A strong warm wind will speed up evaporation giving us higher rates of evaporation in compared to a still cool day
These are all variables used to calculate evaporation rate: The larger the surface area the higher the evaporation (rate) The higher the wind speed the higher the evaporation (rate) The higher the temperature the higher the evaporation (rate) The higher the relative humidity the lower the evaporation (rate)
By carrying away moisture the wind allows air with a greater ability to absorb evaporation and so increased evaporation will occur (until equilibrium in vapor pressure is reached).
Steam is a form of visible evaporation.
No only the speed of light can
wind aids removing the evaporated water from of zone of evaporation and consequently creates grater scope for evaporation.
A strong warm wind will speed up evaporation giving us higher rates of evaporation in compared to a still cool day
A strong warm wind will speed up evaporation giving us higher rates of evaporation in compared to a still cool day
Evaporation is one of the 3 types of boiling.
Clouds can form from sea water evaporation during night or day. Basically it depends on wind strength and air temperature.
Wind
Adjust the temperature. This is very fidgety if you want evaporation to occur at a particular rate. But try lowering the temperature back towards the boiling point (for a liquid is 100 degrees celcius) but not below because the evaporation process will stop.
Evaporation Fog Wind Precipitation
Wind or air movement also promotes evaporation. Evaporation is also much faster in a vacuum.
These are all variables used to calculate evaporation rate: The larger the surface area the higher the evaporation (rate) The higher the wind speed the higher the evaporation (rate) The higher the temperature the higher the evaporation (rate) The higher the relative humidity the lower the evaporation (rate)
By carrying away moisture the wind allows air with a greater ability to absorb evaporation and so increased evaporation will occur (until equilibrium in vapor pressure is reached).
by wind