Titlebook: Atmospheric Trace Constituents; Proceedings of the 5 Fritz Herbert Conference proceedings 1982 Friedr. Vieweg & Sohn Verlagsgesellschaft mb

Expressly

On a Diurnal Variation of NO2 Found in North Atlantic Air Masses lower than 10 pptv most of the time. In addition a diurnal variation in the mixing ratios of NO. was found with higher daytime values than at night, 84 ± 49 pptv NO. overall and 37 ± 6 pptv NO. at night.

游行

A Discussion of Approximate Relations for Transfer and Deposition of Trace Constituents in the ABLed. For deter-ming actual values and profiles these methods are applicable to field measurements obtained from instrumented towers or boundary layer soundings. The theoretical concept is general enough to enable numerical evaluations at variable stability conditions in the atmosphere.

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GULF

Tropospheric OH Measurementsering effects, saturation and self-generating, which are encountered in the method of laser-induced fluorescence (LIF) are discussed with respect to the applicability of this method. An absorption method is introduced as an alternative. An interference effect due to SO. is described and experimental

FELON

nocturnal

The Determination of the Atmospheric Heating Rate Due to the Absorption of Shortwave Radiation in Paerivation the shortwave radiation supply and the mean absorption coefficient of the aerosol particles have to be ascertained by measurements. A radiometer was developed, which is used to measure the shortwave radiation supply, i.e. the shortwave radiation coming from all directions towards the point

離開可分裂

New Meteorological Applications of the Aerosol Physical Chemistryd Lehmann 1981) that at present enough information is available allowing reliable meteorological applications. In this paper two processes, the settlement of particles through the atmosphere under the influence of gravity and the activation of particles in fog and clouds, are considered.

conscience

On the Flux and Collision Mechanism of the Scavenging Process of Atmospheric Aerosol Particlesjected to a series of dynamical driving forces. A practicable mathematical treatment is developed by applying the method of irreversible processes in connection with specialized momentum laws for the atmosphere and the particles and useful expressions for various transport parameters. Collection ker