Abstract

Abstract. The investigation of the impact of aircraft parameters on contrail properties helps to better understand the climate impact from aviation. Yet, in observations, it is a challenge to separate aircraft and meteorological influences on contrail formation. During the CONCERT campaign in November 2008, contrails from 3 Airbus passenger aircraft of types A319-111, A340-311 and A380-841 were probed at cruise under similar meteorological conditions with in situ instruments on board DLR research aircraft Falcon. Within the 2 min-old contrails detected near ice saturation, we find similar effective diameters Deff (5.2–5.9 μm), but differences in particle number densities nice (162–235 cm−3) and in vertical contrail extensions (120–290 m), resulting in large differences in contrail optical depths τ at 550 nm (0.25–0.94). Hence larger aircraft produce optically thicker contrails. Based on the observations, we apply the EULAG-LCM model with explicit ice microphysics and, in addition, the Contrail and Cirrus Prediction (CoCiP) model to calculate the aircraft type impact on young contrails under identical meteorological conditions. The observed increase in τ for heavier aircraft is confirmed by the models, yet for generally smaller τ. CoCiP model results suggest that the aircraft dependence of climate-relevant contrail properties persists during contrail lifetime, adding importance to aircraft-dependent model initialization. We finally derive an analytical relationship between contrail, aircraft and meteorological parameters. Near ice saturation, contrail width × τ scales linearly with the fuel flow rate, as confirmed by observations. For higher relative humidity with respect to ice (RHI), the analytical relationship suggests a non-linear increase in the form (RHI-12/3. Summarized, our combined results could help to more accurately assess the climate impact from aviation using an aircraft-dependent contrail parameterization.

Highlights

  • Aircraft contrails affect climate by reflection of incoming solar radiation and trapping of outgoing terrestrial radiation

  • In situ observations of young contrails were used to investigate the dependence of contrail properties on the aircraft type

  • Contrails with ages less than 2 min from A319-111, A340-311 and A380-841 aircraft were probed with the Falcon research aircraft during the CONCERT2008 campaign under similar meteorological conditions

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Summary

Introduction

Aircraft contrails affect climate by reflection of incoming solar radiation and trapping of outgoing terrestrial radiation. Contrails may survive for several hours in ice supersaturated conditions (Graf et al, 2012), with the total contrail cover being dependent on air traffic movement and distribution. Voigt et al (2011) derived a mean (median) contrail optical depth of 0.27 (0.13) from 14 young < 5 min-old contrails near ice saturation of nine different aircraft. Lidar observations combined with numerical studies by Sussmann and Gierens (1999, 2001) suggest that early contrail properties depend on atmospheric conditions as well as on the aircraft type. We compare the results with two model studies performed with the EULAG-LCM Lagrangian particle tracking model (Sölch and Kärcher, 2010) and the contrail cirrus prediction model (CoCiP) (Schumann, 2012) to identify the aircraft influence on contrail properties under identical meteorological fields. We compare our findings with our observations and previous measurements and model results

Instrumentation
The FSSP-300 forward scattering spectrometer probe
The Polar Nephelometer
Hygrometers
The NO and NOy chemiluminescence instrument
Contrail chasing and meteorology
Mean particle size and surface area distributions
Contrail optical depth distributions
Model simulations and results
The EULAG-LCM model system
Atmospheric conditions and contrail initialization
The CoCiP model
CoCip model results and comparison with observations
Comparison with the EULAG-LCM model results
Impact of fuel flow on contrail optical properties
Findings
Discussion
Conclusions and outlook
Full Text
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