bathroom
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.
A trough on an upper level isobaric chart indicates an area of relatively lower pressure aloft. This typically corresponds to an area of rising air and potential for unsettled weather, such as clouds, precipitation, and atmospheric instability. Troughs are often associated with the formation of weather systems like low pressure systems or storm development.
A NorLun trough is a inverted trough that usually occurs along northeast coast of the United States. It generally extends from the surface up to near 850 or 800 mb. Winds around the trough are convergent and light. This helps to keep the trough in place to produce heavy snow. Another important ingredient for a NorLun trough is to have steep lapse rates in the lower part of the atmosphere...again generally from 800 mb and below.
Warm air aloft is usually associated with stable atmospheric conditions. It can lead to fair weather with minimal cloud cover, as the warm air sits above cooler air at the surface, preventing vertical movement and thus inhibiting cloud formation and precipitation.
Weather balloons typically stay aloft in the atmosphere for about 12 to 24 hours before they burst and fall back to the ground.
A surface low pressure is typically associated with a trough on an upper level isobaric chart. This is because the trough represents a region of lower pressure aloft which tends to enhance surface low pressure systems below. The interaction between the surface and upper-level features influences 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.
A trough is distinguished on the weather chart by system of isobars which appear sharply curved along a line .this curves are concave towards low pressure. Trough may be termed deep or shallow according to whether the curvature of the isobar is acute or gentle. The weather associated with a trough is generally cloudy with precipitation.
A trough on an upper level isobaric chart indicates an area of relatively lower pressure aloft. This typically corresponds to an area of rising air and potential for unsettled weather, such as clouds, precipitation, and atmospheric instability. Troughs are often associated with the formation of weather systems like low pressure systems or storm development.
I believe trough is high tide but I'm not 100% sure A trough is the low part of a wave, the opposite of crest.
Generally taken as the height between the crest and the preceding trough.
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.