Relative humidity is a ratio between the partial pressure of water vapor and the saturation pressure of water vapor at the current temperature and pressure. If the temperature and pressure change, then the relative humidity will change also. You are correct that higher temperatures allow the atmosphere to hold more water. That means that the saturation pressure of water vapor has increased while the current vapor pressure has remained the same, causing the relative humidity to drop. We think of humidity as how hot and sticky it is outside. The closer the water vapor pressure is to its saturation point, the more hot and sticky we feel. We associate humidity with heat since that is when we are uncomfortable, but rain is caused by the relative humidity rising to 100% because the humid air cooled to the point that the saturation pressure dipped below the current vapor pressure (or other pressure changes, or a combination of both). You can learn more at the link below. I hope this helps.
The word humidity does have a plural, humidities, but the state of "being humid" itself is uncountable. What we actually measure as humidity is the relative humidity, comparing it to the maximum possible at that pressure and temperature. Referring to these measurements as "relative humidities" would not be grammatically incorrect, but you could also use the singular just as well. ("We're going to compare the relative humidity in Texas and Oklahoma.")
As temperature increases, air's capacity to hold water vapor also increases. If the air's relative humidity remains constant while temperature rises, it will eventually reach saturation as it approaches its new higher dew point temperature. This process, known as adiabatic cooling, can lead to cloud formation and precipitation.
Evaporation is the process by which a liquid turns into a gas, while relative humidity is the ratio of the amount of water vapor present in the air compared to the maximum amount the air can hold at a specific temperature. A higher relative humidity means the air is already holding a lot of water vapor and so evaporation will be slower, while a lower relative humidity allows for faster evaporation as the air has more capacity to hold additional water vapor.
because land heats up and cools down very fast so at night when the sun is not there the land starts to cool down quickly and the excess of heat is sent back by long wave radiation
When temperature increases, humidity typically decreases. Warmer air can hold more moisture, so as the air's temperature rises, its capacity to hold water vapor also increases, resulting in a lower relative humidity. Conversely, when temperature drops, humidity tends to increase because cooler air can hold less moisture.
The Apparent Temperature, also known as the Heat Index, is a measure of how hot it feels when relative humidity is factored in with the actual air temperature. To calculate the Heat Index, you can use an online calculator or a chart. At an air temperature of 80°F and a relative humidity of 30%, the Apparent Temperature (Heat Index) would be around 80°F.
To determine the relative humidity of the air, you will need a hygrometer, which is a device that measures humidity. Additionally, a thermometer may be helpful to measure the temperature of the air, as relative humidity changes with temperature. A data logging device or paper and pen to record the measurements would also be necessary.
Specific humidity and relative humidity are related but measure different aspects of moisture in the air. Specific humidity is the actual amount of water vapor present in the air, while relative humidity is the ratio of the amount of water vapor present to the maximum amount of water vapor the air can hold at a given temperature. In general, as specific humidity increases, relative humidity also increases because the air is closer to its saturation point. However, changes in temperature can affect this relationship.
Relative humidity is a ratio between the partial pressure of water vapor and the saturation pressure of water vapor at the current temperature and pressure. If the temperature and pressure change, then the relative humidity will change also. You are correct that higher temperatures allow the atmosphere to hold more water. That means that the saturation pressure of water vapor has increased while the current vapor pressure has remained the same, causing the relative humidity to drop. We think of humidity as how hot and sticky it is outside. The closer the water vapor pressure is to its saturation point, the more hot and sticky we feel. We associate humidity with heat since that is when we are uncomfortable, but rain is caused by the relative humidity rising to 100% because the humid air cooled to the point that the saturation pressure dipped below the current vapor pressure (or other pressure changes, or a combination of both). You can learn more at the link below. I hope this helps.
The word humidity does have a plural, humidities, but the state of "being humid" itself is uncountable. What we actually measure as humidity is the relative humidity, comparing it to the maximum possible at that pressure and temperature. Referring to these measurements as "relative humidities" would not be grammatically incorrect, but you could also use the singular just as well. ("We're going to compare the relative humidity in Texas and Oklahoma.")
dry bulb temperature simply tells us the temperature of dry air.but the comfort also depends on humidity ie. water vapour presents in the air.Wet bulb temperature measures the humidity in the air.Because the evaporation of water in the bulb wick depends on the relative humidity of surrounding air.
As temperature increases, air's capacity to hold water vapor also increases. If the air's relative humidity remains constant while temperature rises, it will eventually reach saturation as it approaches its new higher dew point temperature. This process, known as adiabatic cooling, can lead to cloud formation and precipitation.
This is the temperature at which small spheres of dew will form on a smooth surface. As such it is a measure of relative humidity. It is also used as a measure of the goodness of desiccant materials such as P2O5, and CaSO4. i.e. the lowest relative humidity to which this material will dehydrate.
Evaporation is the process by which a liquid turns into a gas, while relative humidity is the ratio of the amount of water vapor present in the air compared to the maximum amount the air can hold at a specific temperature. A higher relative humidity means the air is already holding a lot of water vapor and so evaporation will be slower, while a lower relative humidity allows for faster evaporation as the air has more capacity to hold additional water vapor.
because land heats up and cools down very fast so at night when the sun is not there the land starts to cool down quickly and the excess of heat is sent back by long wave radiation
A psychrometer is a device used to measure the relative humidity in the air. It consists of two thermometers: a wet bulb and a dry bulb. By comparing the differences in temperature readings between the two thermometers, the relative humidity can be calculated.