Newark is the most populous city in New Jersey. It lies in the shift between a humid continental and humid subtropical climate. During a lazy stroll in the afternoon, I observed three distinct types of clouds. The most common is the Cumulus, which often appears on clear sunny afternoons when the sun scorches the earth directly. Their tops are rounded and brilliant white when exposed to the sun while their bottoms remain flat and sort of dark. If there is sufficient atmospheric instability and moisture then powerful updrafts are formed, leading to a deep, mature cumulonimbus. They develop from convection, with updrafts elevating into the atmosphere then condense into cotton-like clouds. I feel they are pleasant to watch on a calm afternoon.
Another type of clouds observable in mid-morning is the Altocumulus clouds. They are featured by gray patches that paint the sky in rounded masses. They appear like sheep’s wool, and when one lifts their hands to the sky in the trajectory of the cloud, the mound is often the size of the thumb. These clouds have vertical development, which can brew heavy rain, wild winds, lighting, and sometimes, tornadoes.
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Altocumulus clouds form through various, including; development via the breakup of altostratus and the elevation of moist air parcels cooled by subtle turbulence. They are often made up of droplets, consisting of ice crystals. This infers that precipitation from Altocumulus clouds is rare although it can be observed in the form of virga .
Perhaps I would like to discern how do we determine atmospheric stability? Are there factors that prompt air to rise and cool? In cloud development, is there a relationship between pressure gradient and temperature?
