Statistical analysis of contrail to cirrus evolution during the Contrail and Cirrus Experiment (CONCERT)

Autor: A. Chauvigné, O. Jourdan, A. Schwarzenboeck, C. Gourbeyre, J. F. Gayet, C. Voigt, H. Schlager, S. Kaufmann, S. Borrmann, S. Molleker, A. Minikin, T. Jurkat, U. Schumann

Publikováno v: Atmospheric Chemistry and Physics, Vol 18, Pp 9803-9822 (2018)

Air traffic affects cloudiness, and thus climate, by emitting exhaust gases and particles. The study of the evolution of contrail properties is very challenging due to the complex interplay of vortex dynamics and the atmospheric environment (e.g.

Externí odkaz: https://doaj.org/article/03fdac09d888470c9a66aa752d81e35f

A new airborne polar Nephelometer for the measurements of optical and microphysical cloud properties. Part I: Theoretical design

Autor: J. F. Gayet, O. Crépel, J. F. Fournol, S. Oshchepkov

Publikováno v: Annales Geophysicae, Vol 15, Pp 451-459 (1997)

A new optical sensor, the airborne Polar Nephelometer, is described. The sensor is designed to measure the optical and microphysical parameters of clouds containing either water droplets or ice crystals or a mixture of these particles ranging in s

Externí odkaz: https://doaj.org/article/92fb0da535024364a7087a88e77e01ba

Porous aerosol in degassing plumes of Mt. Etna and Mt. Stromboli

Autor: V. Shcherbakov, O. Jourdan, C. Voigt, J.-F. Gayet, A. Chauvigne, A. Schwarzenboeck, A. Minikin, M. Klingebiel, R. Weigel, S. Borrmann, T. Jurkat, S. Kaufmann, R. Schlage, C. Gourbeyre, G. Febvre, T. Lapyonok, W. Frey, S. Molleker, B. Weinzierl

Publikováno v: Shcherbakov, V, Jourdan, O, Voigt, C, Gayet, J F, Chauvigne, A, Schwarzenboeck, A, Minikin, A, Klingebiel, M, Weigel, R, Borrmann, S, Jurkat, T, Kaufmann, S, Schlage, R, Gourbeyre, C, Febvre, G, Lapyonok, T, Frey, W, Molleker, S & Weinzierl, B 2016, ' Porous aerosol in degassing plumes of Mt. Etna and Mt. Stromboli ', Atmospheric Chemistry and Physics, vol. 16, no. 18, pp. 11883-11897 . https://doi.org/10.5194/acp-16-11883-2016
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2016, 16 (18), pp.11883-11897. ⟨10.5194/acp-16-11883-2016⟩
Atmospheric Chemistry and Physics 16 (2016) 18
Atmospheric Chemistry and Physics, 16(18), 11883-11897
Atmospheric Chemistry and Physics, Vol 16, Pp 11883-11897 (2016)
Atmospheric Chemistry and Physics, 2016, 16 (18), pp.11883-11897. ⟨10.5194/acp-16-11883-2016⟩

Aerosols of the volcanic degassing plumes from Mt. Etna and Mt. Stromboli were probed with in situ instruments on board the Deutsches Zentrum für Luft- und Raumfahrt research aircraft Falcon during the contrail, volcano, and cirrus experiment CONCER

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7e29656da9f2dcf06b36e9b5248b809f
https://www.research.manchester.ac.uk/portal/en/publications/porous-aerosol-in-degassing-plumes-of-mt-etna-and-mt-stromboli(dea8b7a5-aaf4-450a-bada-08f02326f960).html

Aerosol-cirrus interactions: a number based phenomenon at all?

Autor: M. Seifert, J. Ström, R. Krejci, A. Minikin, A. Petzold, J.-F. Gayet, H. Schlager, H. Ziereis, U. Schumann, J. Ovarlez

Publikováno v: Atmospheric Chemistry and Physics, Vol 4, Iss 2, Pp 293-305 (2004)

In situ measurements of the partitioning of aerosol particles within cirrus clouds were used to investigate aerosol-cloud interactions in ice clouds. The number density of interstitial aerosol particles (non-activated particles in between the cirrus

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doajarticles::3e4ed91bcb7ae4bb63df8ee4eb74e5f9
http://www.atmos-chem-phys.net/4/293/2004/acp-4-293-2004.pdf

In-situ observations of aerosol particles remaining from evaporated cirrus crystals: Comparing clean and polluted air masses

Autor: M. Seifert, J. Ström, R. Krejci, A. Minikin, A. Petzold, J.-F. Gayet, U. Schumann, J. Ovarlez

Publikováno v: Atmospheric Chemistry and Physics, Vol 3, Iss 4, Pp 1037-1049 (2003)

In-situ observations of aerosol particles contained in cirrus crystals are presented and compared to interstitial aerosol size distributions (non-activated particles in between the cirrus crystals). The observations were conducted in cirrus clouds in

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doajarticles::44e17aacb827cb2bfd1342f4d0d7174c
http://www.atmos-chem-phys.net/3/1037/2003/acp-3-1037-2003.pdf