A backdraft. This can happen in a chimney over a fireplace.
A backdrift
One phenomenon caused by the unequal heating of Earth's surface within a small area is a microclimate. Microclimates can occur due to variations in factors like elevation, vegetation, and urban development, leading to localized differences in temperature and humidity. For example, a city park may be cooler than the surrounding urban environment due to the presence of trees and greenery.
Local winds are winds that blow over short distances caused by unequal heating of the earths surface in a small area.
Type your answer here... local winds can be caused by whether fronts moving into the air and any local thing creating temperture difference
Local winds are winds that are influenced by local geographical features such as mountains, valleys, or bodies of water. They are usually short-lived and can vary in speed and direction, depending on the specific local conditions. Examples of local winds include sea breezes, valley breezes, and mountain winds.
Wind is caused by the uneven heating of the atmosphere. When an area has warmer air than surrounding areas, the air rises which creates a region of low pressure. The areas around it have higher pressure, and therefore air moves from there to the low pressure area. The movement of this air is called wind.
local winds-are winds that blow over short distances caused by unequal heating of the earths surface in a small area. global winds-are winds that blow around the earth from the north pole to the south pole.
The combination of convection cells found at every 30 degrees of latitude and the Coriolis effect produces patterns of air circulation called global winds. Local winds blow from any direction and move short distances. Local winds are caused by unequal heating within a small area.
How do you find the area of an unequal quadrangle?
Global convection currents are caused by the unequal heating of Earth's surface by the Sun. As the Sun's rays strike the equator more directly, the air at the equator becomes warmer and rises, creating a low-pressure area. This warm air then moves towards the poles and cools, sinking at around 30 degrees latitude, creating high-pressure areas that flow back towards the equator, completing the convection loop.
Frontal wedging
Winds move from areas of high pressure to areas of low pressure. The pressure difference is caused by the unequal heating of the atmosphere by the sun. As air moves from high to low pressure, the Coriolis effect, caused by the Earth's rotation, influences the direction of the wind. This creates global wind patterns that help redistribute heat around the planet.