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The greatest amount of daily weather change typically occurs in areas with a continental climate, away from large bodies of water. These regions experience larger temperature swings between day and night due to the lack of moderating influence from nearby bodies of water.
The amount of water vapor that air can hold depends on its temperature. Warmer air can hold more water vapor than cooler air. This relationship is described by the concept of relative humidity, which is the ratio of the amount of water vapor present in the air to the maximum amount the air could hold at that temperature.
Yes, 99% of weather occurs in the troposphere because the tropopause, the temperature boundary between the troposphere and stratosphere, disallows formation of clouds and weather due to the separation of low temperatures in the troposphere and higher temperatures in the stratosphere. This boundary is only rarely breached.
Relative humidity is the ratio of the partial pressure of water vapour to the saturation vapour pressure of water at the same temperature. Relative humidity depends on temperature and the pressure. Very roughly speaking, it is a ratio of the amount of water vapour in the air compared to the total amount of water vapour that it possible for that air to contain.
temperature
troposphere
The characteristic that allows the troposphere to contain a significant amount of water vapour is its ability to hold moisture through temperature regulation. The warmer the air, the more water vapor it can hold. This is because warm air has a higher capacity to hold water vapor compared to cold air.
The troposphere. The troposphere is one of the four layers of the atmosphere (0-10km in altitude) containing water vapour. Clouds are formed by water condensing and as air cools. This is why cloud formation is possible because the temperature of the troposphere decreases with altitude.
The atmospheric layer that has the greatest range of temperature is the troposphere. In the troposphere, water vapor plays a huge role in the fluctuation of temperatures.
The layer of the atmosphere with the greatest amount of water vapor is the troposphere. This is the lowest layer of the atmosphere and is where most weather events occur. Water vapor plays a crucial role in cloud formation, precipitation, and other atmospheric processes in the troposphere.
William J. Gutowski has written: 'Temperature-dependent daily variability of precipitable water in special sensor microwave/imager observations' -- subject(s): Satellite observation, Microwave imagery, Ocean surface, Precipitation particle measurement, Sea surface temperature, Temperature distribution, Air water interactions, Precipitation (Meteorology), Water vapor
temperature plays a role in humidity
No, the amount of water does not affect its temperature. The temperature of water is determined by the amount of heat energy it contains, regardless of the quantity of water present.
You need the amount of water, the temperature of the water, and the desired temperature.
The troposphere is the lowest layer of the Earth's atmosphere where most weather occurs. Cloud formation in the troposphere depends on factors such as temperature, humidity, and atmospheric dynamics. If these conditions are not favorable, there may be few or no clouds present in the troposphere.
The troposphere can hold water vapor because it has the right temperature and pressure conditions for evaporation to occur. As air near the Earth's surface warms, it can hold more water vapor. When the warm air rises through the troposphere, it cools down, causing the water vapor to condense and form clouds and precipitation.
temperature plays a role in humidity