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Aviation impacts on climate: Where are we heading?
Kristian J. Walker (Physical Geography BSc) and Ling Lim (Research Fellow)
Figure 2: Aviation and background CO2 concentrations from various forecasts including the observed concentrations.
Introduction
The aim of the project was to review widely‐used aviation scenarios and assess the accuracy of earlier 
forecasts to reported levels of aviation emissions. For example, the IPCC Special Report on Aviation (IPCC, 
1999) provided forecasts from the base year of 1992 to ‘future’ years 2015 and 2050. We are now at a point 
in time, where we can compare  ‘old forecasts’ to reported traffic activities. This project also gave us the 
opportunity to identify where aviation emissions is heading. Therefore, we can determine not only the 
forecast  accuracy, but also the likely growth trajectory of aviation emissions. 
Aviation fuel burn
Generating forecasts for the aviation sector is a challenging task, since the industry can be heavily influenced 
by unpredictable world events such as war, disease outbreak or economic crisis.  An extensive literature 
review was conducted to obtain fuel burn data for various aviation scenarios. The data collected spanned the 
years 1970 to 2100. However, only two scenarios reached 2100, and thus, Table 1 demonstrates a snapshot of 
this extensive collection of data up to 2050.
Table 1: Selected global civil, military and total fuel burn for various inventories/scenarios. n.a. = not available 
Aviation carbon dioxide (CO2) emissions
A selection of aviation scenarios and their associated fuel burn were linearly interpolated between available 
data years, in order to obtain yearly fuel burn. These scenarios were: 
• NASA, CAEP‐4/FESG with data for 1992, 2015 and 2050  (IPCC, 1999)
• CONSAVE with data for 2000, 2020 and 2050  (Berghof et al., 2005)
• QUANTIFY with data for 2000, 2020 and 2050 (Owen et al., 2010)
• GIACC with data for 2006, 2012, 2016, 2020, 2025, 2026, 2036 and 2050 (ICAO, no date)
• Lee et al. (2013) with data for 2006 to 2050.
CO2 emissions for these datasets were calculated using a fuel to emissions conversion factor of 3150 g CO2
per kg fuel. The resulting CO2 emissions are illustrated in Figure 1. These aviation emissions were compared 
with those derived from the International Energy Agency (IEA) kerosene (IEA, 2014) (aviation fuel) sale data 
and the same fuel to emissions conversion factor as in the scenarios. These aviation trends were also 
compared with the various background scenarios for all anthropogenic sources, as shown in Figure 1. The 
background scenarios were obtained from various publications that contributed to the IPCC reports:
• RCP: RCP8.5 (Riahi et al., 2011), RCP3PD (van Vuuren et al., 2011)
• SRES: A1F1, B2 (IPCC, 2000)
• IS92: IS92e, IS92c (Leggett et al., 1992)
• WRE: WRE750, WRE350 (Wigley et al., 1996).
Figure 1: Aviation and background CO2 emissions from various forecasts including the IEA fuel (kerosene) sales data. The 
wedge of the scenario denotes the upper and lower ranges of the forecasts, with the upper/lower scenarios noted in 
brackets.
Aviation CO2 concentration
In order to calculate aviation CO2 concentrations (Figure 2), the aviation emissions scenarios from Figure 1 
and the historical aviation CO2 emissions derived from IEA fuel sales data were used as input in a simple 
climate model, LinClim. Historical background CO2 concentrations from Meinshausen et al. (2011) and future 
projections from RCP (2000‐2100), SRES (1970‐2100), IS92 (1995‐2100) and WRE (1991‐2100) are compared 
with the aviation concentrations in Figure 2. It shows that aviation's contribution to background CO2 increases 
with time. It can also be seen from the figure that  the rate of increase in aviation CO2 concentrations is 
greater than that of the background concentrations.
Aviation CO2 temperature response
In order to account for the non‐linearity effects of aviation CO2 concentrations on temperature, it was 
necessary to calculate the difference between background concentrations, and background without aviation 
concentrations. Therefore, the aviation scenarios are coupled to the relevant background (for example, Lee et 
al., 2013 with RCP background).  As for the climate parameters, those that reproduce the transient behaviour 
of the ECHAM4 General Circulation Model were used. The results from these LinClim simulations are 
demonstrated in Figure 3.
Figure 3: Aviation and background CO2 temperature response for a variety of forecasts.
Dissemination
The output from this work has been presented as a poster at the 4th International Conference on Transport, 
Atmosphere and Climate in Germany.  This will also be written‐up for the conference proceedings and special 
issue peer‐reviewed journal, Meteorologische Zeitschrift. In addition, the results will be presented to the 
International Civil Aviation Organization (ICAO)’s working groups and included in the Centre for Aviation, 
Transport and the Environment (CATE)’s research report for the UK Department for Transport (DfT).
What next?
This placement has provided the opportunity to put skills learnt during university into practice. As such, the 
Research, Enterprise and Innovation (REI) Summer Vacation Studentship has put into motion, my progression 
into the aviation sector and research. I plan on utilising this learning experience to apply skills developed 
during the studentship at a postgraduate level, whilst studying the MSc in Sustainable Aviation.
This work also forms part of a wider high profile research at MMU, which is conducted on behalf of the DfT, 
to assess and mitigate the climate impacts from aviation. The results from this study would be used to inform 
policy makers on whether mitigation efforts are likely to meet the targets set out back in the 1990s or 
whether more stringent legislations/policies are required to achieve them.
References
• Berghof R., Schmitt A., Eyers C., Haag K., Middel J., Hepting M., Grübler A. and Hancox R. (2005): CONSAVE 
2050 Final Technical Report. DLR, Köln, Germany.
• ICAO (no date): GIACC/4: IP/1, IP/2, IP/3. [Online] [Accessed on 15 June 2015] 
http://www.icao.int/environmental‐protection/_layouts/mobile/dispform.aspx?List=caa6919c‐f115‐4c3c‐
9586‐18f6015b43f6&View=8ff2ee57‐7d03‐4f91‐bfce‐6da44ff7365f&RootFolder=%2Fenvironmental‐
protection%2FGIACC%2FGiacc‐4&ID=8
• IEA (2014): Oil Information 2012. International Energy Agency, Paris.
• IPCC (1999): Aviation and the global atmosphere. In: Penner J.E., Lister D.H., Griggs D.J., Dokken D.J. and 
McFarland M. (Eds.), Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, 
UK.
• IPCC (2000): Special Report on Emissions Scenarios. In: Nakicenovic N. and Swart R. (Eds.), 
Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK. 
• Lee D.S., Lim L.L. and Owen B. (2013): Bridging the aviation CO2 emissions gap: why emissions trading is 
needed. Manchester Metropolitan University.
• Leggett J., Pepper W.J. and Swart R.J. (1992): Emissions scenarios for the IPCC: an update. In: Houghton J.T., 
Callander B.A., Varney S.K. (Eds.). Climate Change 1992: The supplementary report to the IPCC Scientific 
Assessment. Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK.
• Meinshausen M., Smith S.J., Calvin K., Daniel J.S., Kainuma M.L.T., Lamarque J‐F., Matsumoto K., Montzka
S.A., Raper S.C.B., Riahi K., Thomson A., Velders G.J.M. and van Vuuren D.P.P. (2011): The RCP greenhouse 
gas concentrations and their extensions from 1765 to 2300. Climatic Change, 109, pp 213‐241.
• Owen B., Lee D.S. and Lim L.L. (2010): Flying into the Future: Aviation Emissions Scenarios to 2050. Environ. 
Sci. Technol. 44, 2255‐2260.
• Riahi K., Rao S., Krey V., Cho C., Chirkov V., Fischer G., Kindermann G., Nakicenovic N. and Rafaj P. (2011): 
RCP8.5 – A scenario of comparatively high greenhouse gas emissions. Climatic Change, 109, pp 33‐57.
• van Vuuren D.P., Stechfest E., den Elzen M.G.J., Kram T., van Vliet J., Deetman S., Isaac M., Klein Goldewijk
K., Hof A., Mendoza Beltran A.,  Oostenrijk R. and van Ruijven B. (2011): RCP2.6: exploring the possibility to 
keep global mean temperature increase below 2°C. Climatic Change, 109, pp 95‐116). 
• Wigley T.M.L, Richels R. and Edmonds J.A. (1996): Economic and environmental choices in the stabilization 
of atmospheric CO2 concentrations. Nature, 379, 240‐243.
Acknowledgements
Kristian Walker is funded by the MMU Research, Enterprise & Innovation Summer Vacation Studentship and 
Ling Lim is funded by the UK Department for Transport. 
Centre for Aviation, Transport and the Environment (CATE)
School of Science & the Environment
Manchester Metropolitan University, United Kingdom

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Final poster

  • 1. Aviation impacts on climate: Where are we heading? Kristian J. Walker (Physical Geography BSc) and Ling Lim (Research Fellow) Figure 2: Aviation and background CO2 concentrations from various forecasts including the observed concentrations. Introduction The aim of the project was to review widely‐used aviation scenarios and assess the accuracy of earlier  forecasts to reported levels of aviation emissions. For example, the IPCC Special Report on Aviation (IPCC,  1999) provided forecasts from the base year of 1992 to ‘future’ years 2015 and 2050. We are now at a point  in time, where we can compare  ‘old forecasts’ to reported traffic activities. This project also gave us the  opportunity to identify where aviation emissions is heading. Therefore, we can determine not only the  forecast  accuracy, but also the likely growth trajectory of aviation emissions.  Aviation fuel burn Generating forecasts for the aviation sector is a challenging task, since the industry can be heavily influenced  by unpredictable world events such as war, disease outbreak or economic crisis.  An extensive literature  review was conducted to obtain fuel burn data for various aviation scenarios. The data collected spanned the  years 1970 to 2100. However, only two scenarios reached 2100, and thus, Table 1 demonstrates a snapshot of  this extensive collection of data up to 2050. Table 1: Selected global civil, military and total fuel burn for various inventories/scenarios. n.a. = not available  Aviation carbon dioxide (CO2) emissions A selection of aviation scenarios and their associated fuel burn were linearly interpolated between available  data years, in order to obtain yearly fuel burn. These scenarios were:  • NASA, CAEP‐4/FESG with data for 1992, 2015 and 2050  (IPCC, 1999) • CONSAVE with data for 2000, 2020 and 2050  (Berghof et al., 2005) • QUANTIFY with data for 2000, 2020 and 2050 (Owen et al., 2010) • GIACC with data for 2006, 2012, 2016, 2020, 2025, 2026, 2036 and 2050 (ICAO, no date) • Lee et al. (2013) with data for 2006 to 2050. CO2 emissions for these datasets were calculated using a fuel to emissions conversion factor of 3150 g CO2 per kg fuel. The resulting CO2 emissions are illustrated in Figure 1. These aviation emissions were compared  with those derived from the International Energy Agency (IEA) kerosene (IEA, 2014) (aviation fuel) sale data  and the same fuel to emissions conversion factor as in the scenarios. These aviation trends were also  compared with the various background scenarios for all anthropogenic sources, as shown in Figure 1. The  background scenarios were obtained from various publications that contributed to the IPCC reports: • RCP: RCP8.5 (Riahi et al., 2011), RCP3PD (van Vuuren et al., 2011) • SRES: A1F1, B2 (IPCC, 2000) • IS92: IS92e, IS92c (Leggett et al., 1992) • WRE: WRE750, WRE350 (Wigley et al., 1996). Figure 1: Aviation and background CO2 emissions from various forecasts including the IEA fuel (kerosene) sales data. The  wedge of the scenario denotes the upper and lower ranges of the forecasts, with the upper/lower scenarios noted in  brackets. Aviation CO2 concentration In order to calculate aviation CO2 concentrations (Figure 2), the aviation emissions scenarios from Figure 1  and the historical aviation CO2 emissions derived from IEA fuel sales data were used as input in a simple  climate model, LinClim. Historical background CO2 concentrations from Meinshausen et al. (2011) and future  projections from RCP (2000‐2100), SRES (1970‐2100), IS92 (1995‐2100) and WRE (1991‐2100) are compared  with the aviation concentrations in Figure 2. It shows that aviation's contribution to background CO2 increases  with time. It can also be seen from the figure that  the rate of increase in aviation CO2 concentrations is  greater than that of the background concentrations. Aviation CO2 temperature response In order to account for the non‐linearity effects of aviation CO2 concentrations on temperature, it was  necessary to calculate the difference between background concentrations, and background without aviation  concentrations. Therefore, the aviation scenarios are coupled to the relevant background (for example, Lee et  al., 2013 with RCP background).  As for the climate parameters, those that reproduce the transient behaviour  of the ECHAM4 General Circulation Model were used. The results from these LinClim simulations are  demonstrated in Figure 3. Figure 3: Aviation and background CO2 temperature response for a variety of forecasts. Dissemination The output from this work has been presented as a poster at the 4th International Conference on Transport,  Atmosphere and Climate in Germany.  This will also be written‐up for the conference proceedings and special  issue peer‐reviewed journal, Meteorologische Zeitschrift. In addition, the results will be presented to the  International Civil Aviation Organization (ICAO)’s working groups and included in the Centre for Aviation,  Transport and the Environment (CATE)’s research report for the UK Department for Transport (DfT). What next? This placement has provided the opportunity to put skills learnt during university into practice. As such, the  Research, Enterprise and Innovation (REI) Summer Vacation Studentship has put into motion, my progression  into the aviation sector and research. I plan on utilising this learning experience to apply skills developed  during the studentship at a postgraduate level, whilst studying the MSc in Sustainable Aviation. This work also forms part of a wider high profile research at MMU, which is conducted on behalf of the DfT,  to assess and mitigate the climate impacts from aviation. The results from this study would be used to inform  policy makers on whether mitigation efforts are likely to meet the targets set out back in the 1990s or  whether more stringent legislations/policies are required to achieve them. References • Berghof R., Schmitt A., Eyers C., Haag K., Middel J., Hepting M., Grübler A. and Hancox R. (2005): CONSAVE  2050 Final Technical Report. DLR, Köln, Germany. • ICAO (no date): GIACC/4: IP/1, IP/2, IP/3. [Online] [Accessed on 15 June 2015]  http://www.icao.int/environmental‐protection/_layouts/mobile/dispform.aspx?List=caa6919c‐f115‐4c3c‐ 9586‐18f6015b43f6&View=8ff2ee57‐7d03‐4f91‐bfce‐6da44ff7365f&RootFolder=%2Fenvironmental‐ protection%2FGIACC%2FGiacc‐4&ID=8 • IEA (2014): Oil Information 2012. International Energy Agency, Paris. • IPCC (1999): Aviation and the global atmosphere. In: Penner J.E., Lister D.H., Griggs D.J., Dokken D.J. and  McFarland M. (Eds.), Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge,  UK. • IPCC (2000): Special Report on Emissions Scenarios. In: Nakicenovic N. and Swart R. (Eds.),  Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK.  • Lee D.S., Lim L.L. and Owen B. (2013): Bridging the aviation CO2 emissions gap: why emissions trading is  needed. Manchester Metropolitan University. • Leggett J., Pepper W.J. and Swart R.J. (1992): Emissions scenarios for the IPCC: an update. In: Houghton J.T.,  Callander B.A., Varney S.K. (Eds.). Climate Change 1992: The supplementary report to the IPCC Scientific  Assessment. Intergovernmental Panel on Climate Change. Cambridge University Press, Cambridge, UK. • Meinshausen M., Smith S.J., Calvin K., Daniel J.S., Kainuma M.L.T., Lamarque J‐F., Matsumoto K., Montzka S.A., Raper S.C.B., Riahi K., Thomson A., Velders G.J.M. and van Vuuren D.P.P. (2011): The RCP greenhouse  gas concentrations and their extensions from 1765 to 2300. Climatic Change, 109, pp 213‐241. • Owen B., Lee D.S. and Lim L.L. (2010): Flying into the Future: Aviation Emissions Scenarios to 2050. Environ.  Sci. Technol. 44, 2255‐2260. • Riahi K., Rao S., Krey V., Cho C., Chirkov V., Fischer G., Kindermann G., Nakicenovic N. and Rafaj P. (2011):  RCP8.5 – A scenario of comparatively high greenhouse gas emissions. Climatic Change, 109, pp 33‐57. • van Vuuren D.P., Stechfest E., den Elzen M.G.J., Kram T., van Vliet J., Deetman S., Isaac M., Klein Goldewijk K., Hof A., Mendoza Beltran A.,  Oostenrijk R. and van Ruijven B. (2011): RCP2.6: exploring the possibility to  keep global mean temperature increase below 2°C. Climatic Change, 109, pp 95‐116).  • Wigley T.M.L, Richels R. and Edmonds J.A. (1996): Economic and environmental choices in the stabilization  of atmospheric CO2 concentrations. Nature, 379, 240‐243. Acknowledgements Kristian Walker is funded by the MMU Research, Enterprise & Innovation Summer Vacation Studentship and  Ling Lim is funded by the UK Department for Transport.  Centre for Aviation, Transport and the Environment (CATE) School of Science & the Environment Manchester Metropolitan University, United Kingdom