A measurement of how much water vapor is in the air at any particular place is called relative humidity. Relative humidity is measured with a psychrometer.
Humidity is a measure of the amount of water vapor present in the air compared to the maximum amount the air can hold at a specific temperature. It is often expressed as a percentage with higher values indicating air that is closer to being saturated.
it doesn't depend on the temperature but depends on how much water was evaporated
Yes, saturation can occur in cold water. Saturation refers to the point at which a solution can no longer dissolve additional solute, and this can happen regardless of temperature. However, the amount of solute that cold water can dissolve is generally lower than that of warm water due to decreased molecular activity, which affects solubility. Therefore, while saturation can occur in cold water, the specific solute's solubility limit will be lower compared to warmer temperatures.
Measurable characteristics are attributes or traits that can be quantified or assessed using a specific measurement scale or method. These characteristics can be objectively observed, documented, and compared. Examples include length, weight, temperature, and time.
Relative humidity is a measure of the amount of moisture in the air compared to the maximum amount of moisture the air can hold at a specific temperature. It is expressed as a percentage and indicates how close the air is to saturation.
Realative humidity
Realative humidity
The temperature at which air reaches saturation is called the dew point temperature. At this temperature, the air is holding the maximum amount of water vapor it can hold at that specific temperature, leading to condensation or saturation.
Humidity is a measure of the amount of water vapor present in the air compared to the maximum amount the air can hold at a specific temperature. It is often expressed as a percentage with higher values indicating air that is closer to being saturated.
The temperature at which air reaches saturation is called the dew point. At the dew point, the air is holding the maximum amount of water vapor that it can at that specific temperature before it begins to condense into liquid water.
it doesn't depend on the temperature but depends on how much water was evaporated
The blast saturation term is basically referring to the boiling point. Everything has a different boiling temperature so please be more specific about what you want to know.
Relative humidity is the amount of water vapor present in the air compared to the maximum amount the air can hold at a specific temperature. It is calculated by dividing the actual water vapor pressure by the saturation water vapor pressure at that temperature, and then multiplying by 100 to get a percentage.
The amount of water actually contained in air compared to the amount it could contain is known as relative humidity.
Perhaps you mean 'who discovered that thermal properties of materials vary with the temperature at which the measurement is done'. I don't know of a specific answer, but almost anyone who made a thermal measurement could have noticed this.
Temperature and thermal heat are related but not the same. Temperature is a measure of the average kinetic energy of particles in a substance, while thermal heat is the total amount of internal energy contained in a substance due to the movement of its particles. Temperature is a specific measurement, while thermal heat reflects the overall energy content of a substance.
Measurable characteristics are attributes or traits that can be quantified or assessed using a specific measurement scale or method. These characteristics can be objectively observed, documented, and compared. Examples include length, weight, temperature, and time.