Precipitation development; Warm and Cold clouds >0 ° C
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Transcript of Precipitation development; Warm and Cold clouds >0 ° C
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Precipitation development;Warm and Cold clouds
>0°C <0°C
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Last lectures from me…
• Cloud droplet formation (micro-scales)
• Cloud/fog formation processes (macro-scales)
• This lecture – return to the micro-scales
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Cloud droplets and Raindrop sizes
How do droplets grow and become raindrops?
r = radius in m
n = numberconcentrationper litre
v = terminalfall speedin cm/s
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Why doesn’t it always rain when there are clouds?
A: Updrafts can keep small cloud droplets suspended
Radius(m)
Terminal Velocity(cm s-1)
Type of Particle
0.1 0.0001 Condensation (Aitken) nuclei
10 1 Typical cloud droplet
100 70 Large cloud droplet
1000 = 1 mm 650 Typical raindrop
2500 = 2½ mm 900 Large raindrop
Need stronger updraughts to support larger drops…
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What do rain drops look like?
equivalent diameter (mm) of rain drop
Drops break up for larger sizes;Max. size ~8-10 mm
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How do cloud droplets (radius = 10 m) turn into rain drops (1 mm) ?
There are 2 main processes:1. In ‘warm’ clouds with cloud top T > -15 °C2. In ‘cold’ clouds with cloud top T <-15 °C
Initial growth by condensation, but this is limited by diffusion…
They never get a chance to grow into raindrops by condensation alone – this process would take D A Y S . . .
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Raindrop formation by collision and coalescencein warm clouds
It takes about 106 small cloud droplets (10 m) to form onelarge raindrop (1000 m)
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Stochastic model of collisions and droplet growth
‘Statistical’
Start with 100 drops
In 1 timestep, 10% grow
Next step, repeat…
End up with a logarithmic size distribution…
Actually, more complicated…
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Cascade process
Raindrops reaching Earth’s surface rarely exceed 5 mm (5000 m). Collisions or glancing blows between large raindrops break them into smaller drops.
Also surface tension is too weak to hold the larger drops together
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Distribution of raindrop sizes – raindrop spectra
the Marshall-Palmer distribution
1 2 3 4 5 6Drop diameter, D (mm)
1000
3000
2000
4000
5000
6000
1 2 3 4 5 6Drop diameter, D (mm)
1
100
10
1000
10000
differentrain rates
n(D) = noe-ΛD
No.
of
drop
s in
eac
h cl
ass
size
per
m3
no = 8 x 103 ; Λ= 4.1 Rh-0.21 where Rh is the rainfall rate (mm h-1)
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Depth of cloud influences type of rain
Stratus – thin cloud (<500 m) and has a slow upwardmovement (< 0.1 ms-1).
Growth by coalescence wouldn’t produce a dropletmore than about 200 m.
If RH below the cloud is high, then the droplets will arrive at the ground as drizzle, defined as diameter of drop < 500 m (0.5mm).
Thicker clouds, formed by convective motion, can have stronger updrafts and can keep larger cloud droplets aloft, permitting them to join (coalesce) with more droplets and grow to greater sizes.
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1 Low – Nimbostratus (Ns)
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3 Cumulonimbus (Cb)
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Supplementary feature: virga
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Cold clouds (temperate latitudes and polewards).
Does water always freeze at 0 °C ?
It depends … on its volume and the presence of ice nuclei.
Ice in your freezer in an ice tray – it’ll freeze at 0 °C.but a 1000 m (1mm) drop will not freeze until T ≈ -11 °C.
For ice to form all the water molecules must align in the proper crystal structure – in a large volume there is a high chance a few of the molecules will line up in the proper manner whereas in a small volume of water the chances are reduced, simply because there are fewer molecules
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Ice nuclei
Ice or freezing nuclei aid the freezing processc.f aitken nuclei (<0.2 m) for condensation nuclei.1 cm3 of pure water in a test tube wouldn’t freeze until T was about -3 to – 5 °C.
all-42
1 in 102-35
1 in 104-30
1 in 105-20
1 in 106-10
none0
Proportionfrozen
T (°C)Proportion ofcloud droplets frozen
at different temperatures
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Ice nuclei
- are less common than Aitken nuclei
- most effective ones have the same crystal shape as ice crystals hence ice can form around and on them easily.
- kaolonite (clay) minerals are effective ice nuclei
- are most effective at about -10 °C
- because of the relative sparseness of ice nuclei, ice crystals and supercooled water can coexist at the same time.
- this last point is crucial in the formation of precipitation in cold clouds as it gives rise to the Bergeron process.
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vapour
pre
ssure
temperature
0 °Cice
Super-cooledwater
Bergeron process arisessince svpice<svpwater
so ice grows at the expense of supercooled water droplets
If you look at the area in-between the two SVP curves you’ll see that an air parcel here would be unsaturated with respect to water but supersaturated with respect to ice. That means net evaporation will take place from the water but net condensation to the ice.
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One of the reasonsyou have to defrostyour freezer regularly…
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Bergeron
process
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Lab ice crystal growing from super-cooled water drops
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Why are snowflakes hexagonal? …it’s complicated!
Angle ~104° +
+
-
Sheets of molecules – viewed from above
http://www.uwgb.edu/dutchs/PETROLGY/Ice%20Structure.HTM
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Shape of H2O molecule and H-bonding gives rise to hexagonal crystals
Melting and re-freezing gives rise to vast variety of snow flakes
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Clouds can be a mixture of water droplets and ice
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Summary
• Cloud particle size limited to a few mm by fall velocity
• Droplets (μm) grow to raindrops (mm) by two main routes:– Warm clouds: condensation, collision, coalescence
(then break-up)– Cold clouds: super-cooled water freezes on ice nuclei
– producing larger ice particles – often melt en route to surface
• Precipitation can evaporate en route
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0000 Fri 06 Nov
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1200 Friday
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0000 Saturday
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1200 Saturday
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0000 Sunday
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1200 Sunday
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0000 Monday