Humidity refers to the amount of water vapor present in the air. It is an important factor in the Earth's atmosphere as it influences weather patterns, and has significant effects on human comfort, health, and the environment.
Types of Humidity
There are several ways to measure and express humidity:
Relative Humidity: This is the most commonly used measure of humidity. It is expressed as a percentage and indicates the amount of water vapor present in the air compared to the maximum amount the air could hold at the same temperature. For example, a relative humidity of 50% means the air is holding half of the maximum water vapor it can hold at that temperature.
Absolute Humidity: This measures the actual amount of water vapor present in a unit volume of air, typically expressed in grams per cubic meter.
Specific Humidity: This is the ratio of the mass of water vapor to the total mass of moist air parcel. It's usually expressed in grams of water vapor per kilogram of air.
Factors Affecting Humidity
Several factors influence humidity levels:
Temperature: Warmer air can hold more water vapor than cooler air. As a result, the relative humidity of warm air will be lower than that of cooler air, even if the actual amount of water vapor is the same.
Human Comfort: High humidity levels can make it feel hotter than it actually is because the body's ability to cool itself through sweat evaporation is reduced. Conversely, low humidity can lead to dry skin and respiratory issues.
Health: Extreme humidity levels can contribute to the growth of mold and bacteria, affecting indoor air quality and potentially causing respiratory problems.
Measuring Humidity
Humidity is measured using instruments called hygrometers. These devices can measure relative humidity, absolute humidity, and other humidity-related parameters, providing valuable data for various applications such as weather forecasting, agriculture, and industrial processes.
Earth/Space Science: Students will use scientific skills and processes to explain the chemical and physical interactions (i.e., natural forces and cycles, transfer of energy) of the environment, Earth, and the universe that occur over time.
Earth History: Explain how sedimentary rock is formed periodically, embedding plant and animal remains and leaving a record of the sequence in which the plants and animals appeared and disappeared.
Explain how sedimentary rock buried deep enough may be reformed by pressure and heat and these reformed rock layers may be forced up again to become land surface and even mountains.
Explain why some fossils found in the top layers of sedimentary rock are older then those found beneath in lower layers: Folding; Breaking; Uplift; Faulting; Tilting.