File:Contrails Climate change atmos-chem-phys.net 19 8163 2019 acp-19-8163-2019-f02.jpg

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Français : Forçage radiatif dans les scénarios C2006-T06 (a), C2006-T50 (b), C2050-T50 (c) et C2050-T50M (d). Les encadrés (lignes continues) et les bandes de latitude (lignes en pointillés) indiquent les régions (définies à la section 2.3 de l’étude de L Bock & U Burkhardt, 2019) comparées sur les Fig. 3 et 4 de la même étude source :Lisa Bock & Ulrike Burkhardt (2019) Contrail cirrus radiative forcing for future air traffic ; | Atmos. Chem. Phys., vol 19, n°12 ; pp8163-8174 |URL :https://doi.org/10.5194/acp-19-8163-2019 |© cc-by-sa 4.0
English: Radiative forcing in scenarios C2006-T06 (a), C2006-T50 (b), C2050-T50 (c) and C2050-T50M (d). Boxes (solid lines) and latitude bands (dashed lines) indicate regions (defined in Sect. 2.3 of the study) which we compare in Figs. 3 and 4 of the same study (Lisa Bock & Ulrike Burkhardt (2019) Contrail cirrus radiative forcing for future air traffic ; | Atmos. Chem. Phys., vol 19, n°12 ; pp8163-8174 |URL :https://doi.org/10.5194/acp-19-8163-2019 |© cc-by-sa 4.0)
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Source Scientific paper : Lisa Bock & Ulrike Burkhardt (2019) Contrail cirrus radiative forcing for future air traffic ; | Atmos. Chem. Phys., vol 19, n°12 ; pp8163-8174 |URL :https://doi.org/10.5194/acp-19-8163-2019 |© cc-by-sa 4.0 License. |rem : les auteurs appartiennent à l’Institut für Physik der Atmosphäre, Oberpfaffenhofen et au Deutsches Zentrum für Luft- und Raumfahrt (Allemagne)|Reçu le 14 Dec 2018, discuté à partir du 25 Jan 2019, révisé le 17 May 2019 et accepté le 23 Mai 2019, puis publié le 27 Juin 2019
Author Lisa Bock & Ulrike Burkhardt
Other versions File:RF-Airtraffic-Acp-19-8163-2019-f02-C2006T06.jpg (only panel a))

The authors in their study have performed the following simulations:

  • a control simulation for the air traffic of 2006 (simulation C2006-T06)
  • a simulation with increased air traffic according to the AEDT projection of air traffic for the year 2050 (simulation C2006-T50)
  • a simulation that additionally accounts for a changed background climate in 2050 (simulation C2050-T50)
  • a simulation that considers additionally an increase in fuel and propulsion efficiency as well as a change in emissions connected with the use of renewable alternative fuel, in particular a reduction in soot emissions by 50 % and a slight increase in the water emission coefficient connected with the use of alternative fuels (simulation C2050-T50M).

Source : chap 3.4 Reduced soot emission and improvement in propulsion efficiency ; in Lisa Bock & Ulrike Burkhardt (2019) Contrail cirrus radiative forcing for future air traffic ; | Atmos. Chem. Phys., vol 19, n°12 ; pp8163-8174 |URL :https://doi.org/10.5194/acp-19-8163-2019 |© cc-by-sa 4.0

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