The Factors That Affect The Formation Of Certain Fogs

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.

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

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

Condensation As the evaporated water vapor gets colder rising into the atmosphere, it changes back into different levels of liquid clouds of different types.

When dry ice is mixed with hot water, it can produce quick bubbling water and a lot of fog. Dry ice produces fog because its cold temperature of -109.3deg F or -78.5deg C, when put in water, it produces a cloud of water vapor fog. When the water get lower than 50deg F. it stops producing fog. Dry ice will smoke longer on a damp day than a dry day.

The study area is subject to easterly prevailing winds, generally tending to the south-east during the morning, particularly from January through September and changing to easterly or north-easterly in the afternoons. Dry westerly winds are typically experienced during the winter months of June and July. Relative humidity remains fairly constant throughout the year, averaging 71% during the morning and decreasing to around 68% on average in the afternoons, with November typically averaging the lowest morning humidity levels and July experiencing the lowest average afternoon relative humidity. While high relative humidity is generally not conducive with bushfire, and the prevailing winds are from the east, it is noted that conditions and associated bushfire hazard and risk within the site will vary on a daily, seasonal and annual

Dolores-induced moisture will arrive in the Los Angeles metropolitan area this weekend, bring the chance of a shower or thunderstorm during the afternoon hours on Saturday and Sunday.

Every winter the Central Valley experiences radiation fog that forms across the area. The Central Valley in California has ideal conditions for radiation fog to form. The valley is between a coastal mountain range on the West Coast and on the east side is where the Sierra Nevada mountains sit (Herckes, et. Al). Due to this topography of this area air masses become stagnant and ventilation of the valley is hindered (Herckes, et. Al). The lack of ventilation in the valley leads to temperature inversions, because of high pressure systems that form of the Great Basin (Herckes, et. Al). This leads to radiation fog forming because of inversion during nights in which a layer of moist air is below a layer of drier air (Ahrens and Sampson 97).

I sit in this AP Language and Composition class trying to decipher the essence of the unending annotations and floods of random texts for the past quarter. Little did I know that I would be taking flight and soaring through the smallest details and threads of literary devices and techniques of analyzing language. Before this class, I looked at a book, aware that it was filled with potential symbolism and crucial themes that were definitely worth considering. Yet, I often paid far less attention to the way words are crafted in efforts to create a beautiful masterpiece. Who knew that the jargon used in Snow Falling on Cedars could significantly shape the overall tone of the book? From the years leading up to this class, the

What weather can be so dangerous that it killed ye twelve thousand people in London, during the year 1952? Fog did! But how could ye fog be so dangerous? Well normally ye fog is not that dangerous, it is only a low-lying, thick or thin, cloud that touches the ground, but different types of fog are dangerous. Fog forms when the water vapor condenses and combines with monocles in the air making the droplets of water that hang in midair. Henceforth Fog is formed, and since the air has to have plenty of water vapor in the air for fog to form, the air has to be very humid. In fact, Newfoundland is the foggiest place in the world because it is very VERY humid. However, that is not the only thing fog needs. This fog also has to have some air

You may not think much when you look outside and see fog. However, it hasn’t always been around. We only have fog because of the everlasting conflict between Cirria, the god of the clouds, and Galia, the goddess of the wind.

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

episode. Normally, during the day the air near the surface is heated and as it