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Marine Plankton Play Far Greater Role in Cloud Formation

| | Source: MEDIA_INDONESIA Translated from Indonesian | Environment
Marine Plankton Play Far Greater Role in Cloud Formation
Image: MEDIA_INDONESIA

Recent research has revealed that microscopic organisms in the ocean have a far greater influence on the Earth’s atmosphere than previously thought. Marine plankton, tiny organisms floating on the ocean surface, play a crucial role in the process of cloud formation and global climate regulation.

Previously, the general understanding of cloud formation over the oceans centred on water vapour and sea salt carried into the atmosphere by wind. However, a team of scientists in this study discovered that organic compounds released by plankton act as primary seeds that accelerate the gathering of water droplets in the air to form clouds.

When plankton bloom in large numbers, they release gases and microscopic particles known as organic aerosols. These particles are then lifted into the atmosphere by wind and ocean wave ripples. Once aloft, the organic aerosols serve as highly effective cloud condensation nuclei, attracting surrounding water vapour until denser, brighter clouds are formed.

This phenomenon has a direct impact on the reflection of solar radiation. Clouds formed with the help of organic particles from plankton tend to be more reflective, bouncing more sunlight back into space. This natural process indirectly helps cool the Earth’s surface temperature in certain regions.

The discovery also provides a crucial missing piece in global climate simulation models. Many previous climate models often underestimated cloud cover over the oceans because they did not accurately account for this marine biological activity. By incorporating the contribution of plankton, scientists can now formulate more precise weather predictions and long-term climate change projections.

However, the researchers caution about the threat posed by global warming. Changes in ocean temperature and the phenomenon of ocean acidification could disrupt plankton ecosystems. If the population or productivity of these microscopic organisms declines, the ocean’s ability to support the formation of reflective clouds will also weaken, potentially accelerating the rate of global warming.

Through this study, the boundary between marine biology and atmospheric science is proven to be deeply interconnected. The existence of invisible organisms like plankton turns out to be one of the pillars supporting our planet’s natural cooling system.

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