Types of Precipitation Flashcards

1
Q

What are the diff. types of pptn?

A
  • clouds
  • rain
  • hail
  • snow
  • dew
  • fog
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2
Q

How do clouds form?

A
  • air rises + cools [adiabatic cooling] - humidity
  • humidity inc to 100% + saturation occurs
  • air warmer than surrounding air continues to rise, creating tall (thunder) clouds: unstable
  • formed of Ms of tiny water droplets held in suspension
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3
Q

What are the diff types of clouds?

A
  • cirrus: wispy + high
    • mostly consists of ice crystals
    • inc. cirrocumulus + cirrostratus
  • alto: middle-height
    • consists of water drops + exists at T°C < 0°C
  • stratus: layered
    • dense, grey + low lying
    • inc. stratocumulus
  • nimbus: rain (water bearing)
    • inc nimbostratus
  • cumulus: heaped + flat-bottomed
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4
Q

What is rain?

A
  • liquid water droplets heavy enough to fall to ground
    • between 0.5-5mm
  • drizzle: rainfall < 0.5mm
  • varies in amount, intensity + duration
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5
Q

What is hail?

A
  • concentric rings of clear + opaque ice
  • raindrops freeze inside a cumulonimbus cloud
  • hailstones then collide w supercooled water, freezing on impact
  • rising + falling in cloud causes repeated melting + freezing until hailstone heavy enough to fall
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6
Q

What is snow?

A
  • frozen pptn
  • forms when T°C is below freezing + water vapour turns solid
  • heaviest snowfall: when warm moist air is forced to rise in orthographic or frontal rainfall, as v. cold air contains limited moisture
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7
Q

What is dew?

A
  • direct deposition of water on a surface
  • occurs in anticyclonic systems w rapid radiation cooling at night
  • T°C reaches dew point, + condensation/direct ground/veg. pptn occurs
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8
Q

What is fog?

A
  • cloud at ground lvl + results from radiation cooling
  • common over sea in autumn + spring bc contrast in T°C between land + sea is sig.
  • steam fog: localised when cold air blows over warmer water + air becomes saturated due to evaporation, resulting condensation causes steam
  • advection fog:
  • formed when winds move towards pole over cold sea, so chilled below due point
  • forms over cold ocean current, the wind blows over
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