Southern China: Relative humidity hits 100%
Posted: Wed Mar 13, 2024 6:04 pm
Southern China: Relative humidity hits 100%
Read more here:
https://www.chinagrammar.com/2024/03/so ... -hits.html
South China Morning Post on Youtube has the story.
Residents in southern China found themselves grappling with extreme dampness when relative humidity climbed to 100% on March 6, according to the Guangdong Meteorological Bureau. The moisture has swept through cities in the country’s south, causing water droplets to accumulate on ceilings.
Humidity is the concentration of water vapor present in the air. Water vapor, the gaseous state of water, is generally invisible to the human eye. Humidity indicates the likelihood for precipitation, dew, or fog to be present.
Humidity depends on the temperature and pressure of the system of interest. The same amount of water vapor results in higher relative humidity in cool air than warm air. A related parameter is the dew point. The amount of water vapor needed to achieve saturation increases as the temperature increases. As the temperature of a parcel of air decreases it will eventually reach the saturation point without adding or losing water mass. The amount of water vapor contained within a parcel of air can vary significantly. For example, a parcel of air near saturation may contain 28 g of water per cubic metre of air at 30 °C (86 °F), but only 8 g of water per cubic metre of air at 8 °C (46 °F).
Read more here:
https://www.chinagrammar.com/2024/03/so ... -hits.html
South China Morning Post on Youtube has the story.
Residents in southern China found themselves grappling with extreme dampness when relative humidity climbed to 100% on March 6, according to the Guangdong Meteorological Bureau. The moisture has swept through cities in the country’s south, causing water droplets to accumulate on ceilings.
Humidity is the concentration of water vapor present in the air. Water vapor, the gaseous state of water, is generally invisible to the human eye. Humidity indicates the likelihood for precipitation, dew, or fog to be present.
Humidity depends on the temperature and pressure of the system of interest. The same amount of water vapor results in higher relative humidity in cool air than warm air. A related parameter is the dew point. The amount of water vapor needed to achieve saturation increases as the temperature increases. As the temperature of a parcel of air decreases it will eventually reach the saturation point without adding or losing water mass. The amount of water vapor contained within a parcel of air can vary significantly. For example, a parcel of air near saturation may contain 28 g of water per cubic metre of air at 30 °C (86 °F), but only 8 g of water per cubic metre of air at 8 °C (46 °F).