🇹🇿 United Republic of Tanzania's Sources of CH₄ Emissions

United Republic of Tanzania's Sources of CH4 Emissions

Key Insights

Methane’s Role And Scale

In the United Republic of Tanzania, methane accounts for around 40% of the country's warming impact. Emissions are dominated by livestock, contributing roughly two-thirds, with crop production adding about a sixth. Energy-related sources-fugitive emissions and fuel combustion-each form notable shares, while waste is smaller and other sources are negligible.

Livestock Drives Rapid Growth

From the post-war era to the early 2000s, livestock emissions rose steadily from low single-digit levels to around 20 megatonnes. Since the early 2000s they have accelerated sharply, nearly doubling to close to 40 today, making this by far the largest and fastest-growing component.

Energy And Waste Rising

Fugitive emissions climbed gradually through the late twentieth century and have risen more quickly since the mid‑1990s, reaching around 7 megatonnes today. Fuel combustion stayed modest until the mid‑1980s, then trended upward to roughly 6 megatonnes. Waste remained low for decades but has increased since around 2010 to just over 3. Crop production has also moved upward since the mid‑1980s, now in the high single digits.

Outlook And Near-Term Priorities

Most major sources are still rising, led by livestock, with continued increases in crop production and energy‑related methane (fugitive and fuel combustion), and waste also climbing from a smaller base. Reversing the growth in livestock first, while slowing energy and crop‑related increases, would deliver the biggest gains. Because methane's effect is short‑lived, cutting these emissions can reduce their warming impact relatively quickly.

Background

The chart shows a national breakdown by source of the yearly methane (CH4) emissions from human activities expressed as weight in megatonnes (Mt). In the scientific literature, these are referred to as anthropogenic emissions. Human-induced methane emissions increase atmospheric methane, which is warming the Earth. The sources of human methane emissions are

  • Livestock
  • Fugitive emissions from the fossil fuel industry
  • Crop production
  • Fossil fuel combustion
  • Waste management
  • Other processes

Methane's Global Warming Potential

Methane has a much higher Global Warming Potential (GWP) than CO2. However, the effect lasts only for a relatively brief period (9 years on average), compared to hundreds of years for CO2. A reduction in emissions can cause a rapid decline in its atmospheric levels and climate impact.

Livestock

Livestock emits methane that is produced in the animals' digestive system. Most methane is emitted from the mouth during rumination. A much smaller amount of methane is emitted from the manure. Depending on how the manure is managed, i.e., wet or dry, more methane is emitted. Wet management leads to higher methane emissions than dry management. However, dry management also emits nitrous oxide (N2O), which is another potent greenhouse gas.

Fugitive emissions from fossil fuel industry

Fugitive methane emissions are from the intentional and accidental release of methane, which happens during the extraction, storage, and transportation processes in the fossil fuel industry. Examples are methane leaks during oil and gas handling, storage, transport, incomplete combustion, and many more. Also, methane is deliberately ventilated from mines during the extraction of coal.


Methane is a primary part of “gas”, also called “natural gas” or “fossil gas”. Natural gas is used, for example, for heating and electricity generation, whereby it emits CO2 during the combustion process. However, when natural gas leaks (unburned) it contains a lot of fugitive methane emissions.

Waste

Waste from landfills and wastewater produces a lot of methane when biodegradable material breaks down without oxygen.

Crop production

Crop production emissions are largely from rice cultivation, which generates large amounts of methane during plant growth. These emissions are from flooded paddies, which create the swamp-like environment of rice fields. There are agricultural techniques to reduce emissions significantly, like periodic drainage and aeration. Rice is the main staple for about half the world's population, and its emissions are a significant part of total human methane emissions.

Fuel combustion

Fuel combustion emissions are mostly from the incomplete combustion of fossil fuels. As mentioned before, natural gas consists largely of methane, and when the combustion does not happen completely, methane enters the atmosphere.

Other

Other human-induced methane emissions include industrial processes and product uses.

Wikipedia: Anthropogenic Sources of Atmospheric Methane
IPCC: AR6, 5.2.2.2 Anthropogenic CH4 emissions

Units and Measures

CH4 emissions are expressed in the total weight in megatonnes per year. 1 Megatonne is equal to 1 million tonnes.

Wikipedia: Megatonne
Wikipedia: Global warming potential

About the Data

The last available year in all the emission datasets is 2023. Methane emissions come from the PRIMAP-Hist dataset. It is a rich dataset that combines several published sources to create a historical emissions time series for various greenhouse gases.

The Key Insights paragraph was created using a large language model (LLM) in combination with our data, historic events, and a structured approach for best accuracy by separating the context generation from the interpretation and narrative.

Data Sources

PRIMAP-hist The PRIMAP-hist national historical emissions time series (1750-2023)
Update cycle: Every few monthsDelay: Less than 1 yearCredits: Gütschow, Johannes; Busch, Daniel; Pflüger, Mika (2024): The PRIMAP-hist national historical emissions time series (1750-2023) v2.6. Zenodo.

Tanzania, the United Republic of's Sources of CH₄ Emissions