What is this in meteorology?
sea smoke is a meteorological event caused by the interaction of cold air and warm water. Sea smoke, which is often observed in coastal areas, is sometimes known as advice or steam fog and has a clear appearance that can cause water water to appear or steaming. Sea smoke often disperses rapidly, due to the warming effect of the ocean on the freezing air.
When cold air, such as the wind from polar regions, reaches a relatively warm area of water, sea smoke can be formed on the surface. Warm air contains more water vapor than cold air and is lighter, which increases the speed at which it rises from the surface. The naturally occurring warm air just above the water level rises faster than the icy polar air above it and adds water vapor to the cool layer. Because cold air is unable to absorb most water vapor, warm air condenses as it rises. Condensation action is what allows sea smoke to become visible as well as warmThe breath becomes Visible in the cold air on a cold day.
Since sea smoke is created by air just above the climb and condensation of water, it has a unique appearance that leads to its name. Instead of the low shore of the fog, sea smoke is the form of large clouds of gray or white air and rises from the surface of the water. Long vertical cords of smoke can rise separately, especially in areas where there is low wind speed, giving the water levels the appearance of smoldering lava fields. In higher wind areas, smoke can connect into a thick fog layer that may pose a risk of visibility for ships.
Despite the potential of visibility problems, sea smoke rarely pose a serious risk. Because the effect is caused by a warm air rising by cold air, the smoke disperses and disappears as the air temperature rises. As the growing heat spreads through colder air, it will be absorbMore, leading to a reduction in conditional and smoke scattering. Smoke rarely condenses into extremely large banks, because simple warming actions of rising air limits the amount of space that can be overtaken before disappearance. Although sea smoke may occur on almost any kind of water, it often occurs in the northern Atlantic ocean when transfer of polar air from the polar region passes through the somewhat warmer area of the ocean.