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Titlebook: Air Pollution Modeling and its Application XXIV; Douw G. Steyn,Nadine Chaumerliac Conference proceedings 2016 Springer International Publi

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樓主: 夸大
31#
發(fā)表于 2025-3-27 00:26:41 | 只看該作者
32#
發(fā)表于 2025-3-27 02:20:32 | 只看該作者
Aerosol Variability and Weather Regimes over the Mediterranean Regionre opposed to these high aerosol loads. These weather regimes are based on a statistical method of automated classification. This method enables to characterize the effects of aerosols on climate for each weather regime, and the links between aerosol variability and climate oscillations such as the North-Atlantic Oscillation (NAO).
33#
發(fā)表于 2025-3-27 06:38:40 | 只看該作者
https://doi.org/10.1007/978-3-642-51999-4sport (GOCART) model and satellite and in situ data to investigate (1) long-term variations of aerosols over polluted and dust source regions and downwind ocean areas in the past three decades and the cause of the changes and (2) anthropogenic and volcanic contributions to the sulfate aerosol in the
34#
發(fā)表于 2025-3-27 11:12:20 | 只看該作者
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發(fā)表于 2025-3-27 15:12:15 | 只看該作者
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發(fā)表于 2025-3-27 18:04:39 | 只看該作者
Geschichte der Kenntnisse vom Gesichtsfeld,concentration in central Europe is investigated. Depending on crop growth, temperature and local legislation individual temporal profiles for fertilizer and manure application are calculated for each model grid cell of the SMOKE-EU emission model. The emission data was used as input for the CMAQ che
37#
發(fā)表于 2025-3-27 22:19:08 | 只看該作者
Geschichte der Kenntnisse vom Gesichtsfeld,anisms of secondary organic aerosols (SOA) remain one of the least understood processes relevant to the atmosphere. Laboratory experiments, in situ measurements and numerical simulations recently highlighted the formation of SOA through aqueous chemistry in humid aerosol particles and in cloud dropl
38#
發(fā)表于 2025-3-28 05:16:58 | 只看該作者
39#
發(fā)表于 2025-3-28 09:13:34 | 只看該作者
40#
發(fā)表于 2025-3-28 10:51:48 | 只看該作者
Anthropologie und Popularphilosophieng with emissions of air pollutants such as NO., NH., and SO. leading to the formation of HNO., H.SO., and particulate matter. Gaseous bases and acids (mainly HNO., H.SO. and NH.) tend to form new particles or to condense on existing ones. Meteorological conditions and size distribution of existing
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