Cloud Microphysics Flashcards
Supersaturation
the air contains more water vapour than is needed to cause saturation
Nucleation
describes initial formation of droplet or ice
Homogenous Nucleation
- droplets spontaneously form in pure air
- no particles present in the droplet formation
Heterogenous nucleation
- droplets form on particles (aerosols) called cloud condensation nuclei
Curvature (kelvin) effect
- greater probability that molecules from curved surface can escape from surface of liquid
- saturation over curved surface needs to be higher than over flat surfaces to keep drop in equilibrium
Solute
chemical that is being dissolved
Solvent
chemical that dissolves solute
Processes of precipitation drop growth
- Warm cloud processes (only liquid drops)
- cold cloud processes (ice and liquid drops)
Types of droplet collisions
collision-coalescence: large drops collect small drops
riming: falling ice collects liquid water and freezes
capture nucleation: Large drops capture small ice particles which results in the freezing of the drop
aggregation: falling snowflakes collect smaller snowflakes
Supercooled water
-liquid water with temp<0C
- homogenous nucleation: if water is pure then spontaneous freezing will occur at -40C
- heterogenous nucleation: water impurities cause freezing around ice nucleus to occur much higher than -40C
Bergeron Process