Water Cycle Pack D Flashcards

1
Q

What causes clouds?

A
  • Air rises and cools to saturation points (when the air can hold no more moisture)
  • There is a fall in pressure as altitude increases, so air expands
  • There are fewer collisions between air molecules, so the amount of heat energy falls and therefore temperature falls
  • Clouds form as water vapour condenses into water droplets
  • Dew point must be reached for condensation to occur
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2
Q

What causes rain in general?

A
  • Cloud droplets have to grow or fuse with
  • There are two theories about this
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3
Q

What is the Bergeron-Findeisen theory of rain droplet formation?

A
  • Clouds at high altitudes contain a mix of very cold water droplets and ice crystals (as temperature is just below 0)
  • The ice crystals grow rapidly because every water droplet that comes into contact freezes and adds to the crystal
  • They eventually become too large and dense to be held up and fall to the ground due to gravity
  • If the air between the clouds and ground is <2°C, snowflakes remain as snow
  • If the air temperature is warmer, they turn into raindrops as they fall
  • We can generate rainfall by adding dry-ice to the top of clouds, so this supports the theory
  • Theory does not explain the generation of rainfall in the Tropics, where temperatures are too high
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4
Q

What is the collision theory of rain droplet formation?

A
  • Super sized condensation nuclei (e.g. salt particles) provide ‘seeds’ around which water can condense
  • Much larger and heavier than normal droplets
  • Large droplets fall and collide with smaller droplets, absorbing them
  • Super-droplets move faster than others as they are larger, enabling them to overtake and absorb them
  • Theory can explain how rainfall forms in the Tropics, unexpected downpours and flash floods
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5
Q

What causes orographic rain?

A
  • Air is forced to rise over a barrier
  • it cools and condensation occurs
  • Rain forms
  • The leeward slope receives relatively little rainfall (the rain shadow effect)
  • Augmented by the feeder-seeder mechanism
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6
Q

What is the seeder-feeder effect?

A
  • The fallout of precipitation from a seeder cloud into a lower-level cloud generated by relief
  • Can result in the growth of ice crystals or rain that originated in the seeder cloud as they fall through the feeder cloud
  • Leads to precipitation enhancement over the mountains
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7
Q

Where in the UK does orographic rainfall occur?

A
  • North and western UK
  • West cost of Scotland
  • Cumbrian coastline
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8
Q

What two cells from the tricellular model is the UK between?

A
  • Polar cell bringing cold air
  • Ferrel cell bringing warm air
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9
Q

What causes frontal rain?

A
  • Warm air is lighter and less dense
  • It is forced to rise over cold, denser air
  • As it rises, the air cools and its ability to hold water vapour decreases
  • Condensation occurs which forms clouds and rain
  • Forms where two surface air streams meet
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10
Q

Where in the UK does frontal rain occur?

A

All over the UK

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11
Q

What causes convectional rain?

A
  • When the land becomes hot, the air above it rises as it becomes warmer and expands
  • As it rises, it cools and condensation occurs so its ability to hold water vapour decreases
  • Further ascent causes more cooling
  • Cool air descends and replaces warm air
  • Results from intense daytime heating of the land
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12
Q

When and where is there convectional rain in the UK?

A
  • Southern UK
  • In summer
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