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We find that while the determination of object size needs to be reviewed, the altitude distribution provides a good fit to the model prediction.
The 3D hybrid receptor models presented herein are designed to identify altitude distribution of potential sources, whereas CWBL can be used for analyzing the vertical distribution of pollutant concentrations along the transport pathway.
Importantly, different measurement techniques applied at different geographical locations and under different geophysical conditions all provide undisputable evidence for the ubiquitous presence of these particles in the upper atmosphere, even though admittedly some of the specific features like the detailed altitude distribution and the charging characteristics are not completely understood.
The altitude distribution of data is shown in Fig. 1.
It is observed that the altitude distribution of the ionospheric plasma is very asymmetrical although the spacecraft sampled the same solar zenith angles.
This early model instability can be reduced by instituting a more realistic altitude distribution of the photochemical production of sulfuric acid, or the introduction of additional sulfur chemistry to smooth away such spikes in vapor concentrations.
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The 70 profiles of temperature, zonal and meridional wind used to derive atmospheric stability statistics are also presented, as are wind shear amplitude and altitude distributions.
In this paper we describe a retrieval approach for the simultaneous determination of the altitude distributions of p, T and VMR of atmospheric constituents from limb-scanning measurements of the atmosphere.
An approach to determine the dependence of the mid-latitude topside ionospheric electron number density (Ne) altitude distributions and ion composition changes on long-term solar-cycle variations and short-term solar-wind and magnetic disturbances has been developed.
From the open-loop recorded data, the altitude distributions of the temperature, the H2SO4 vapor mixing ratio, and the electron density are being successfully retrieved.
Both species have wide altitude distributions, ranging from 2900 m to 5000 m [ 26, 27] and the use of molecular data combined with macro-evolutionary modeling may provide useful insights into the dynamics of their range evolution.
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