Aerosols
Weather balloons typically stay aloft in the atmosphere for about 12 to 24 hours before they burst and fall back to the ground.
A trough aloft is generally associated with unstable weather conditions, such as the potential for thunderstorms, heavy rain, and strong winds. This is because a trough aloft represents a region of lower pressure in the upper atmosphere, which can lead to the development of unsettled weather patterns.
Cold air aloft is associated with a surface low pressure system. The reverse is true for warm air aloft. In a baroclinic low pressure system, the upper-level low/trough is usually situated over the cold air, while upper level highs/ridges are around warm air aloft.
Inversion aloft refers to a situation where the temperature in the atmosphere increases with height instead of decreasing, as is typically the case. This can lead to stable atmospheric conditions that inhibit vertical mixing of air and can result in trapped pollutants or fog at the surface. Inversions aloft are common in certain weather patterns, such as high pressure systems.
The predominance of westerly flow aloft is due to the rotation of the Earth, which creates the Coriolis effect. This effect deflects moving air to the right in the Northern Hemisphere and to the left in the Southern Hemisphere, resulting in the westerly flow pattern. Additionally, the positioning and movement of high and low-pressure systems in the atmosphere play a role in maintaining this dominant westerly flow at upper levels.
Weather balloons typically stay aloft in the atmosphere for about 12 to 24 hours before they burst and fall back to the ground.
"Winds aloft" refers to the wind patterns and speeds at higher altitudes in the atmosphere, typically above the surface layer. These winds are crucial for aviation, as they can significantly affect flight paths, fuel efficiency, and weather patterns. Meteorologists analyze winds aloft to forecast weather changes and to understand atmospheric dynamics, as they play a key role in the movement of air masses and storm systems.
A trough aloft is generally associated with unstable weather conditions, such as the potential for thunderstorms, heavy rain, and strong winds. This is because a trough aloft represents a region of lower pressure in the upper atmosphere, which can lead to the development of unsettled weather patterns.
The plane was flying aloft.
Aloft is an antonym for below or down.
The drawers were aloft , and I am too short to reach.
There were three flags aloft.
The Borrowers Aloft was created in 1961.
Aloft Hotels was created in 2005.
Allfighters shouldbe aloft within ten minutes. Please go aloft and furlthat mizzen topsail.
Cold air aloft is associated with a surface low pressure system. The reverse is true for warm air aloft. In a baroclinic low pressure system, the upper-level low/trough is usually situated over the cold air, while upper level highs/ridges are around warm air aloft.
Inversion aloft refers to a situation where the temperature in the atmosphere increases with height instead of decreasing, as is typically the case. This can lead to stable atmospheric conditions that inhibit vertical mixing of air and can result in trapped pollutants or fog at the surface. Inversions aloft are common in certain weather patterns, such as high pressure systems.