Factors driving the change in magnitude of water stores over time and space— Condensation, Precipitation and Cloud Formation Flashcards
Define condensation
. When water vapour changes state to become a liquid — it loses energy to the surroundings
Causes of warm air to cool (condensation), leading to precipitation
. Air containing water vapour needs to cool to its dew point but the volume of air remains constant. This occurs when:
— warm moist air passes over a cold surface
— In winter night, when heat is radiated out to space and the grounds get colder, cooling the air directly in contact with it
. When volume of air increases but there is NO addition of heat, instead there’s adiabatic cooling . Lower pressure exists at higher altitudes. This happens when air rises and expands in the lower pressure of the atmosphere. This happens due to:
Topography — when air meets mountains, it’s forced to rise, causing it to cool. This results in orographic precipitation
Other air masses — Warm air is less dense than cool air. As result when warm air meets cold air, the warm air forced up above the cool air. It cools down as it rises This results in frontal precipitation.
Convection — when the sun heats up the ground, moisture on the ground evaporates and rises up in a column of warm air. As it gets higher, it cools. This results in convective precipitation.
Define dew point
The temperature at which water changes from gas to a liquid.
Why does condensation leading to precipitation happen?
. As air cools it is able to hold less water
. If cooled sufficiently, air will get to a temperature at which it becomes fully saturated with water vapour. This is the dew point
. Excess water in the air will then be converted to liquid water in this process
Factors that affect size / rate of condensation
. Amount of water vapour in the atmosphere — more water vapour in the the air, the higher the condensation rate
. Size of temperature drop — if there’s a rapid or large drop in temperature, condensation will be high
. Air pressure — the lower the pressure, the higher the condensation. If there is a fall in pressure, it is air is able to hold less water.
Define adiabatic cooling
. the process of reducing heat through a change in air pressure caused by volume
What is the cause of precipitation?
Condensation
Define precipitation
.Precipitation is any liquid or frozen water that forms in the atmosphere and falls to the Earth
How do clouds form, leading to precipitation?
- )Heat from the sun warms the ground, causing warm air with water vapour to rise
- ) Cloud formation is due to water vapour in the atmosphere becoming concentrated due to cooling of air and increase in water vapour
- )Clouds form when warm air to cools down, causing the water vapour in it to condense into water droplets or ice crystals, which gather as clouds
- )Water droplets caused by condensation are too small to form clouds on their own. For clouds to form, there have to be tiny particles of other substances (e.g dust or soot) to act as cloud condensation nuclei. They give water a surface to condense on. This encourages clouds to form, rather than allowing the moist air to disperse.
- )When the water droplets gathered get big enough, they fall as precipitation
Define Topography
the arrangement of the natural and artificial physical features of an area.
Examples of precipitation
. Snow . Rain . Hail . Sleet . Ice crystals
How do cloud formation and precipitation vary in regards to time and space?
. Seasonally — e.g. in the UK there’s more rainfall in the winter than the summer
. Location — e.g. precipitation tends to be higher in the tropics than at the poles as cold air cannot hold as much water vapour. Remember this is as cold air can’t as much water vapour as warm air.
Are clouds gas?
. Although clouds look like they are made out of gas, they are actually a large mass of water droplets of liquid water or ice crystals
Name the three types of precipitation
. Convective precipitation
. Orographic precipitation
. Frontal precipitation
Define condensation nuclei
. tiny particles (e.g. dust) in the atmosphere where water vapour condenses on.