Relative Humidity goes above 90%, that means there is dew or fog forming or has formed.
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A device to measure relative humidity in BC times was done with a simple twig placed parallel to the ground and mounted several feet up. When relative humidity increases, the twig points down, and when it decreases, the twig points up.
relative humidity is 100 percent.
Answeractuall humidity is given as the amount of water. use a table stating how much water the air can hold at the given temp, this is your 100% humidity. now calculate howw much you got and that would be relative humidityAnswer:To calculate relative humidity you need a wet bulb and a dry bulb thermometer and a psychrometric chart (a graph of the physical properties of moist air at a constant pressure). The chart graphically expresses how various properties relate to each other.Using an ordinary thermometer you read the dry bulb temperature(DBT). You will locate this temperature on the x-axis of the chart.Next you will determine the wet bulb temperature (WBT) from a thermometer who's bulb is covered with a wet wad of cotton and typically waved in the air until the temperature goes to its minimum. This works because dry air evaporates water and evaporation cools the wad. The temperature it reaches is related to the air's humidity. This value goes on the curved line at the top of the chart.The relative humidity (RH) is read off the chart from the intersection of the lines from these two points.
Yes, radiosonde instruments can measure dew points indirectly. They collect data on temperature and relative humidity as they ascend through the atmosphere. From these measurements, the dew point can be calculated using established formulas. This information is crucial for meteorological analysis and weather forecasting.
Because relative humidity changes with temperature. Air at 30 F and 90% humidity actually is holding less water than air at 90 F and 20% humidity. Dew point will give you a better idea of how much moisture is in the air because it doesn't change with temperature. For example, dew points in the 70's will always feel very sticky and uncomfortable because that is a lot of moisture in the air.
Given the relative humidities at various temperatures, calculate the absolute humidities (in grains of water per pound of air) at those temperatures. The absolute humidity of the ambient air is the saturation humidity multiplied by the percentage relative humidity and divided by 100: Habs = (Hsat )(RH / 100) where: Habs = absolute humidity at a given temp Hsat = saturation humidity at the same given temp RH = percentage relative humidity at the same given temp First, you must calculate the saturation humidity at each of your temperature data points: Hsat = (7000)(18.02 / 28.85)(PS)/(Pamb - PS) where: Hsat = grains of water per pound of air 7000 = grains per pound 18.02 = molecular weight of water 28.85 = molecular weight of dry air (taken as 79 vol % nitrogen, 21 vol % oxygen) PS = vapor pressure of water at temperature T Pamb = ambient pressure (You will need a good set of steam tables to look up the vapor pressure of water at each of your temperature data points) Example calculation of Hsat at 68 oF and an ambient atmospheric pressure of 14.696 psia: From the steam tables, the vapor pressure of water is 0.3389 psia at 68 oF. Hsat = (7000)(18.02/28.85)(0.3389)/(14.696 - 0.3389) = 103.2 grains of water/lb of air Now if your relative humidity data point at 68 oF was say 60%, then: Habs = (103.2)(60/100) = 61.9 grains of water/lb of air It is quite easy to set up a spreadsheet to convert your relative humidity data as per the above example ... then all that would be needed is to enter the water vapor pressure values at each of your temperature data points. You can also just use calculator apps to do it for you - like EZ Air: http://www.parkssoft.com/ezair.html
The design temperature in Kampala, Uganda is typically around 25-27 degrees Celsius, with humidity levels ranging from 70-80%. These values are used as reference points for building design and HVAC system sizing.
No, Fahrenheit and Kelvin are two different temperature scales. Kelvin is an absolute temperature scale based on the properties of matter, while Fahrenheit is a relative temperature scale based on the freezing and boiling points of water. They have different zero points and increments.
what are main points on temperature
I really don't think that's the convention for these regions - I think most places usually mention relative humidity. Dew point tends to be a more useful metric, especially for comfort in the summer.
Five points equals .5 carats where one carat equals 1.00 points.
Temperature is a measure of the average kinetic energy of the particles in a substance. It quantifies how hot or cold an object or environment is relative to a reference point, such as absolute zero or the freezing and boiling points of water.