A differential equation called the Aerosol General Dynamic Equation (GDE) characterizes the evolution of the number density of particles in an aerosol due to these processes. Aerosols are small particles in the air that can either cool or warm the climate, depending on the type and color of the particle. Aerosol particles, microscopic bits of dust, soot, and sea spray suspended in the air, are the most poorly understood component of Earth’s atmosphere. Aerosol, a system of liquid or solid particles uniformly distributed in a finely divided state through a gas, usually air . Aerosol particles, such as dust, play an important role in the precipitation process, providing the nuclei upon which condensation and freezing take place.

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