23. January 2019

Cli­mate mod­el shows that clean­er air­craft emis­sions re­duce the cli­mate im­pact of con­trail cir­rus

Contrail cirrus in the sky
Con­trail cir­rus in the sky
Image 1/2, Credit: DLR (CC-BY 3.0).

Contrail cirrus in the sky

Air­craft en­gines emit soot par­ti­cles. These act as con­den­sa­tion nu­clei for small, su­per­cooled rain­drops that freeze im­me­di­ate­ly to form ice crys­tals that are vis­i­ble in the sky as con­trails.
Reduced effect of contrail cirrus
Re­duced ef­fect of con­trail cir­rus
Image 2/2, Credit: DLR (CC-BY 3.0).

Reduced effect of contrail cirrus

Re­duc­tion of the warm­ing ef­fect of con­trail cir­rus (in mil­li­watts per square me­tre [mW/m2) due to an 80 per­cent re­duc­tion in ice crys­tal for­ma­tion in con­trails. Shad­ed ar­eas show sta­tis­ti­cal­ly sig­nif­i­cant changes us­ing a 95 per­cent sig­nif­i­cance lev­el.
  • Contrail cirrus clouds have a similar climate impact to carbon dioxide emissions from aviation.
  • Fewer ice crystals reduce the optical thickness of contrail cirrus and also shorten their lifetime.
  • Focus: Aviation, climate change

Fewer soot particles in the exhaust stream of aircraft reduces the formation of ice crystals and therefore the climate impact of the resulting contrail cirrus. Halving the ice particles that form in the contrail decreases the climate-warming effect of the contrail cirrus by 20 percent. The effect is halved if there are 80 percent fewer ice crystals. This is shown in a study conducted by the German Aerospace Center (Deutsches Zentrum für Luft- und Raumfahrt; DLR), the results of which have been published in the Nature Partner Journal (npj) Climate and Atmospheric Science.

"In our theoretical estimates, we found that a significant reduction in soot emissions is required to reduce the climate impact of contrails effectively," explains Ulrike Burkhardt from the DLR Institute of Atmospheric Physics in Oberpfaffenhofen. "Research into low-soot engines and alternative fuels to counteract the climate impact of aviation is worthwhile, as contrail cirrus today have an impact similar to the total of all the atmospheric carbon dioxide emissions due to air travel over the past 100 years combined."

Soot, ice crystals – contrails with climatic impact

Aircraft engines emit soot particles. These act as condensation nuclei for small, supercooled raindrops that freeze immediately to form ice crystals that are visible in the sky as contrails. The ice crystals in the contrails can last for several hours in cold, damp conditions at heights of around eight to 12 kilometres, and high clouds form that are known as contrail cirrus. Depending on the position of the Sun and the ground, the clouds can trigger a local warming or cooling effect, with research work showing that the warming effect predominates globally. The occurrence of contrail cirrus can vary greatly depending on time and location, so just a few contrail cirrus outbreaks are responsible for much of the warming effect.

"Based on our theoretical model calculations, we were able to establish how fewer ice crystals reduce the optical thickness of the contrail cirrus, due to the reduced numbers of soot particles, and also shorten the lifetime of the clouds," says Burkhardt. "Overall, this results in less cloud cover due to contrail cirrus-induced clouds and a lower climate impact. A reduction in soot particle emission is particularly effective during significant contrail cirrus outbreaks."

The interplay between the choice of fuel and combustion in the engine is decisive in reducing soot emissions in aviation. For example, new engine technologies enable soot emissions to be reduced as a result of combustion at higher temperatures, even using conventional fuels.

Intensive research is being carried out into the reduction of soot emissions through the use of alternative fuels with a lower proportion of cyclic hydrocarbons, which have a significant influence on the formation of soot in the combustion process. DLR and NASA conducted joint research flights in January 2018 to investigate the effect of different fuel blends on soot emissions and the associated formation of ice crystals. Based on data from the research flights, the researchers hope to demonstrate in practice and in detail the theoretically estimated reduction in the formation of ice crystals through less soot. The results are expected in summer 2019.

Contact
  • Falk Dambowsky
    Ed­i­tor
    Ger­man Aerospace Cen­ter (DLR)
    Me­dia Re­la­tions
    Com­mu­ni­ca­tions and Me­dia Re­la­tions
    Telephone: +49 2203 601-3959
    Fax: +49 2203 601-3249
    Linder Höhe
    51147 Cologne
    Contact
  • Ulrike Burkhardt
    Ger­man Aerospace Cen­ter (DLR)
    In­sti­tute of At­mo­spher­ic Physics
    Münchener Straße 20
    82234 Oberpfaffenhofen

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