Behind the changing climate, little-known small particles - cloud condensation nuclei (CCN) - are quietly affecting our weather and climate. These tiny particles, with a diameter of about 0.2 μm, are equivalent to one hundredth the size of cloud droplets and silently participate in the cloud formation and precipitation process. Cloud condensation nuclei are a unique type of aerosol in the atmosphere that provide the necessary non-gaseous surface for the condensation of water vapor. This article will delve into the huge impact these small particles have on weather, climate, and the future of climate engineering.
Water vapor needs to attach to a non-gaseous surface to turn into liquid, a process called condensation.
Cloud condensation nuclei are usually composed of dust, sea salt, sulfate and other substances. Their size and composition will greatly affect their ability to form cloud droplets. For example, sulfates and sea salt readily absorb water, whereas soda, carbon, and other minerals do not. The number of these particles in the atmosphere is typically between 100 and 1,000 per cubic centimeter, with an estimated total mass of up to 2 trillion kilograms per year.
The number and type of cloud condensation nuclei directly affect precipitation, cloud lifespan and optical properties. Studies have shown that the stable concentration of CCN is affected by aggregation and merging, and changes in its number may also be affected by solar changes, thereby indirectly changing the characteristics of the clouds. Therefore, understanding cloud condensation nuclei may not only help improve precipitation forecasts, but also provide key information for responding to climate change.
The number and type of cloud condensation nuclei directly affect precipitation, cloud lifespan and optical properties.
Cloud seeding is a technique that adds small particles to the atmosphere to promote cloud formation and precipitation. Many researchers have explored different approaches, including aerial or ground spraying of salt and even using laser pulses to excite molecules in the atmosphere. Although these methods are sometimes effective in increasing precipitation, many studies have failed to find significant differences in precipitation.
Another CCN-related technology is marine cloud brightening, a method of climate engineering that injects tiny particles into clouds to enhance their ability to reflect sunlight. While this technology is intended to reduce temperatures on the Earth's surface, it could face many challenges in implementation, including the effects of compounds such as chlorine and bromine on other molecules in the atmosphere.
Techniques such as cloud seeding and marine cloud brightening, while challenging to implement, reveal the options we have in the face of climate change.
The growth of marine phytoplankton has an important influence on the formation of cloud condensation nuclei. Certain phytoplankton release dimethyl sulfide (DMS), a substance that can form sulfate aerosols. When phytoplankton flourish in warm waters, they release large amounts of DMS, which in turn leads to an increase in CCN, which further promotes cloud formation and creates a disruptive climate regulation loop.
Gases and ash released during volcanic eruptions can also significantly affect CCN concentrations in the atmosphere. Gases such as sulfur dioxide released by volcanoes can be converted into sulfuric acid, which in turn forms fine sulfate aerosols that increase the probability of cloud formation. These aerosols can also reflect solar radiation, leading to global cooling.
With the continuous advancement of science and technology, research on cloud condensation nuclei is still ongoing. Their presence not only affects weather systems, but also plays a key role in broader contexts such as climate change. However, there is still much unknown to explore for future research on cloud condensation nuclei, the protective mechanisms of their stability, and their possible applications in climate regulation. Have you ever thought that one day in the future, cloud condensation nuclei might actually become an important tool in our fight against climate change?