Atmospheric perspective occurs when objects in the distance appear lighter, bluer, and less detailed due to the scattering of light by the atmosphere. This phenomenon is often used in art to create depth and a sense of distance in landscapes. As the distance increases, colors become more muted and hazy, mimicking the effects of air and moisture on visibility. It helps convey a three-dimensional space on a two-dimensional surface.
The layer of the atmosphere that contains all atmospheric storms is the troposphere. This is the lowest layer of the atmosphere, where most of Earth's weather occurs. Within the troposphere, storms such as thunderstorms, hurricanes, and tornadoes can develop due to the mixing of warm and cold air masses.
The troposphere, where all weather occurs, is the lowest and densest layer in the atmosphereIt is the lowest atmospheric layer. It is also the densest layer, containing 90% of the atmosphere's total mass. Almost all of the earth's carbon dioxide, water vapor.
A storm surge occurs over water. It is a rising of the sea as a result of atmospheric pressure changes and wind associated with a storm.
The five forms of precipitation are rain, snow, sleet, hail, and drizzle. Each form occurs depending on the temperature and atmospheric conditions in the atmosphere.
Water's boiling point decreases with increases in elevation due to the reduction in atmospheric pressure at higher altitudes. Boiling occurs when the vapor pressure of the liquid equals the surrounding atmospheric pressure. As altitude increases, the lower atmospheric pressure means that water can reach its boiling point at a lower temperature. This is why, for example, water boils at a temperature lower than 100°C in mountainous regions.
aerial perspective
Steve
Giotto contributed to the Renaissance's use of atmospheric perspective as he showed he showed it first in his artworks. Gentile da Fabriano's Adoration of the Magi (1422) would be the first one in the period but Masaccio's Tribute Money (1426) is the first one which showed the accurate use of atmospheric perspective.
Linear perspective is about the size and proportions of objects represented in a piece. Atmospheric perspective is about the clarity and detail of these objects. Most art that tries to replicate 3-dimensional scenes in 2-dimensions uses both.
Many paintings offer an illustration of both atmospheric and linear perspective, I would recommend Looking at Claude Lorrain's 1648 oil painting "Embarkation of the Queen of Sheba". Linear perspective can be seen by the straight lines which angle in towards the sun on the horizon. Atmospheric perspective can be seen by the way the closest building is detailed and the farther buildings have less detail.
Atmospheric
The term atmospheric perspective was coined by Leonardo da Vinci to describe the visual effect where objects appear to change in color and detail as they recede into the distance due to the presence of air particles.
Linear perspective is created by making closer objects appear larger than farther objects, proportionate to the distance between lines that recede towards a vanishing point on the horizon. Atmospheric perspective shows objects that are closer to the foreground with more detail than objects that are farther away. Realistic artworks normally use both.
Rain typically occurs in low atmospheric pressure systems where air rises, cools, and condenses to form clouds and precipitation. High atmospheric pressure systems typically bring stable and clear weather conditions with less likelihood of rain.
boiling
atmospheric perspective
aerial atmospheric perspective