Fog In North America

The process begins when the sun starts to heats up the surface which creates warm air. The warm, less heavy air rises and converges with the cold less heavy air above. This process is known as wind shears. Wind shears are when two

In a growing world, electricity production is becoming a problem due to coal fired electrical plants releasing millions of gallons of greenhouse gases, ecological problems with pollution in water, and health risks concerning workers and people living nearby. But with new technology and advances in renewable energy sources, wind energy is becoming one of the most popular energy sources for many states.

Clouds to form in the atmosphere have to have water vapor present. This water vapor makes up a cloud. The water vapor in the atmosphere comes from evaporation or deposition. Also the temperature of the air is below the dew point. When the water is fully saturated, it starts to rise and the expansional cooling process begins. During the process of condensation, the aerosol particles act like a nuclei in the atmosphere, which began to grow, creating ice crystals that are big enough to produce a cloud.

Condensation is the opposite of Evaporation. It is when saturated air cools down below the dew point which causes them molecules to stick together and from clouds. When we see clouds they don’t all look the same. This goes back to when the temperature causes the amount of water to evaporate. So that’s why clouds are all different shapes and sizes.

Clouds- Clouds are a mass of water or ice droplets in the air. An example of a

What is Mist?Mist is a substance that covers Mortal eyes so they can not see what is actually happening.

3. Windward side: humid air moves up the mountain’s slopes and cools to form clouds that produce precipitation; leeward side: the air is warm and very dry.

because the dew point is below freezing and the moisture goes from a gas to a

2. Wind power is generating electricity by collecting wind, and it saves energy in the world.

F. Nimbotratus – A dark gray continuous rain cloud resulting from a thickening altostratus. Thick enough to blot out the sun.

Realistically, fog obscures one’s vision and it renders the viewer “blind” to what’s around them due to the fact that the fog encapsulates the person in a visual area that is generally only immediately in front of you. For example, the purpose of a lighthouse is to

So the warm moist air creates clouds of rain and thunderstorm. Adding to that winds with different speed going in different directions assisting in expanding these great clouds of rain and thunderstorm. With

el nino is a warm band of water that periodically develops in the Pacific Ocean near the equator off western South America. El Niño—Spanish for “the child” because it often occurs around Christmas—occurs about once every two to seven years. El Niño can affect the weather in large parts of Asia, Africa, Indonesia, and North and South America, causing both floods and droughts. An El Niño event is often followed by a band of colder than normal ocean waters called La Niña, which is Spanish for “the girl.” La Niña produces the opposite weather conditions. Both of these phenomena cause changes in air pressure in the western Pacific. Together these two events are known as ENSO, or El Niño–Southern

They are known as rime and clear ice, and a mixture of the two is not uncommon. For rime ice to form, an aircraft needs to fly through an area of tiny super-cooled liquid drops. This super-cooled liquid is actually suspended in the cloud cover at temperatures already below freezing. Once the aircraft surface plows through this moisture, the drops are disrupted immediately adhere to and freeze before spreading out over the entire surface. This forms a rough and cloudy-white layer of ice known as rime. Even though the rime surface is rough and creates an airflow disturbance, it is lighter and easier to remove by deicing equipment than clear ice. For clear ice to form, larger sized super-cooled drops would need to be encountered. These larger droplets spread out over the surface and airfoils before freezing. This allows for the build-up of a clear, hard and slick layer of ice on the surface (Ahrens, 2009).

17) In calm winter conditions in NW Europe dense fog is cleared most effectively by"/>