Zobrazeno 1 - 10
of 23
pro vyhledávání: '"E. R. Lovejoy"'
Autor:
R. Weigel, S. Borrmann, J. Kazil, A. Minikin, A. Stohl, J. C. Wilson, J. M. Reeves, D. Kunkel, M. de Reus, W. Frey, E. R. Lovejoy, C. M. Volk, S. Viciani, F. D'Amato, C. Schiller, T. Peter, H. Schlager, F. Cairo, K. S. Law, G. N. Shur, G. V. Belyaev, J. Curtius
Publikováno v:
Atmospheric Chemistry and Physics, Vol 11, Iss 18, Pp 9983-10010 (2011)
New particle formation (NPF), which generates nucleation mode aerosol, was observed in the tropical Upper Troposphere (UT) and Tropical Tropopause Layer (TTL) by in situ airborne measurements over South America (January–March 2005), Australia (Nove
Externí odkaz:
https://doaj.org/article/e7bb2790aad74ae787c95f8b6044ff72
Autor:
J. Kazil, E. R. Lovejoy
Publikováno v:
Atmospheric Chemistry and Physics, Vol 7, Iss 13, Pp 3447-3459 (2007)
The formation of new aerosol from the gas phase is commonly represented in atmospheric modeling with parameterizations of the steady state nucleation rate. Present parameterizations are based on classical nucleation theory or on nucleation rates calc
Externí odkaz:
https://doaj.org/article/41aa3adc985342f2a0c429470042c30e
Publikováno v:
Atmospheric Chemistry and Physics, Vol 7, Iss 5, Pp 1407-1413 (2007)
The recent observation of ultrafine aerosol particles in cirrus clouds has raised the question whether aerosol formation within cirrus clouds is possible, and if so, what mechanisms are involved. We have developed an aerosol parcel model of neutral a
Externí odkaz:
https://doaj.org/article/7a84114acb2448f882cc0f3bc322c031
Publikováno v:
Atmospheric Chemistry and Physics, Vol 6, Iss 2, Pp 505-523 (2006)
We studied the possible role of iodine oxides in atmospheric new particle formation with the one-dimensional marine boundary layer model MISTRA, which includes chemistry in the gas and aerosol phase as well as aerosol microphysics. The chemical react
Externí odkaz:
https://doaj.org/article/7da3b5e51e1b4934ab1bb11665612b2b
Publikováno v:
Atmospheric Chemistry and Physics, Vol 6, Iss 12, Pp 4905-4924 (2006)
We investigate formation of sulfate aerosol in the marine troposphere from neutral and charged nucleation of H2SO4 and H2O. A box model of neutral and charged aerosol processes is run on a grid covering the oceans. Input data are taken from a model o
Externí odkaz:
https://doaj.org/article/c14352549d24414b986fc23cc7638dcb
Publikováno v:
Atmospheric Chemistry and Physics, Vol 4, Iss 1, Pp 19-34 (2004)
Laboratory experimental results of iodine oxide nucleation are presented. Nucleation was induced following UV photolysis of CF3I or CH2I2 in the presence of excess ozone. Measurements were performed in a 70 L Teflon reactor with new particles detecte
Externí odkaz:
https://doaj.org/article/c5e305daf02142fe9812eedc3a7f5a80
Autor:
E. R. Lovejoy, C. B. Moore
Publikováno v:
ChemInform. 24
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a43e9f313a219dd9b772e9f3a0b1175f
https://doi.org/10.1002/chin.199337112
https://doi.org/10.1002/chin.199337112
Publikováno v:
Solar Variability and Planetary Climates ISBN: 9780387483399
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::aa2a5bfd14bf72d59a87063903f8a7e1
https://doi.org/10.1007/978-0-387-48341-2_13
https://doi.org/10.1007/978-0-387-48341-2_13
Publikováno v:
Atmospheric Chemistry and Physics
Atmospheric Chemistry and Physics, European Geosciences Union, 2007, 7 (5), pp.1407-1413
Atmospheric Chemistry and Physics, European Geosciences Union, 2007, 7 (5), pp.1407-1413
International audience; The recent observation of ultrafine aerosol particles in cirrus clouds has raised the question whether aerosol formation within cirrus clouds is possible, and if so, what mechanisms are involved. We have developed an aerosol p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b5e4a7718dec7da3ff256eb8772b7f37
https://hal.archives-ouvertes.fr/hal-00302314
https://hal.archives-ouvertes.fr/hal-00302314