Zobrazeno 1 - 10
of 23
pro vyhledávání: '"J. Skrotzki"'
Autor:
J. Skrotzki, P. Connolly, M. Schnaiter, H. Saathoff, O. Möhler, R. Wagner, M. Niemand, V. Ebert, T. Leisner
Publikováno v:
Atmospheric Chemistry and Physics, Vol 13, Iss 8, Pp 4451-4466 (2013)
Cirrus clouds and their impact on the Earth's radiative budget are subjects of current research. The processes governing the growth of cirrus ice particles are central to the radiative properties of cirrus clouds. At temperatures relevant to cirrus c
Externí odkaz:
https://doaj.org/article/7e982ef6eba54867841c6bfd01b9d9bf
Publikováno v:
Atmospheric Chemistry and Physics, Vol 12, Iss 21, Pp 10465-10484 (2012)
The article presents the laser scattering and depolarisation instrument SIMONE that is installed at the large aerosol and cloud chamber facility AIDA of the Karlsruhe Institute of Technology. SIMONE uses a 488 nm cw laser to probe simulated atmospher
Externí odkaz:
https://doaj.org/article/d8917ca2272e4a36be4bcbdfe668ab08
Autor:
T. W. Wilson, B. J. Murray, R. Wagner, O. Möhler, H. Saathoff, M. Schnaiter, J. Skrotzki, H. C. Price, T. L. Malkin, S. Dobbie, S. M. R. K. Al-Jumur
Publikováno v:
Atmospheric Chemistry and Physics, Vol 12, Iss 18, Pp 8611-8632 (2012)
Atmospheric secondary organic aerosol (SOA) is likely to exist in a semi-solid or glassy state, particularly at low temperatures and humidities. Previously, it has been shown that glassy aqueous citric acid aerosol is able to nucleate ice heterogeneo
Externí odkaz:
https://doaj.org/article/69b0b33694d045fca03652a0b5bc7bec
Autor:
R. Wagner, O. Möhler, H. Saathoff, M. Schnaiter, J. Skrotzki, T. Leisner, T. W. Wilson, T. L. Malkin, B. J. Murray
Publikováno v:
Atmospheric Chemistry and Physics, Vol 12, Iss 18, Pp 8589-8610 (2012)
The ice nucleation potential of airborne glassy aqueous aerosol particles has been investigated by controlled expansion cooling cycles in the AIDA aerosol and cloud chamber of the Karlsruhe Institute of Technology at temperatures between 247 and 216
Externí odkaz:
https://doaj.org/article/9c5750a7b3ed4784a1819310d39085bc
Autor:
I. Steinke, O. Möhler, A. Kiselev, M. Niemand, H. Saathoff, M. Schnaiter, J. Skrotzki, C. Hoose, T. Leisner
Publikováno v:
Atmospheric Chemistry and Physics, Vol 11, Iss 24, Pp 12945-12958 (2011)
During the eruption of the Eyjafjallajökull volcano in the south of Iceland in April/May 2010, about 40 Tg of ash mass were emitted into the atmosphere. It was unclear whether volcanic ash particles with d < 10 μm facilitate the glaciation of cloud
Externí odkaz:
https://doaj.org/article/6ff994c36d0347b89848a21d2b78a9a2
Autor:
Thomas Leisner, M. Niemand, Ottmar Möhler, Volker Ebert, Robert Wagner, J. Skrotzki, Harald Saathoff, Martin Schnaiter, Paul Connolly
Publikováno v:
Skrotzki, J, Connolly, P, Schnaiter, M, Saathoff, H, Mo\"hler, O, Wagner, R, Niemand, M, Ebert, V, Leisner, T & Möhler, O 2013, ' The accommodation coefficient of water molecules on ice-cirrus cloud studies at the AIDA simulation chamber ', Atmospheric Chemistry and Physics, vol. 13, no. 8, pp. 4451-4466 . https://doi.org/10.5194/acp-13-4451-2013
Atmospheric chemistry and physics, 13 (8), 4451-4466
Atmospheric Chemistry and Physics, Vol 13, Iss 8, Pp 4451-4466 (2013)
Atmospheric chemistry and physics, 13 (8), 4451-4466
Atmospheric Chemistry and Physics, Vol 13, Iss 8, Pp 4451-4466 (2013)
Cirrus clouds and their impact on the Earth's radiative budget are subjects of current research. The processes governing the growth of cirrus ice particles are central to the radiative properties of cirrus clouds. At temperatures relevant to cirrus c
Publikováno v:
Atmospheric Chemistry and Physics, Vol 12, Iss 21, Pp 10465-10484 (2012)
The article presents the laser scattering and depolarisation instrument SIMONE that is installed at the large aerosol and cloud chamber facility AIDA of the Karlsruhe Institute of Technology. SIMONE uses a 488 nm cw laser to probe simulated atmospher
Autor:
Harald Saathoff, Corinna Hoose, Alexei Kiselev, J. Skrotzki, Martin Schnaiter, Ottmar Möhler, Isabelle Steinke, M. Niemand, T. Leisner
Publikováno v:
Atmospheric Chemistry and Physics, Vol 11, Iss 24, Pp 12945-12958 (2011)
Atmospheric Chemistry and Physics Discussions, 11 (6), 17665-17698
Atmospheric Chemistry and Physics, 11 (28), 12945-12958
Atmospheric Chemistry and Physics Discussions, 11 (6), 17665-17698
Atmospheric Chemistry and Physics, 11 (28), 12945-12958
During the eruption of the Eyjafjallajökull volcano in the south of Iceland in April/May 2010, about 40 Tg of ash mass were emitted into the atmosphere. It was unclear whether volcanic ash particles with d < 10 μm facilitate the glaciation of cloud
Autor:
H. C. Price, S. Dobbie, Martin Schnaiter, Ottmar Möhler, T. W. Wilson, Benjamin J. Murray, J. Skrotzki, Sardar M. R. K. Al-Jumur, Harald Saathoff, Robert Wagner, T. L. Malkin
Publikováno v:
Atmospheric Chemistry and Physics Discussions
Atmospheric Chemistry and Physics, Vol 12, Iss 18, Pp 8611-8632 (2012)
Atmospheric Chemistry and Physics, Vol 12, Iss 18, Pp 8611-8632 (2012)
Atmospheric secondary organic aerosol (SOA) is likely to exist in a semi-solid or glassy state, particularly at low temperatures and humidities. Previously, it has been shown that glassy aqueous citric acid aerosol is able to nucleate ice heterogeneo