Journal of Atmospheric & Earth Sciences Category: Agriculture Type: Research Article

Analysis of annual CO2 gas emissions in West Africa

Marie Laurene Gonsan1, François-Xavier Djézia Bella Bouo1*, Réné Anoumou Tano1, Dro Touré Tiémoko1, Jacques Aka Adon1, Justin Koffi Kouamé2, Yao Tchétché1, Sylvain Djédjé Zézé1, Bafétigué Ouattara1, Yao Kramo1 and François N’doli Koffi1
1 Equipe de la Physique pour l'Environnement, Laboratoire de Physique Fondamentale et Appliquée, Université NANGUI ABROGOUA, 02 B.P. 801 Abidjan 02, Abidjan, Côte d'Ivoire, West africa
2 Département de Physique, Université de Man, B.P. 20 Man, Côte d'Ivoire, West africa

*Corresponding Author(s):
François-Xavier Djézia Bella Bouo
Equipe De La Physique Pour L'Environnement, Laboratoire De Physique Fondamentale Et Appliquée, Université NANGUI ABROGOUA, 02 B.P. 801 Abidjan 02, Abidjan, Côte D'Ivoire, West Africa
Email:bouobellafrancois@gmail.com

Received Date: Jul 25, 2023
Accepted Date: Aug 10, 2023
Published Date: Aug 17, 2023

Abstract

Temporal trends and variability of annual anthropogenic CO2 emissions in 16 West African countries over the 1970-2015 period are analyzed using EDGAR data. HUBERT segmentation methods and Empirical Modal Decomposition (EMD) were used to characterize the time-series of each country and detect breakpoints in anthropogenic emissions, respectively. This segmentation technique allowed us to observe that the number of breakpoints varies between 2 and 7, with unequal durations and intensities. However, the minimum and maximum numbers of these breakpoints are observed in the time series evolution of annual emissions in Nigeria (2), Niger (7) and Senegal (7). Results obtained by the EMD approach showed that the highest growth rate in anthropogenic CO2 emissions was obtained in Nigeria (1.812 kton.yr-1), while the lowest was observed in CaboVerde (0 kton.yr-1). These trends are correlate with the demographic and economic growth of these countries.

Keywords

Co2 Emissions Variability; Empirical Mode Decomposition Method; Segmentation method; West Africa

Introduction

The emission of greenhouse gases, particularly carbon dioxide (CO2), is one of the main contributors to climate change. CO2 emissions are mainly due to the use of fossil fuels and industrial production, and are constantly increasing at a global scale. West Africa is a developing region that is particularly vulnerable to the negative impacts of climate change [1], including drought, flooding and coastal erosion. In effect, during the 2000-2010 period, this region has lost 1.1% forest cover per year. In term of climate parameters, one observed an increasing of temperature from 0.2 to 0.8 C since the end of 1970s [1] and, a strong reduction of precipitation in the Sahel with a southward migration of 200 km of the isohyets. In additional, it estimated at 40 to 60% (15 to 30%) the decreasing of the annual averaging debit of the main rivers in West Africa [2]. Understanding CO2 emissions in this region is therefore crucial for developing effective mitigation and adaptation policies. However, estimating annual CO2 emissions in West Africa presents challenges due to variability and uncertainty in the available data [1] Several studies have been conducted to quantify CO2 emissions in West Africa [1,3-5]. For example, a recent study conducted by [3] used a combination of satellite data and models based on forest fires and agricultural practices to estimate CO2 emissions in the West African region. Results showed that forest fire emissions were highest in the arid Sahel regions, while agricultural emissions were more distributed across the region. Another study assessed CO2 emissions in urban areas in the West African region, focusing on emissions from road traffic. The results showed that CO2 emissions were concentrated in large cities such as Lagos, Abidjan and Accra [4]. Using long in situ time series of CO2 concentration of Lamto station (Côte d’Ivoire) [1], observed a strong seasonal and interannual variability of CO2 associated to the biomass fires regime and the large-scale circulation of air coming from North-east of the continent. These authors obtained an increasing rate of 7 ppm.yr-1 of CO2 concentration. This trend closes to the world trend, whilst this region is not classified as an important zone of CO2 emission. These innovate and appreciated results provide by these studies open several perspectives fields such as the quantification of the different CO2 emissions sources using time series at different timescales. This study aims to analyze CO2 emissions in 16 West African countries over a 46-year period from 1970 to 2015 using data provided by the Emissions Database for Global Atmospheric Research (EDGAR) [6]. We use two trend analysis methods, the segmentation method and the empirical mode decomposition method, to assess the temporal trends and variability of CO2 emissions in the region. In section 2, the study region, including its geography and the countries included in the analysis are described. Section 3 presents the data used in the study, including their source and temporal coverage. The trend analysis methods are presented in section 4. The results of analysis are presented in Section 5, followed by a discussion in Section 6. Finally, section 7 is devoted to conclusions, as well as avenues for future research.

Study Area

The area of interest covers West Africa. It extends in latitude from the Equator (0°N) to the South of Algeria (25°N) and in longitude from Senegal (20°W) to Cameroon (15°E). The 16 countries in the study area are: Benin, Burkina Faso, Cabo Verde, Côte d'Ivoire, Gambia, Ghana, Guinea, Guinea Bissau, Liberia, Mali, Mauritania, Niger, Nigeria, Sierra Leone, Senegal and Togo (Figure 1).

 Figure 1: Studyarea. Scale: 1/2500000

Data

The data consist of time series of annual inventory emissions of carbon dioxide (CO2) emissions from these 16 West African countries. They are provided by the Emissions Database for Global Atmospheric Research (EDGAR) [6] and span a period of forty-six years (from 1970 to 2015) at 0.1°x0.1° spatial and 1-year temporal resolutions [7]. These annual anthropogenic CO2 emissions are due to fossil fuel use and industrial processes (cement production, limestone and dolomite carbonate use, non-energy fuel use and other combustions, chemical and metal processes, solvents, agricultural liming and urea, waste and fossil fuel fires).Short-cycle biomass burning (such as agricultural waste burning), large-scale biomass burning (such as forest fires), and carbon emissions/removals related to land use, land-use change, and forestry are excluded.

Trend Analysis Method

We use the segmentation of [8] to detect the presence or absence of one or more break points in the inter annual behavior of the time series constituted by the annual anthropogenic carbon dioxide (CO2) emissions released into the atmosphere in the different countries of the study area. The temporal evolution of annual CO2 emissions can sometimes include breakpoints that express changes in the regime of this parameter. These changes clearly show an increase or decrease in emission intensity from one period to another. To highlight these likely changes in the year-to-date (YTD) CO2 emissions, Hubert's statistical test or segmentation [8] was applied to the time series of each country. This technique allows the initial series to be broken down into two or more-time sub-series and to highlight the presence or absence of one or more breakpoints characteristic of probable changes in the regime of the parameter studied. The YTD time series of CO2 emissions analyzed may also exhibit trends. To characterize these trends, the method based on empirical modal decomposition (EMD) [9] was applied to the time series of each country. This method decomposes the original signal into a finite number of intrinsic mode functions (IMF) with different time scales, and the trend function with at most one extremum corresponds to the last intrinsic function. This intrinsic trend corresponds here to the instantaneous rate of change of emissions in kton CO2 per year (kton.yr-1). The EMD method provides a better estimate of the trend than the conventional linear regression technique [9].

Results

The temporal analysis of the annual CO2 gas emissions exhibits several changes in interannual variability in some countries during the study period. These changes which are characterized by some breakpoint obtained by Hubert segmentation statistical test [8] (have unequal durations and intensities (Table 1). The number these breakpoints ranged between 2 and 7. The minimum and maximum numbers of breakpoint are observed in Nigeria (2), and Niger (7) and Senegal (7) annual CO2 gas emissions time series evolution respectively. The first and the main breakpoints occur in 1972 in Nigeria and around the 1990s in all West Africa countries. The periodicity of the appearance of these breakpoints ranged between 1 and 25 years. Negative trends have been observed in Cabo Verde (-132.84%), Liberia (-145.06%), and Sierra Leone (-26.56%) before and after 1981, 1989 and1991, respectively. These values show a reduction of CO2 emissions in these countries. Positive trends that signify an increase of CO2 gas emissions have been observed in the other West African countries with varying intensity and duration from one country to another. The strongest trends of relatively short durations are generally observed in the 1970s. The maximum positive trend value has been recorded in Mauritania before and after the 1991s (Table 1).

Country

Breakpoint year

Mean value before breakpoint

Mean value after breakpoint

Rate of CO2 gas emissions (%)

Benin

1995

446.238

1293.375

65.49

 

1999

1293.375

1841.733

29.77

 

2002

1841.733

2582.367

28.68

 

2005

2582.367

4198.4

38.49

 

2008

4198.4

4992.233

15.9

 

2011

4992.233

5654.275

11.71

Burkina Faso

1978

491.456

660. 556

25,60

 

1987

660.556

852. 233

22.5

 

1993

852.233

1219.718

30.14

 

2004

1219.718

1520.6

19.79

 

2007

1520.6

2012.167

24.43

 

2010

2012.167

2271.82

11.43

Cabo Verde

1975

45.817

82.833

44.69

 

1978

82.833

111.167

25.49

 

1981

111.167

47.744

-132.84

 

1999

47.744

73.64

35.16

 

2009

73.64

93.9

21.58

Cote d’Ivoire

1995

3377.289

5057.733

33.22

 

1998

5057.733

6479.582

21.94

 

2009

6479.582

7711.85

15.98

 

2013

7711.85

9544.85

19.2

Gambia

1976

41.929

78.51

46.59

 

1986

78.51

111.7

29.71

 

1996

111.7

138.8

19.52

 

2000

138.8

168.683

17.71

 

2006

168.683

207.125

18.56

 

2010

207.125

242.44

14.56

Ghana

1981

2676.159

3961.017

32.44

 

1997

3961.017

6803.463

41.78

 

2005

6803.463

8859.125

23.2

 

2009

8859.125

11872.75

25.38

 

2011

11872.75

14337.85

17.19

Guinea

1978

650.478

900.038

27.73

 

1986

900.038

1169.808

23.06

 

1998

1169.808

1426.489

17.99

 

2007

1426.489

1694.033

15.79

 

2010

1694.033

1951.48

13.19

Bissau Guinea

1978

43.489

79.333

45.18

 

1987

79.333

154.059

48.5

 

1996

154.059

180.85

14.81

 

2002

180.85

218.025

17.05

 

2006

218.025

262.225

16.86

 

2010

262.225

304.42

13.86

Liberia

1974

342.98

614.7

44.2

 

1978

614.7

838.545

26.69

 

1989

838.545

342.173

-145.06

 

2000

342.173

556.578

38.52

 

2009

556.578

757.167

26.49

Mali

1976

297.986

464.1

35.79

 

1986

464.06

586.086

20.82

 

1993

586.086

929.578

36.95

 

2002

929.578

1076.325

13.63

 

2006

1076.325

1294.025

16.82

 

2010

1294.025

1530.9

15.47

Mauritania

1978

202.667

429.846

52.85

 

1991

429.846

1141.778

62.35

 

2000

1141.778

1508

24.28

 

2005

1508

1995.6

24.43

 

2010

1995.6

2414.8

17.35

Niger

1978

366.133

649.037

43.58

 

1986

649.037

873.99

25.74

 

1996

873.99

1133.867

22.92

 

2002

1133.867

1377.475

17.68

 

2006

1377.475

1612.533

14.57

 

2009

1612.533

1866.9

13.62

 

2012

1866.9

2138.067

12.68

Nigeria

1972

37882.1

68801.832

44.94

 

1991

68801.832

83971.371

18.06

Senegal

1975

1511.367

2175.563

30.53

 

1991

2175.563

2780.25

21.75

 

1997

2780.25

3896

28.64

 

2000

3896

4780.95

18.5

 

2004

4780.95

5913.25

19.14

 

2008

5913.25

7051.025

16.13

 

2012

7051.025

8021.567

12.1

Sierra Leone

1978

394.233

592.875

33.5

 

1986

592.875

809.02

26.72

 

1991

809.02

639.256

-26.56

 

2000

639.256

822.04

22.24

 

2005

822.04

991.85

17.12

 

2009

991.85

1193.85

16.92

Togo

1985

432.544

653.44

33.8

 

1995

653.44

1003.2

34.86

 

1998

1003.2

1269

20.94

 

2007

1269

1662.133

23.65

 

2010

1662.133

2249.32

26.11

Table 1: Summary of annual CO2emissions breakpoint year obtained by segmentation method and associated rate of COgasemissions in West African countries.

Country

Trend

Burkina Faso

0.112

Niger

0.103

Mali

0.075

Mauritania

0.146

Senegal

0.210

Bissau Guinea

0.017

Cabo Verde

0

Guinea

0.083

Sierra Leone

0.035

Gambia

0.013

Liberia

0.003

Cote d’Ivoire

0.335

Ghana

0.689

Togo

0.112

Benin

0.125

Nigeria

1.812

Table 2 : Linear trend with slopes in kton CO2 per year.

The maximum (~1.812kton. yr-1) and minimum (~0kton. yr-1) trends are observed in Nigeria and Cabo Verde, respectively.The upward linear trend shows the increasing CO2 gas emissions in all West African countries over the 1970-2015 period.

Figure 2 : Intern annual variability of annual CO2gasemissions in kton.yr-1 in West African countries. The linear trend (in red) obtained by EMD was added on each figure.

Discussion

Temporal trends in annual anthropogenic CO2 emissions were analysed during the 1970-2015 period over the 16 West African countries. The results for each country indicated that CO2 emissions exhibited a high annual variability with an increasing trend. Nigeria, Côte d'Ivoire, Ghana and Senegal have the highest CO2emission values (>1340 Kton) with rates of 12.10%, respectively. These high values are probably due to the increase in anthropogenic activities associated with population and economic growth in these countries. Similar trends are also observed in the study of [10] over the 1960-2010 period in 39 African countries. In fact, these four countries (i.e., Nigeria, Côte d'Ivoire, Ghana and Senegal) are the most industrialised and highly populated in West Africa with population growth rates of 2.63%, 3.26%, 2.62% and 2.65% per year respectively during the 45 years [11]. This is corresponding to a population increase of roughly 231%, 330%, 226% and 220% respectively over the 1970-2015 period, which is of the same order of magnitude as the increase in bio fuel emissions. Moreover [12,13], highlighted that bio fuel emissions have increased at a higher rate than other sources due to an increase in low-income population in sub-Saharan Africa, where biomass constitutes about 80% of the total energy consumption. In addition, results of this study corroborate those of [14] on carbon emissions between 1990 and 2019 in West Africa. These authors showed that the regional net warming potential between 1990 and 2019 was estimated to be 11.44 Pg and Nigeria had the highest potential at 18.7%, closely followed by Mali and Ghana at 15% and 13.2%, respectively. Similarly, using Kaya identity, [15] indicated that the largest CO2 emitters in West Africa in 2017 were respectively Nigeria (86 MtCO2), Ghana (14 MtCO2), Cote d’Ivoire (10.2 MtCO2) and Senegal (8.5 MtCO2), in agreement to our results. The authors explained this result by many factors, including GDP. In fact, they noted that countries with high CO2 emissions per capita also have high GDP per capita. Our results showed that anthropogenic CO2 emissions increased significantly in 32% of the countries of the West African sub-region in agreement with GDP per capita in the same period [16] arrived at the same conclusion for other regions. These authors highlighted that in South Africa, between 1994 and 2019, CO2gasemissions levels were generally correlated with economic growth. Furthermore, in Africa, many studies have concluded that pollutant emissions are increasing [1,12,16]. In the present study, trends of CO2emissions are in the same order of magnitude compared to those obtained for the other pollutants (i.e., BC, OC, NOx, CO, SO2 and NMVOCs) in different African regions. For example, [12] showed that all pollutant emissions are globally increasing in Africa during the period 1990-2015 with a growth rate of 95%, 86%, 113%, 112%, 97% and 130% for BC, OC, NOx, CO, SO2 and NMVOCs, respectively. These authors also pointed out that West Africa is the highest emitting region for some pollutants such as CO, mainly due to domestic fires and traffic activities. CO is an atmospheric pollutant that is emitted mainly from anthropogenic sources [17]. It was reported that many processes that emit CO also emit CO2, and therefore knowledge of CO emission rates can provide additional information on CO2 emissions [18,19] The work of [1] using atmospheric concentrations of CO2 and the tracer CO measured continuously at Lamto showed that both compounds had strong similarities between their seasonal cycles and similar emission sources as well as high and very significant correlation values depending on the time of year and concluded that the trend of CO partly explains that of CO2. Therefore, in this study different trends of CO2 by country are not surprising since the values of CO2 obtained in some regions of West Africa from direct measurements are very high compared to those in other regions of the world.

Unlike the four countries mentioned above, Cabo Verde, Gambia, Guinea Bissau and Liberia showed lower levels of CO2 emissions and a reduction in CO2 emissions for particular years (Table 2), indicating a low level of industrialisation in these countries [20] . Furthermore, for many years, most tropical countries such as Ghana [21] and Côte d'Ivoire [5] have considered themselves as being net carbon sinks or, at worst, carbon neutral. This assertion is based on the relatively low level of industrialisation in these countries. But given the intensification of industrial processes and the use of fossil fuels, it is conceivable that their CO2 emissions will increase significantly as indicated by the upward trends (in red) observed in long-term change in temporal evolution CO2 gas emission in each West African country (Figure 2).

Conclusion

Anthropogenic CO2 emissions in 16 West African countries over a 46-year period from 1970 to 2015 were analyzed on an annual scale using EDGAR data. The results show that CO2 emissions exhibit high annual variability for each country. Furthermore, the results have shown that CO2 emissions have increased significantly in 32% of West African sub-region countries, in agreement with GDP per capita over the same period in these countries. Nigeria, Côte d'Ivoire, Ghana and Senegal presented the highest CO2 emission values (> 1340 kton) associated with strong upward trends. In contrast, CaboVerde, Gambia, Guinea-Bissau and Liberia showed the lowest emission levels with reductions in specific years. Statistical analysis using the HUBERT segmentation method highlighted the different breakpoints and their duration in the CO2 emissions time series of each of these 16 countries. The application of this method enabled us to identify that the breakpoints in the various time series are in the interval [2,7]  indicating several regime changes in CO2 emissions. However, the time series observed in Gambia (2 points) shows the lowest number of breakpoints, where Senegal and Nigeria (7 points) show the highest number of breakpoints. Furthermore, EDGAR data used here are based on inventories, statistical models and generated knowledge, presenting sometimes very large uncertainties throughout the African region due to the scarcity of quality data. This can underestimate and/or overestimate the sources and trends of CO2 in particular and GHGs in general in the region. Thus, to reduce uncertainties, an extensive network of GHG measurements in Africa is a privileged observable that can both help diagnose the impact of human activities and help model the various components of the carbon cycle.

Acknowledgements

The authors thank the Emissions Database for Global Atmospheric Research (EDGAR) which provided us with high-quality data.

References

  1. Tiemoko TD, Ramonet M, Yoroba F, Kouassi KB, Kouadio K, et al. (2021) Analysis of the temporal variability of CO2, CH4 and CO concentrations in West Africa. Tellus B. Chem. Phys. Meteorology 73: 1-24.
  2. Niasse M (2004) Prévenir les conflits et promouvoir la coopération dans la gestion des fleuves transfrontaliers en Afrique de l’Ouest. Vertigo 5: 1‌-22‌.
  3. Gast LF, Gash JHC, Elbers AFA, Jongen M, Kruijt FAM, et al. (2019) Spatial and temporal patterns of CO2 and CH4 fluxes from the African equatorial rainforest in Cameroon. Bio geosciences 16: 3567-3588.
  4. Agbejule A, Ogunseitan OS, Obokoh LO (2020) Analysis of carbon dioxide emission and economic growth in Nigeria. International Journal of Energy Economics and Policy 10: 364-369.
  5. Tiemoko DT, Yoroba F, Diawara A, Kouadio K, Kouassi BK, et al. (2020) Understanding the Local Carbon Fluxes Variations and Their Relationship to Climate Conditions in a Sub-Humid Savannah-Ecosystem during 2008-2015 : Case of Lamto in Cote d’Ivoire. ACS 10: 186-205.
  6. EDGAR (2016) European Commission, Joint Research Centre (JRC)/PBL Netherlands Environmental Assessment Agency. Emission Database for Global Atmospheric Research (EDGAR), Europe.
  7. Olivier JGJ, Janssens-Maenhout G, Muntean M, Peters JAHW (2016) Trends in global CO2 emissions: 2016 Report. European Commission, Joint Research Centre (JRC), Directorate C - Energy, Transport and Climate; PBL Netherlands Environmental Assessment Agency the Hague 1-86.
  8. Hubert P, Carbonnel JP, Ali C (1989) Segmentation des séries hydrométriques. Application à des séries de précipitations et de débits de l’Afrique de l’Ouest. Journal of hydrology 110: 349-367.
  9. Wu Z, Huang NE, Long SR, Peng CK (2007) On the trend, detrending, and the variability of nonlinear and nonstationary time series. Proceedings of the National Academy of Sciences 104: 14889-14894.
  10. Sakiru AS (2014) Convergence of CO2 emission levels: Evidence from African countries. Journal of Economic Research 19: 65-92.
  11. Banquemondiale (2022) Indicateurs du développementdans le monde. DataBank, France.
  12. Keita S, Liousse C, Assamoi EM, Doumbia T, N'Datchoh ET, et al. (2021) African anthropogenic emissions inventory for gases and particles from 1990 to 2015. Earth Syst. Sci. Data 13: 3691-3705.
  13. Ozturk I, Bilgili F (2015) Economic growth and biomass consumption nexus: Dynamic panel analysis for Sub-Sahara African Countries. Appl. Energy 137: 110-116.
  14. Abdulraheem KA, Adeniran JA, Aremu AS (2022) Carbon and precursor gases emission from forest and non-forest land sources in West Africa. Int. J. Environ. Sci. Technology 19: 12003-12018.
  15. Ayompe LM, Davis SJ, Egoh BN (2020) Trends and drivers of African fossil fuel CO2 emissions 1990–2017. Environ. Research Letters 15: 124039.
  16. Shikwambana L, Mhangara P, Kganyago M (2021) Assessing the Relationship between Economic Growth and Emissions Levels in South Africa between 1994 and 2019. Sustainability 13: 1-15.
  17. Zhong Q, Huang Y, Shen H, Chen Y, Chen H, et al. (2017) Global estimates of carbon monoxide emissions from 1960 to 2013. Environ. Sci. Pollution Res 24: 864-873.
  18. Wu D, Liu J, Wennberg PO, Palmer PI, Nelson RR, et al. (2022) Towards sector-based attribution using intra-city variations in satellite-based emission ratios between CO2 and CO. Atmos. Chem. Phys. 22: 14547-14570.
  19. Park H, Jeong S, Park H, Labzovskii LD, Bowman KW (2021) An assessment of emission characteristics of Northern Hemisphere cities using spaceborne observations of CO2, CO, and NO2. Remote Sens. Environ 254: 1-12.
  20. CEDEAO (2010) Politiqueindustrielle commune de l’Afrique de l’Ouest. CEDEAO 1-77.
  21. Dilys SM, Robert BZ, Pierre BIA, Eric K, Patrice S, et al. (2018) Assessment of Greenhouse Gas Emissions from Different Land-Use Systems: A Case Study of CO2 in the Southern Zone of Ghana. Applied and Environmental Soil Science 2018: 1-12.

Citation: Gonsan ML, Bouo FXDB, Tano RA, Tiemoko DT, Adon JA, et al. (2023) Analysis of annual CO2 gas emissions in West Africa. J Atmos Earth Sci 7: 038.

Copyright: © 2023  Marie Laurene Gonsan, et al. This is an open-access article distributed under the terms of the Creative Commons Attribution License, which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.


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