Unit 2 Notes Flashcards
When does precipitation form?
When water vapour condenses, and requires a condensation nuclei, and cooling below the dew point.
What is the condensation nuclei?
A small particle around which condensation can take place.
What is the dew point?
The temperature at which condensation occurs, depends upon the humidity of the air.
What happens as altitude increases?
Temperature decreases.
What is the lapse rate?
The change in temperature with altitude.
How does the lapse rate change temperature?
Temperature drops between 6.5-9.8 degrees for every 1000m increase in altitude.
What are the main mechanisms of air uplift producing rainfall?
Orographic rainfall, relief rainfall, frontal rainfall.
What happens if there is a positive correlation between topography and rainfall?
There will be more rainfall under a higher altitude.
How is orographic rainfall formed?
Air blows up into an area of high altitude, forced upwards. Air cools, reaches dew point, condensation occurs. Water vapour changes into a liquid.
Where is orographic rainfall found?
Upland western regions of the UK, Westerly winds from the Atlantic Ocean. Rise over areas like Dartmoor, Snowdonia, Lake district.
What are the first two steps of convectional rainfall forming?
Energy of the sun heats the earth’s surface, causes water to evaporate, changes to water vapour, Warm, moist air rises, boils, reaches dew point, results in condensation.
What are the final two steps of convectional rainfall forming?
Leads to development of cumulonimbus clouds, as clouds continue to grow. Weight of water droplets leads to precipitation.
Where is convectional rainfall found?
Tropical rainforests, Tropical climates. South east of the UK in Summer.
What are the first two steps of frontal rainfall forming?
Two air masses of different temperature and density meet, but don’t mix. A front is the boundary separating two different air masses.
What are the final two steps of frontal rainfall forming?
As cold air is denser than warm air, warm air is forced upwards. As it rises, cools and reaches dew point, resulting in condensation and water vapour.
Where is frontal rainfall found?
The UK, where warm tropical air collides with warm polar air.
What are the two main mechanisms of precipitation?
Bergeron - Findeisen theory of ice-crystal growth, Collision mechanism.
What are the first two steps of the Bergeron - Findeisen theory?
Occurs in clouds where temperatures are just below 0 degrees, higher latitudes, and higher altitudes. Water vapour droplets can become supercooled, stay as a liquid below the normal point of freezing.
What are the next two steps of the Bergeron - Findeisen theory?
Dust particles act as condensation nuclei, and allow droplets to freeze. Upon contact with other supercooled droplets, they will also freeze, enables snowflakes to form.
What is the final step of the Bergeron - Findeisen theory?
Eventually, large snowflake becomes too heavy to be kept aloft.
Where does the Bergeron - Findeisen theory operate?
Over the UK, where cloud temperatures are below 5 degrees, and temperatures close to the ground remain below 2 degrees, snow reaches the ground.
What are the first two steps of the collision mechanism?
Explains the formation of rain in tropics where cloud temperatures are too high for ice crystals to form. Super sized condensation nuclei around which very large water droplets form.
What are the final two steps of the collision mechanism?
Larger super droplets fall and collide with smaller droplets. Associated with conventional rainfall resulting in heavy downfall pours and flash flooding, because of infiltration - excess overland flow.
What is excess runoff?
The rate at which the rain falls is greater than the rate at which it can infiltrate into the ground.