The temperature at which air becomes saturated and produces dew
Yes, temperature and dewpoint are related. Dewpoint is the temperature at which air becomes saturated with water vapor and begins to condense into liquid. When the temperature equals the dewpoint, the air is saturated and relative humidity is 100%.
The word that goes with that definition is "door."
No, a drawing of an atom is not a scientific definition. A scientific definition of an atom would describe it as the smallest unit of matter that retains the properties of an element.
Electrical charge is a fundamental property of matter that determines how it interacts with electromagnetic fields. To choose the appropriate definition, one should consider the context in which the term is being used and select the definition that best fits that context.
The definition of sunset is determined by the moment when the upper edge of the sun disappears below the horizon.
psychrometera hygrometer would be useful!
Yes, temperature and dewpoint are related. Dewpoint is the temperature at which air becomes saturated with water vapor and begins to condense into liquid. When the temperature equals the dewpoint, the air is saturated and relative humidity is 100%.
That would be "dewpoint"...When the air temperature falls to the dewpoint (or dewpoint rises to the air temperature), then you have 100% relative humidity.
dewpoint apparatus
It is called the dewpoint.
Dewpoint
The dewpoint in this case would be approximately 12 degrees Celsius.
The approximate dewpoint temperature can be calculated using the difference between the dry-bulb and wet-bulb temperatures. In this case, the difference is 5 degrees Celsius. The dewpoint temperature is approximately 21 degrees Celsius.
A dewpoint temperature between 0°C and 10°C indicates that the air is relatively humid, but not excessively so. It means that the air is slightly moist but still comfortable.
The temperature to which air must be cooled to become saturated.
In areas covered by fog, the air temperature is typically close to the dewpoint temperature. This is because fog forms when the air temperature cools to the dewpoint temperature, causing water vapor in the air to condense into tiny water droplets that make up the fog.
There aren't many. Relative humidity isn't usually of much interest to serious meteorologist. Stations report dewpoint; calculating RH is another step. Intellicast.com (see link) has national RH maps. I usually get my humidity information from dewpoint maps from weather.unisys.com. Contour plots of dewpoint (related link) are among of the most useful.