Humid ones.
That would be a stratus cloud.
That would be a stratus cloud.
A low-level cloud that often produces fog and drizzle is called a stratus cloud. These clouds typically appear as a uniform gray layer covering the sky, leading to overcast conditions. Stratus clouds can lead to light precipitation, such as drizzle, and are commonly associated with cool, damp weather.
it is a bunch of water droplets that have not joined together and it is like a drizzle but even lighter
A mist is precipitation that can be characterized as "fog". While the sky might not be raining, there is still moisture in the air. Also mist is composed of ground water, not rain water. Drizzle is a light rain that continues for more than a few minutes. It's rather like comparing a drip from the faucet to having it full open. Drizzle is the drip, rain is full open.
A maritime tropical air mass is responsible for fog and drizzle in coastal regions. This air mass is warm and humid, which can lead to the formation of fog and light precipitation when it interacts with the cooler coastal waters or land.
the boogers
Tiny drops of water in the air are called mist or fog, depending on their density and visibility.
Another word for thin fog is mist. Mist is a fine spray or drizzle that hovers in the air and often gives a hazy or ethereal appearance.
fog
Maritime polar air masses have more effect on the west coast due to the prevailing westerly winds that bring these air masses from the Pacific Ocean. The west coast is more influenced by these moist and cool air masses, leading to more precipitation and cooler temperatures. In contrast, the east coast is shielded by the Appalachian Mountains, which hinder the penetration of maritime polar air masses from the Atlantic Ocean.
It can't. Even in the highest power transmission lines there isn't enough potential to overcome the resistance in the rain drops and air gaps. If it could arc to ground in drizzle it would be able to do so in fog too.
haze, fog, smog, murk, cloud, drizzle, spray
The maritime polar air masses influence the climate of San Francisco. These air masses originate from the Pacific Ocean and bring cool, moist conditions to the region. This contributes to the characteristic fog and moderate temperatures experienced in San Francisco.
coastal areas and valleys where there is a convergence of air masses and temperature variations. Additionally, urban areas with high levels of pollution can also experience increased fog due to the presence of particulates in the air.
That would be a stratus cloud.
That would be a stratus cloud.