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Finally, a weak atmospheric magnetic field can slightly, by a few percent, increase the frequency of the eigen-mode.
A weak atmospheric turbulence (clear-air condition) scenario is considered, for which the received signal intensity fluctuation can be modeled as a log-normal random process.
Analytical formulae are also provided for the frequency shifts due to the presence of a thin transitional layer and a weak atmospheric magnetic field.
On May 20, satellite imagery showed evidence of a weak atmospheric circulation.
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The decay rates of CO and BC were slightly greater in summer than in winter for both freeways, suggesting a weaker atmospheric dilution effect in winter.
Two main cases are shown in this figure: severe atmospheric turbulence conditions (α=4.341 and β=1.309) and weak atmospheric turbulence conditions (α=6.993 and β=5.460).
This method enables us to identify weak atmospheric signatures such as neon (73.5 nm) and argon (104.8 nm), which could not be detected with conventional detector systems.
The ergodic channel capacity versus SNR is plotted in Fig. 10 under weak atmospheric turbulence conditions for different values of N 1=N 2. The gain achieved in the system capacity due to decreasing N 1=N 2 or, equivalently, due to selecting a better source and destination is shown in this figure.
The log-normal fading model is usually used to model the FSO links assuming weak atmospheric turbulence conditions, whereas the Gamma-Gamma fading model is more accurate and can be used to model the FSO links under both weak and strong turbulence conditions.
In general, iFis elevated for emissions that occur during periods of weak atmospheric dispersion (e.g., nighttime, Figure SI.8, Supporting Information).
Future climate change may increase ground-level ozone pollution in Europe due to higher temperatures and weaker atmospheric circulation.
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