🇨🇺 Cuba's Sources of CH₄ Emissions

Cuba's Sources of CH4 Emissions

Key Insights

2024 CH4 Emissions Profile

Cuba's anthropogenic methane emissions totalled around 11.6 megatonnes CO2e in 2024. Livestock was largest, at about 6.3 megatonnes CO2e (54.5%), followed by waste at 4.5 megatonnes CO2e (38.6%); together they dominated emissions. Over the ten years to 2024, livestock fell by around 0.14 megatonnes CO2e per year and waste rose by 0.03. Crop, fugitive and fuel emissions were smaller and declining, at 0.3, 0.4 and 0.09 megatonnes CO2e respectively.

Historic Livestock Emissions

Livestock emissions rose from around 1.3 megatonnes CO2e in 1851 to roughly 11.8 megatonnes CO2e at their 1968 peak. They then declined to about 7.4 megatonnes CO2e by 2002, with a modest rebound around 2014, before falling to around 6.3 megatonnes CO2e in 2024.

Historic Fugitive Emissions

Fugitive emissions were negligible until around 1900, then reached about 0.25 megatonnes CO2e by 1904 and changed little for decades. They rose from the early 1970s, peaking at roughly 1.0 megatonnes CO2e in 1997, before declining to around 0.4 megatonnes CO2e in 2024.

Historic Waste Emissions

Waste emissions began at around 0.2 megatonnes CO2e in 1851 and increased steadily through the twentieth century, reaching roughly 3.5 megatonnes CO2e by 1982. Growth continued more gradually thereafter, and emissions reached their record high of around 4.5 megatonnes CO2e in 2024.

Historic Crop Emissions

Crop emissions started at about 0.2 megatonnes CO2e in 1851 and increased unevenly through the mid-twentieth century. They fluctuated between roughly 0.9 and 1.9 megatonnes CO2e from the 1970s, peaking in 1996, then fell sharply after 2013 to around 0.3 megatonnes CO2e in 2024.

Historic Fuel Emissions

Fuel emissions began near 3.8 megatonnes CO2e in 1851 and rose to a peak of roughly 11.3 megatonnes CO2e in 1944. They then dropped rapidly to around 1.0 megatonnes CO2e by 1963, remained low with some variation, and ended at about 0.09 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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