Precipitation And Excess Runoff Within The Water Cycle Flashcards
Name the three types of precipitation
Orographic
Frontal
Conventional
Name the two competing theories on precipitation formation
The collision mechanism
The Bergeron-Findeisen process
How is conventional precipitation formed?
- Sun heats ground and warm air rises
- As air rises it begins to cool and water vapour condenses
- When saturation point is reached, large cumulonimbus clouds are formed
- Heavy rainfall occurs
How is frontal precipitation formed?
- Area of warm air meets area of cold air
- Warm air is forced over cold air due to different densities, creating the ‘front’
- The warm, less dense, air cools and water vapour condenses
- Clouds form and precipitation occurs
How is orographic precipitation formed?
- Moist air is lifted as it moves over a mountain range
- As air rise it cools and water vapour condenses forming clouds
- Most rainfall falls on mountain ridge, on Lee side of mountain rainfall is low (rain shadow)
- Alternating bands of cloud and rain shadow is known as orographic bounce
How do clouds form?
- Cloud droplets get head start by forming on a particle e.g. dust, soot or sea salt. These are cloud condemnation nuclei
- Cloud droplets grow - either by more water condense ms into each droplet or by several droplets coming together and coalescing
- Continues up to 9mm in diameter
- They fall as rain, snow or hail
Name the three types of cloud
Stratus
Cumulus
Cirrus
What is cloud seeding?
By changing the number of cloud condensation nuclei in the atmosphere, you can control how many cloud droplets there are
Adding nuclei to clean atmosphere could cause a cloud to form
Substances used in cloud seeding included silver iodide, frozen CO² and salt
They are dispersed from aircrafts or fired into atmosphere
What is air uplift?
Uplift occurs when hot air rises due to warm air expanding
As air expand it becomes less dense than cold air around it
Less dense hot air floats in denser cold air
Outline the Bergeron-Findeisen process
- Clouds at high altitude contain a mixture of water droplets and ice crystal
- Ice crystal grow rapidly at expense of water droplets due to rapid flux of water vapour from droplets to ice crystals
- Ice crystals fracture due to fast high altitude air currents. Hexagonal ice shapes develop with larger surface areas. More water vapour condenses around larger snowflakes accelerating growth
- Eventually snowflakes become too large and fall under gravity. As they warm they melt to produce rain
How has the Bergeron-Findeisen process proved and disproved?
Proved - Cloud seeding with dry ice can generate rainfall
Disproved - Cannot explain rainfall formation in warm tropics
Outline the collision process
- ‘Super sized’ condensation nuclei provide ‘seeds’ around which droplets form. They are far larger and heavier than normal droplets
- These ‘super sized’ droplets collide with smaller droplets sweeping them along into their wake
How has the collision process been proved?
Langmuir carried out experiments
He argued higher terminal velocity of large droplets allows them to absorb smaller droplets, causing rapid fusion and raindrop growth
What are the three key physical causes of excess runoff?
Prolonged rainfall
Snowmelt
Monsoon
How does prolonged rainfall affect surface runoff?
In the UK storms and intense rainfall are the most important contributors to excess runoff
Ground cannot hold anymore water and becomes saturated