New-particle formation events in a continental boundary layer: First results from the SATURN experiment
| Autor: | Ulla Wandinger, C. Seidel, Holger Siebert, Andreas Stohl, Gerald Spindler, R. Rinke, O. Hellmuth, Dietrich Althausen, Jost Heintzenberg, U. Uhrner, U. Schmieder, Thomas Tuch, F. Stratmann, Birgit Wehner, A. Wiedensohler, Manfred Wendisch, D. Schell |
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| Přispěvatelé: | Leibniz Institute for Tropospheric Research (TROPOS), enviscope GmbH, Technische Universität Munchen - Université Technique de Munich [Munich, Allemagne] (TUM) |
| Jazyk: | angličtina |
| Rok vydání: | 2003 |
| Předmět: |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere Atmospheric Science Particle number 010504 meteorology & atmospheric sciences Planetary boundary layer SODAR Geophysics 010501 environmental sciences 01 natural sciences lcsh:QC1-999 lcsh:Chemistry Boundary layer lcsh:QD1-999 13. Climate action Saturn Capping inversion Particle Layer (electronics) Geology lcsh:Physics 0105 earth and related environmental sciences |
| Zdroj: | Atmospheric Chemistry and Physics Discussions Atmospheric Chemistry and Physics Discussions, European Geosciences Union, 2003, 3 (2), pp.1693-1731 Atmospheric Chemistry and Physics, Vol 3, Iss 5, Pp 1445-1459 (2003) Scopus-Elsevier Atmospheric Chemistry and Physics Atmospheric Chemistry and Physics, European Geosciences Union, 2003, 3 (5), pp.1445-1459 |
| ISSN: | 1680-7367 1680-7375 1680-7316 1680-7324 |
| Popis: | During the SATURN experiment, which took place from 27 May to 4 June 2002, new particle formation in the continental boundary layer was investigated. Simultaneous ground-based and tethered-balloon-borne measurements were performed, including meteorological parameters, particle number concentrations and size distributions, gaseous precursor concentrations and SODAR and LIDAR observations. Newly formed particles were observed inside the residual layer, before the break-up process of the nocturnal inversion, and inside the mixing layer throughout the break-up of the nocturnal inversion and during the evolution of the planetary boundary layer. |
| Databáze: | OpenAIRE |
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