Atmospheric Aerosol Loading

Atmospheric aerosol loading refers to the amount of tiny particles, called aerosols, suspended in the air. These particles originate from natural sources like dust, pollen, and sea spray, as well as human activities such as pollution and burning fossil fuels. Aerosols influence climate by reflecting sunlight and affecting cloud formation, and they can impact air quality and health. Higher aerosol loading means more particles in the atmosphere, which can lead to changes in weather patterns, temperature, and visibility. Monitoring aerosol levels helps scientists understand environmental changes and develop strategies to protect both climate and public health.