METEO 300
Fundamentals of Atmospheric Science

5.7 Vapor Deposition

The growth of the cloud drop depends initially on vapor deposition, where water vapor diffuses to the cloud drop, sticks, and thus makes it grow. senv must be greater than sk for this to happen, but as the drop continues to grow, sk approaches 0 (i.e., eeq approaches es), so smaller amounts of supersaturation still allow the cloud drop to grow. Deriving the actual equation for growth is complex, but the physical concepts are straightforward.

  • The growth rate (dmd/dt) is proportional to senv – sk. Physically, this statement means that the greater the difference between the supersaturation in the environment and supersaturation at the particle’s surface, the faster water vapor will diffuse and stick on the surface. For instance, if senv equaled s, then the evaporation and condensation of water on the particle’s surface would be equal and there would be no mass growth.
  • As water vapor diffuses to the drop and forms water, energy is released (i.e., latent heat of condensation) and this raises the temperature of the cloud drop surface so that Tsfc > Tenv. But an outward energy flow occurs and is proportional to Tsfc -Tenv. Physically, this statement means that the particle and the air molecules around it are warmed by latent heat release. These warmer molecules lose some of this energy by colliding with the cooler molecules further away from the particle, and warm them by increasing their kinetic energy (see figure below).
Schematic of the two physical processes in the growth of a cloud drop by vapor deposition as described in the text above
Schematic of the two physical processes in the growth of a cloud drop by vapor deposition. One is vapor deposition and the other is the transfer of condensational heating to the atmosphere;
Credit: W. Brune (after Lamb and Verlinde)
  • When we account for both the flow of water molecules to the cloud drop surface and the flow of energy away from the surface, we can show that:

d m d dt =4π r d ρ l G( T,p )( s environment s k ) This equation is not rendering properly due to an incompatible browser. See Technical Requirements in the Orientation for a list of compatible browsers.

[5.14]
 
where G is a coefficient that is a function of T and p, ρL is the density of liquid water, and senvironment is the supersaturation of the environment while sk is the supersaturation of the particle. G incorporates the effects of the mass transport of water vapor molecules to the surface and the transport of heat generated on condensation away from the particle surface.
r d = C×time , where C is a constant
[5.15]
 
Growth of a cloud drop by vapor deposition as a function of time as described in the text below
Growth of a cloud drop by vapor deposition as a function of time. Dashed lines indicate drop size after the typical cloud lifetime.
Credit: W. Brune

Physical explanation:

  • The nucleated cloud drop radius increases fairly rapidly at the beginning, but within minutes slows down because of the square root dependence on time.
  • So, cloud drops can grow to 10-20 μm in 15 or so minutes, but then grow bigger much more slowly.
  • Since a typical cloud only lasts 10s of minutes, it is not possible for cloud drops to grow into rain drops by vapor deposition alone.
  • CCN nucleation followed by vapor deposition can make clouds, but it can’t make them rain.
  • We can develop a similar expression for vapor deposition on ice, but the vapor depositional growth on ice is a little faster than on liquid.

Conclusion:

We need other processes to get cloud drops big enough to form precipitation, either liquid or solid.