Condensation & Clouds: Understanding Water's Transformation

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SUMMARY

The discussion centers on the process of condensation, specifically the necessity of surfaces for liquid water formation. Participants clarify that while condensation typically requires cloud condensation nuclei (CCNs) or surfaces, water can condense without them if chilled below freezing. The conversation references key concepts such as nucleation and dew point, emphasizing that temperature plays a critical role in droplet formation. The importance of ambient conditions and particle presence in the atmosphere is also highlighted.

PREREQUISITES
  • Understanding of condensation and phase changes in water
  • Familiarity with cloud condensation nuclei (CCNs)
  • Knowledge of nucleation theory
  • Basic concepts of dew point and its significance in meteorology
NEXT STEPS
  • Research "Classical Nucleation Theory" for deeper insights into condensation mechanisms
  • Explore "Cloud Condensation Nuclei" and their role in weather phenomena
  • Study the "Dew Point" and its impact on humidity and condensation
  • Investigate the effects of atmospheric particles on condensation and precipitation
USEFUL FOR

Meteorologists, atmospheric scientists, and anyone interested in the physical processes of water transformation and weather patterns will benefit from this discussion.

EEristavi
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I understand that condensation occurs when water (in gas form) looses energy and becomes liquid. What I don't understand why some surface is needed to form a liquid water
 
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EEristavi said:
I understand that condensation occurs when water (in gas form) looses energy and becomes liquid. What I don't understand why some surface is needed to form a liquid water
Here is a wiki article on the phenomenon:
https://en.wikipedia.org/wiki/Cloud_condensation_nuclei
Water can condense without a surface - but the water must be chilled well below freezing before that will happen.

I am not sure if the exact mechanism for this is described, but I would point out that without a surface, most water particles that collide with each other will be at a temperature above the ambient - simply because of the speed of the collision. Then, both the heat of the collision and the latent heat of condensation would need to be somehow surrendered to the environment.
 
.Scott said:
Water can condense without a surface - but the water must be chilled well below freezing before that will happen.
What happens at the spout of a boiling kettle?
 
sophiecentaur said:
What happens at the spout of a boiling kettle?
Leave it to an Englishman to focus on a boiling kettle. :wink: I love those powerful electric tea kettles you have there.
 
anorlunda said:
I love those powerful electric tea kettles
The water needs to nearly boiling when it first comes into contact with the tea. Everywhere else in the World they pour luke warm water - or even dip the tea bag into a cup of water that was heated way back at the bar or in the kitchen. You've no idea, you guys. But you put whisky into ice, too!:smile:

.Scott said:
According to the wiki article,
I scanned through it but couldn't actually find that statement and I also looked at the other article. We all know that you can form fog and mist without the temperature being very low so they must be looking deeper and considering large droplet formation. It'll be the temperature that determines whether large enough drops can form to cause rain, probably because there will be an equilibrium when the evaporation rate is the same as the condensation rate.
 
EEristavi said:
I understand that condensation occurs when water (in gas form) looses energy and becomes liquid. What I don't understand why some surface is needed to form a liquid water

To understand, read about „Nucleation“: https://en.wikipedia.org/wiki/Classical_nucleation_theory
 
sophiecentaur said:
I scanned through it but couldn't actually find that statement and I also looked at the other article.
From the first paragraph of the wiki article:
In the atmosphere, this surface presents itself as tiny solid or liquid particles called CCNs. When no CCNs are present, water vapour can be supercooled at about −13°C (8°F) for 5–6 hours before droplets spontaneously form (this is the basis of the cloud chamber for detecting subatomic particles).
sophiecentaur said:
We all know that you can form fog and mist without the temperature being very low so they must be looking deeper and considering large droplet formation. It'll be the temperature that determines whether large enough drops can form to cause rain, probably because there will be an equilibrium when the evaporation rate is the same as the condensation rate.
At low altitudes and certainly indoors at a residence, there are always lots of airborne particles.
The second article I cited (the college Meteorology text) also notes that very humid conditions are unusual in polluted urban areas - because there are so many seeds available in the air.
 
.Scott said:
Water can condense without a surface - but the water must be chilled well below freezing before that will happen.

.Scott said:
From the first paragraph of the wiki article:

it doesn't say must be super cooled

In the atmosphere, this surface presents itself as tiny solid or liquid particles called CCNs. When no CCNs are present, water vapour can be supercooled at about −13°C (8°F) for 5–6 hours before droplets spontaneously form (this is the basis of the cloud chamber for detecting subatomic particles).

"can be cooled ... before" big differencethis is all related to dew point
https://en.wikipedia.org/wiki/Dew_point
 

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