Rwanda's Yearly Greenhouse Gas Emissions in CO₂ Equivalent

✨ Key Insights

Colonial Impact on Emissions

Rwanda's greenhouse gas emissions have been influenced by historical events, particularly during colonial times. The establishment of German colonial rule in 1897 and the subsequent Belgian mandate in 1924 led to significant land-use changes. The introduction of cash crops like coffee and tea resulted in deforestation and land conversion, contributing to increased CO₂ emissions. These agricultural shifts marked the beginning of a trend where land management practices significantly impacted Rwanda's emissions profile.

Post-Independence and Economic Development

Following Rwanda's independence in 1962, the nation embarked on development efforts that included agricultural expansion and infrastructure projects. These activities likely contributed to rising CO₂ emissions due to increased land clearing. The Rwandan Revolution in 1959 and the subsequent changes in land ownership also played a role in altering land-use patterns, further affecting emissions. The Vision 2020 development plan launched in 2000 aimed to transform Rwanda into a middle-income nation, which included expanding agriculture and infrastructure, likely increasing emissions through land-use change.

Modern Efforts Towards Sustainability

In recent years, Rwanda has made significant strides towards sustainability. The implementation of the Green Growth and Climate Resilience Strategy in 2011 and the commitment to the Paris Agreement in 2015 reflect the country's dedication to reducing greenhouse gas emissions. These initiatives focus on promoting renewable energy and reforestation, aiming to balance economic growth with environmental protection. Rwanda's updated Nationally Determined Contributions in 2019 further demonstrate its commitment to sustainable development and mitigating the impact of climate change on emissions.

Background

Greenhouse gas emissions from human activities are the main drivers of human-induced warming. In the scientific literature, human-induced emissions are often referred to as anthropogenic emissions.

CO₂ Fossil Fuels and Industry (CO₂ FFI)
CO₂ Land-Use, Land-Use Change and Forestry (CO₂ LULUCF)
Methane (CH₄)
Moderate: above 2.5 tonnes
Nitrous oxide (N₂O)
Fluorinated gases (F-gases)

Emissions from all different gases are expressed in CO₂-equivalent units to make it possible to compare the relative emissions from these different gases. CO₂-equivalents are calculated using the global warming potentials of the respective gases, in this case using a 100-year time horizon.

Wikipedia: Global Warming Potential

Total Historic Share

CO₂ From Fossil Fuels and Industry

The sources are mostly fossil-fuel combustion emissions from coal, oil, and gas, as well as emissions from industrial processes such as cement production. Cement also absorbs CO₂ out of the atmosphere through carbonation, which reduces emissions by about 0.8 Gt per year and is included here.

CO₂ From Land-Use, Land-Use Change, and Forestry

The main driver of these emissions is deforestation, which includes logging and forest degradation, as well as other land-use change activities. The emissions also take into account the absorption of CO₂ by processes that remove CO₂ from the atmosphere, such as afforestation and reforestation. It is the net effect that is indicated here.

Methane (CH₄)

Methane emissions are caused by human activities such as rearing livestock, agricultural practices, and fugitive fossil fuel emissions.

Nitrous Oxide (N₂O)

Common sources of these emissions are fossil fuel emissions and the agricultural use of synthetic fertilizer and manure.

Fluorinated Gases (F-gases)

Fluorinated gases are a group of gases defined by UNFCCC: hydrofluorocarbons (HFCs), perfluorocarbons (PFCs), sulfur hexafluoride (SF6), and nitrogen trifluoride (NF3). Fluorinated gases are also known as halogenated gases.

Wikipedia: Greenhouse Gas Emissions
IPCC: Annual Report 6, 5.2.1 5.2 Historical Trends, Variability and Budgets of CO₂, CH₄ and N₂O

Units and Measures

CO₂-equivalent 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

Climate Change Intelligence — Powered by You.

If you've found value in Climate Change Tracker, we'd really appreciate your donation. We rely on people like you to keep our platform running.

About the Data

The last available year in all the emission datasets is 2023. CO₂ emissions data is from the Global Carbon Project. It contains national CO₂ emissions from fossil sources and land-use change. Emissions from CH₄, N₂O and F-gases 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 generated using a large language model (LLM) using a structured approach to improve the accuracy. This included separating the context generation from the interpretation and narrative.

Data Sources

Global Carbon Budget 2024 Global Carbon Budget
Update cycle: yearlyDelay: ~ 10 months after the end of the year. Current year values are estimated and published in November.Credits: Friedlingstein et al., 2024, ESSD. Friedlingstein, P., O'Sullivan, M., Jones, M. W., Andrew, R. M., Hauck, J., Landschützer, P., Le Quéré, C., Li, H., Luijkx, I. T., Olsen, A., Peters, G. P., Peters, W., Pongratz, J., Schwingshackl, C., Sitch, S., Canadell, J. G., Ciais, P., Jackson, R. B., Alin, S. R., Arneth, A., Arora, V., Bates, N. R., Becker, M., Bellouin, N., Berghoff, C. F., Bittig, H. C., Bopp, L., Cadule, P., Campbell, K., Chamberlain, M. A., Chandra, N., Chevallier, F., Chini, L. P., Colligan, T., Decayeux, J., Djeutchouang, L., Dou, X., Duran Rojas, C., Enyo, K., Evans, W., Fay, A., Feely, R. A., Ford, D. J., Foster, A., Gasser, T., Gehlen, M., Gkritzalis, T., Grassi, G., Gregor, L., Gruber, N., Gürses, Ö., Harris, I., Hefner, M., Heinke, J., Hurtt, G. C., Iida, Y., Ilyina, T., Jacobson, A. R., Jain, A., Jarníková, T., Jersild, A., Jiang, F., Jin, Z., Kato, E., Keeling, R. F., Klein Goldewijk, K., Knauer, J., Korsbakken, J. I., Lauvset, S. K., Lefèvre, N., Liu, Z., Liu, J., Ma, L., Maksyutov, S., Marland, G., Mayot, N., McGuire, P., Metzl, N., Monacci, N. M., Morgan, E. J., Nakaoka, S.-I., Neill, C., Niwa, Y., Nützel, T., Olivier, L., Ono, T., Palmer, P. I., Pierrot, D., Qin, Z., Resplandy, L., Roobaert, A., Rosan, T. M., Rödenbeck, C., Schwinger, J., Smallman, T. L., Smith, S., Sospedra-Alfonso, R., Steinhoff, T., Sun, Q., Sutton, A. J., Séférian, R., Takao, S., Tatebe, H., Tian, H., Tilbrook, B., Torres, O., Tourigny, E., Tsujino, H., Tubiello, F., van der Werf, G., Wanninkhof, R., Wang, X., Yang, D., Yang, X., Yu, Z., Yuan, W., Yue, X., Zaehle, S., Zeng, N., and Zeng, J.: Global Carbon Budget 2024, Earth Syst. Sci. Data Discuss. [preprint], https://doi.org/10.5194/essd-2024-519, in review, 2024.

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.