Chapter 5: Cloud development and precipitation - PowerPoint PPT Presentation

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Chapter 5: Cloud development and precipitation

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Chapter 5: Cloud development and precipitation Atmospheric Stability Determining stability Cloud development and stability Precipitation processes – PowerPoint PPT presentation

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Title: Chapter 5: Cloud development and precipitation


1
Chapter 5 Cloud development and precipitation
  • Atmospheric Stability
  • Determining stability
  • Cloud development and stability
  • Precipitation processes
  • Precipitation types
  • Measuring precipitation

2
Atmospheric stability
3
Atmospheric stability
  • stable and unstable equilibria
  • air parcels
  • adiabatic process
  • adiabatic lapse rates
  • Stability does not control whether air will rise
    or sink.Rather, it controls whether rising air
    will continue to riseor whether sinking air will
    continue to sink

4
Determining stability
5
A stable atmosphere
  • environmental lapse rate
  • absolute stability
  • stabilizing processes
  • subsidence inversions
  • stable air provides excellent conditions for
    high pollutionlevels

6
An unstable atmosphere
  • absolute instability
  • warming of surface air
  • destabilizing processes
  • superadiabatic lapse rates
  • unstable air tends to be well-mixed

7
Conditionally unstable air
  • conditional instability
  • dry and moist adiabatic lapse rates

8
Cloud development and stability
9
Cloud development and stability
  • surface heating and free convection
  • uplift along topography
  • widespread ascent
  • lifting along weather fronts

10
Convection and clouds
  • thermals
  • fair weather cumulus
  • fair weather cumulus provide a visual marker of
    thermals
  • bases of fair-weather cumulus clouds marks the
    lifting condensation level, the level at which
    rising airfirst becomes saturated

11
Topography and clouds
  • orographic uplift
  • rain shadow
  • The rain shadow works for snow too. Due to
    frequentwesterly winds, the western slope of the
    Rocky Mountainsreceives much more precipitation
    than the eastern slope.

12
Precipitation processes
13
Collision and coalescence process
  • terminal velocity
  • coalescence
  • warm clouds
  • A typical cloud droplet falls at a rate of 1
    centimeter per second.At this rate it would take
    46 hours to fall one mile.

14
Ice crystal process
  • cold clouds
  • supercooled water droplets
  • saturation vapor pressures over liquid water and
    ice
  • accretion
  • The upper portions of summer thunderstorms are
    cold clouds!

15
Cloud seeding and precipitation
  • cloud seeding
  • silver iodide
  • It is very difficult to determine whether a
    cloud seedingattempt is successful. How would
    you know whetherthe cloud would have resulted in
    precipitation if it hadntbeen seeded?

16
Precipitation in clouds
  • accretion
  • ice crystal process

17
Precipitation types
18
Rain
  • rain
  • drizzle
  • virga
  • shower
  • Virga is much more commonly observed in the
    westernUS, because the humid climate of the
    eastern US reduces the visibility.

19
Snow
  • snow
  • fallstreaks
  • dendrite
  • blizzard
  • Snowflake shape depends on both temperature
    andrelative humidity

20
Sleet and freezing rain
  • sleet
  • freezing rain
  • rime
  • Sleet makes a tap tap sound when falling on
    glass

21
Snow grains and snow pellets
  • snow grains
  • snow pellets
  • graupel

22
Hail
  • updraft cycles
  • accretion
  • a hailstone can be sliced open to reveal
    accretion rings,one for each updraft cycle

23
Measuring precipitation
24
Instruments
  • standard rain gauge
  • tipping bucket rain gauge
  • It is difficult to capture rain in a bucket when
    thewind is blowing strongly

25
Doppler radar and precipitation
  • radar
  • Doppler radar
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