Detection and attribution of aerosol-cloud interactions in large-domain large-eddy simulations with ICON

Medientyp: E-Artikel

Titel: Detection and attribution of aerosol-cloud interactions in large-domain large-eddy simulations with ICON

Beteiligte: Costa-Surós, Montserrat [VerfasserIn]; Sourdeval, Odran [VerfasserIn]; Madenach, Nils [VerfasserIn]; Meyer, Catrin I. [VerfasserIn]; Schrödner, Roland [VerfasserIn]; Seifert, Patric [VerfasserIn]; Senf, Fabian [VerfasserIn]; Brueck, Matthias [VerfasserIn]; Cioni, Guido [VerfasserIn]; Engels, Jan Frederik [VerfasserIn]; Fieg, Kerstin [VerfasserIn]; Gorges, Ksenia [VerfasserIn]; Acquistapace, Claudia [VerfasserIn]; Heinze, Rieke [VerfasserIn]; Siligam, Pavan Kumar [VerfasserIn]; Burkhardt, Ulrike [VerfasserIn]; Crewell, Susanne [VerfasserIn]; Hoose, Corinna [VerfasserIn]; Seifert, Axel [VerfasserIn]; Tegen, Ina [VerfasserIn]; Quaas, Johannes [VerfasserIn]; Baars, Holger [VerfasserIn]; Carbajal Henken, Cintia [VerfasserIn]; Genz, Christa [VerfasserIn]; [...]

Erschienen: Forschungszentrum Jülich: JuSER (Juelich Shared Electronic Resources), 2019

Sprache: Englisch

DOI: https://doi.org/10.5194/acp-2019-850

ISSN: 1680-7367

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Beschreibung: Abstract. Clouds and aerosols contribute the largest uncertainty to current estimates and interpretations of the Earth’s changing energy budget. Here we use a new-generation large-domain large-eddy model, ICON-LEM, to simulate the response of clouds to realistic anthropogenic perturbations in aerosols serving as cloud condensation nuclei (CCN). The novelty compared to previous studies is that (i) the LEM is run in weather prediction mode and with fully interactive land surface over a large domain, and (ii) a large range of data from various sources are used for the detection and attribution. The aerosol perturbation was chosen as peak-aerosol conditions over Europe in 1985, with more than five-fold more sulfate than in 2013. Observational data from various satellite and ground-based remote sensing instruments are used aiming at a detection and attribution of this response. The simulation was run for a selected day (2 May 2013) in which over the selected domain of central Europe a large variety of cloud regimes was present. It first is demonstrated, using satellite aerosol optical depth retrievals available for both 1985 and 2013, that the aerosol fields for the reference conditions and also for the perturbed ones, as well as the difference between the two, were consistent in the model and the satellite retrievals. In comparison to retrievals from ground-based lidar for 2013, CCN profiles for the reference conditions were consistent with the observations, while the ones for the 1985 conditions were not. Similarly, detection-and-attribution was successful for droplet number concentrations: the ones simulated for the 2013 conditions were consistent with satellite as well as new ground-based lidar retrievals, while the ones for the 1985 conditions were outside the observational range. For other cloud quantities, including cloud fraction, liquid water path, cloud-base altitude, and cloud lifetime, the aerosol response was small compared to their natural variability. Also, large uncertainties in satellite and ...

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