Precipitation Air becomes saturated - Search results - Wiki Precipitation Air Becomes Saturated
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METAR codes for each phenomenon. Precipitation occurs when evapotranspiration takes place and local air becomes saturated with water vapor, and so can no... |
possibly acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce... |
orographic—causes air containing invisible water vapor to rise and cool to its dew point, the temperature at which the air becomes saturated. The main mechanism... |
Lapse rate (redirect from Absolute stable air) contains latent heat of vaporization. As a parcel of air rises and cools, it eventually becomes saturated; that is, the vapor pressure of water in equilibrium... |
which funnels cool air down a stretch of land east of the mountains. The higher the mountain chain, the deeper the cold air mass becomes lodged to its east... |
glufosinate herbicides. Ammonium sulfate precipitation is a common method for protein purification by precipitation. As the ionic strength of a solution increases... |
Electrostatic precipitator (redirect from Electrostatic Precipitation) electrostatic precipitator (WESP or wet ESP) operates with water vapor saturated air streams (100% relative humidity). WESPs are commonly used to remove... |
Supercell (redirect from High precipitation supercell) This wet, cold air quickly saturates as it is lifted by the updraft, forming a cloud that seems to "descend" from the precipitation-free base. Wall clouds... |
Supersaturation (redirect from Super-saturated) superheated steam at the inlet, which transitions to saturated state at the outlet. Supersaturation thus becomes an important factor to be taken into account... |
Rain (section Water-saturated air) temperature. Warmer air can contain more water vapor than cooler air before becoming saturated. Therefore, one way to saturate a parcel of air is to cool it... |
Fog (redirect from Precipitation fog) the air cannot hold additional moisture, thus, the air will become supersaturated if additional moisture is added. Fog commonly produces precipitation in... |
Lake-effect snow (redirect from Lake-effect precipitation) layer with more time to become saturated with water vapor and for heat energy to move from the water to the air. As the air mass reaches the other side of... |
and air temperatures, insolation, and wind all affect this. A dryland is a place where annual potential evaporation exceeds annual precipitation. Often... |
Humidity (redirect from Air humidity) in the air. Water vapor, the gaseous state of water, is generally invisible to the human eye. Humidity indicates the likelihood for precipitation, dew,... |
Thundersnow (section Lake effect precipitation) 50 km/h (31 mph) is required so that the air passing over the lake or ocean water will become sufficiently saturated with moisture and will acquire thermal... |
Tillandsia (redirect from Air Plant) branches of trees, in deserts and on other substrates that will not be saturated with water for very long. Tillandsia are perennial herbaceous plants which... |
companion tornado. saturated adiabat A curved line drawn on a thermodynamic diagram that traces the path of a moisture-saturated air parcel as it moves... |
factor affecting the time until soil becomes saturated. This runoff is called saturation excess overland flow, saturated overland flow, or Dunne runoff. Soil... |
Cloud (category Clouds, fog and precipitation) cause a parcel of air containing invisible water vapor to rise and cool to its dew point, the temperature at which the air becomes saturated. The main mechanism... |
Extreme weather (redirect from Extreme precipitation) the movement of air. Areas along the coast or located in tropical regions are more likely to experience storms with heavy precipitation than temperate... |