, N₂O), by land use and climate IPCC 2013 Wetlands Supplement Ch.2 Tables 2.1–2.5
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)

Dissolved organic carbon flux and drainage emission factors IPCC 2013 Wetlands Supplement Ch.2 §2.2.2
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.

Rewetted organic soil emission factors (CO₂, CH₄), by climate and nutrient status IPCC 2013 Wetlands Supplement Ch.3
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.

Coastal wetland (blue carbon) biomass and soil carbon parameters, by ecosystem and climate IPCC 2013 Wetlands Supplement Ch.4
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

The calculation

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.

Where the wetlands factors apply
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

  1. 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.
  2. Forgetting the 44/28 on N₂O. N₂O factors are N₂O–N (nitrogen); convert to N₂O before applying the GWP.
  3. 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.
  4. 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.
  5. 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.
  6. 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.
  7. Treating blue-carbon stocks as emissions. Coastal biomass and soil carbon are stocks; the emission or removal is the change on clearing or restoration.
  8. 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

  1. 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).
  2. 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).
  3. REST & CSV — the /afolu-wetlands-factors endpoint projects these rows as JSON; the CSV button below serves the identical set.
  4. Calculators — GreenCalculus land-sector tools read the same keys, so a published inventory and this page cannot diverge.
  5. 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.

JSON — REST API
All 106 wetlands parameters with keys, values, units, gas, GHG scope/category and source references. Cache-Control: max-age=3600; X-GC-Version header signals dataset updates.

/wp-json/greencalculus/v1/afolu-wetlands-factors

Open API endpoint →

CSV — flat dataset
Flat CSV of all 106 rows (key, name, value, unit, gas, GHG scope/category, source, note) — ready for spreadsheet import.

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

Substantive revisions to this dataset reference page
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.

Primary source. IPCC (2014). 2013 Supplement to the 2006 IPCC Guidelines for National Greenhouse Gas Inventories: Wetlands (Hiraishi, T., et al., eds), Chapters 2–4. Published by the IPCC, Switzerland. Available via: ipcc-nggip.iges.or.jp. Licence: CC BY 4.0.

Reporting basis. CO₂ and DOC factors t CO₂–C/ha/yr (×44/12); N₂O kg N₂O–N/ha/yr (×44/28, then GWP); CH₄ kg/ha/yr (GWP). Drainage emissions recur annually; a negative CO₂ factor (rewetting) is a removal; coastal carbon is a stock whose change is the flux. Scope 1 land-management emissions.

GreenCalculus implementation. MasterBrain v2026.203 (2026-09-22). All 106 parameters reproduced cell-for-cell from the IPCC 2013 Wetlands Supplement, verified against the MasterBrain data layer by Jeremiah Say, July 2026. Part of the IPCC AFOLU Tier-1 dataset (DOI 10.5281/zenodo.20621658). Revalued on a new IPCC refinement.

Disclaimer. Published for reference and calculation. Convert CO₂–C and N₂O–N, count drainage emissions every year, net the rewetting methane against the CO₂ saving, and match the climate and land use before finalising your methodology.

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