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The severe drought that California has experienced in recent years may also have decreased the number of fog events even more since 2012.
The concurrent occurrence of dense fog events and heavy rain events are seldom.
The impact of individual fog events can be seen in Figure 7. Figure 7 Obtained CDs of attenuation due to fog events on the FSO path over the 6-year period of observation.
It can be seen in Figure 11. Figure 11 Obtained CDs of visibility due to all the fog events combined and to the individual fog events separately on the FSO path over the 6-year period of observation.
It can also be seen that the influence of all the fog events on the total attenuation is entirely insignificant.
It can be seen in Figure 10 that the visibility is significantly reduced by all fog events.
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An extremely dense sea fog event was observed around the Shandong Peninsula in the morning of 11 April 2004.
A 30-h modeling that started from 18 UTC 10 April 2004 reproduced the main characteristics of this fog event.
These measurements do not differentiate between fog-only events and the combinations of fog with the other hydrometeors.
The obtained CD of visibility due to fog-only events, denoted in Figure 11 as F, was also used for the calculation of attenuation due to fog only by the aforementioned methods.
Others are intended to help residents deal with FOG-saturated events like Thanksgiving or Christmas.
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