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Titlebook: Atmospheric Physics; Background – Methods Ulrich Schumann Book 2012 Springer-Verlag Berlin Heidelberg 2012 Air Composition and Aerosol Mode

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發(fā)表于 2025-3-28 17:03:05 | 只看該作者
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發(fā)表于 2025-3-28 20:36:25 | 只看該作者
Potenzen und M?biustransformationenenhouse effect is a synonym for the trapping of infrared radiation by radiatively active atmospheric constituents. It generally causes a warming of the planet’s surface, compared to the case without atmosphere. Perturbing the radiation balance of the planet, e.g., by anthropogenic greenhouse gas emi
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發(fā)表于 2025-3-28 23:55:38 | 只看該作者
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發(fā)表于 2025-3-29 04:42:01 | 只看該作者
Potenzen und M?biustransformationen The main local NO sources in the upper troposphere are emissions from aircraft and production by lightning. In the past 20?years, DLR studied the latter source in airborne field experiments accompanied with model simulations. The global lightning NO source is found to be distinctly larger than that
45#
發(fā)表于 2025-3-29 08:44:46 | 只看該作者
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發(fā)表于 2025-3-29 15:15:57 | 只看該作者
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發(fā)表于 2025-3-29 18:01:47 | 只看該作者
Funktionentheorie in der Ebene und im Raum on lifetime and other properties. Transported emissions include primary pollutants emitted from industry and vehicles (e.g., nitric oxide) and natural pollutants released by forest fires (e.g., soot). Also secondary pollutants (e.g., ozone) that are formed near the source region undergo transport.
48#
發(fā)表于 2025-3-29 20:42:55 | 只看該作者
49#
發(fā)表于 2025-3-30 03:45:59 | 只看該作者
https://doi.org/10.1007/3-7643-7430-6 safety and capacity of the air-transportation system. This section gives an overview of the wake vortex issue commencing at its historical roots, proceeding with a sketch of the nature and characteristics of wake vortices resulting from field measurement and numerical simulation, and concluding wit
50#
發(fā)表于 2025-3-30 06:12:37 | 只看該作者
Integrals?tze und Integralformelnion changes cloudiness also by soot emissions and other aerosols. In the global mean, contrail cirrus warms the atmosphere. The local warming induced by a contrail varies strongly relative to the global mean, and may be positive or negative, depending on aircraft, route, solar and Earth-atmosphere p
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