🇦🇱 Albania's Sources of CH₄ Emissions

Albania's Sources of CH4 Emissions

Key Insights

2024 CH4 Emissions Profile

Albania's methane emissions in 2024 totalled around 2.15 megatonnes CO2e. Livestock dominated, at around 1.31 megatonnes CO2e (61.1%), followed by waste at 0.55 megatonnes CO2e (25.5%) and fugitive emissions at 0.22 megatonnes CO2e (10.5%). Over the ten years to 2024, livestock fell by around 0.124 megatonnes CO2e per year, while waste rose by roughly 0.010; fugitive emissions were broadly stable. Fuel fell by around 0.002 per year and crop emissions remained very small, edging down.

Historic Livestock Emissions

Livestock methane emissions began at around 0.35 megatonnes CO2e in 1851 and rose gradually to roughly 0.7 by the early 1930s. Growth then accelerated, reaching about 2.3 in 1987 and peaking at around 3.4 megatonnes CO2e in 1995. Emissions subsequently declined steadily, ending at approximately 1.31 megatonnes CO2e in 2024.

Historic Fugitive Emissions

Fugitive methane emissions were near zero through the late 1920s, then began to rise, briefly reaching around 0.23 megatonnes CO2e in 1949 before falling back. They increased strongly from the mid-1950s, peaking at roughly 1.76 megatonnes CO2e in 1983, then dropped sharply. Since the mid-1990s they have fluctuated at low levels, ending near 0.22 megatonnes CO2e in 2024.

Historic Waste Emissions

Waste methane emissions started at around 0.02 megatonnes CO2e in 1851 and increased gradually through the mid-twentieth century, reaching roughly 0.11 in 1958. They rose further to around 0.31 by 1980, then continued a slower long-term increase. Waste emissions reached their record high of approximately 0.55 megatonnes CO2e in 2024.

Historic Crop Emissions

Crop methane emissions began at about 0.006 megatonnes CO2e in 1851 and climbed through the twentieth century, peaking at roughly 0.054 megatonnes CO2e in 1970. They then declined to around 0.01 by the late 1990s. Since then, emissions have remained very low despite a brief rise during the 2000s, ending at around 0.008 megatonnes CO2e in 2024.

Historic Fuel Emissions

Fuel-combustion methane emissions began at around 0.22 megatonnes CO2e in 1851 and rose to approximately 0.42 by the early twentieth century. They peaked at roughly 0.44 megatonnes CO2e in 1942, then declined to around 0.17 by 1971. After a modest rebound and fluctuations around 1990, emissions fell again, reaching about 0.054 megatonnes CO2e in 2024.

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, Methane emissions in the atmosphere decay with an average lifetime of about 12 years so its long term warming-effect is much less compared to CO2 which stays on average for hundreds of years in the atmosphere. Meaning: Methane's short term warming effect is much higher, but long term warming effect is much lower. A reduction in emissions can cause a rapid decline in its atmospheric levels.

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

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About the Data

National methane emissions data through 2024 is from the PRIMAP-hist dataset, which combines several published sources into a historical emissions time series.

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 (1750-2024)
Update cycle: Every few monthsDelay: Less than 1 yearCredits: Gütschow, J.; Busch, D.; Pflüger, M. (2025): The PRIMAP-hist national historical emissions time series v2.7 (1750-2024). zenodo. doi:10.5281/zenodo.17090760

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