barometric
Humidity typically increases before precipitation. As moisture in the air rises and cools, it condenses into water droplets, leading to cloud formation and eventual rainfall. This increase in humidity often occurs as warm, moist air is lifted and cools in the atmosphere.
Relative humidity usually increases before precipitation occurs. As air cools and reaches its dew point, the relative humidity increases due to the saturation of moisture in the air, leading to the formation of clouds and eventually precipitation.
precipitation means any thing wet that falls from the sky and usually has a cloud were it came from.
Clouds, then Precipitation, usually in the form of rain.
TRUE
The clouds that usually produces precipitation are called cumulus, cumulonimbus and nimbostratus clouds. These clouds are in the lowest level of the atmosphere.
the total varible cost is inverted S because The varible cost increases t n decreasing rte in the starting stages then increases t n increasing rte due to law of variable proportions
Liquid water falling from the atmosphere is called precipitation. It occurs in various forms, including rain, drizzle, and in warmer conditions, it usually takes the shape of droplets. Precipitation is a crucial part of the water cycle, helping to replenish Earth's water sources.
Light precipitation refers to any form of water falling from the atmosphere (such as rain, drizzle, or snow) in small amounts. It is usually characterized by low intensity and can vary in size of droplets or flakes.
Unstable atmosphere often leads to conditions with high winds and precipitation. This can result in severe weather events such as thunderstorms, heavy rain, and strong winds. These conditions are common during periods of rapid temperature changes and the presence of atmospheric instability.
A dependent variable is usually on the side of the equation by itself. The independent variable usually has something being done to it. And, the dependent variable is usually written to the left of the equation.
Stratus clouds are typically found in the lower portion of the atmosphere, usually below 6,500 feet. They are characterized by their flat, layered appearance and often bring overcast conditions and light precipitation.