Understanding Climate Part 2: Volcanoes, Oceans, and Internal Variability


Summary

This video explains how volcanic eruptions can temporarily cool the Earth's surface by releasing dust and sulfur dioxide gas, balancing out the warming effects of greenhouse gases. Despite significant events like the Mount Pinatubo eruption in 1991, human activities produce more emissions overall. Ocean currents, driven by factors like temperature and salinity differences, play a crucial role in redistributing heat energy globally, impacting climate and ocean ecosystems. The ocean acts as a carbon sink, removing carbon dioxide from the atmosphere through deep water formation, regulating climate. Feedback cycles like La Niña and El Niño influence global temperatures and weather patterns, affecting food production and ocean ecosystems.


Volcanic Impact on Climate

Volcanic eruptions release dust, ash, and sulfur dioxide gas that can block sunlight and cool the Earth's surface, outweighing the warming effect of greenhouse gases. Mount Pinatubo eruption in 1991 was significant but volcanic emissions are minor compared to human activities.

Ocean Currents and Circulation

Ocean currents operate horizontally and vertically on local and global scales, driven by temperature, salinity, and density differences. The global-scale circulation system redistributes heat energy, affecting climate and ocean ecosystems. Warm ocean waters holding less carbon dioxide lead to global impacts.

Carbon Dioxide Balance in Ocean

The ocean removes carbon dioxide from the atmosphere through deep water formation and sequesters it, acting as a buffer to regulate climate. Positive feedback cycles like La Niña and El Niño influence global temperatures and ocean ecosystems, impacting food production and weather patterns.

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