Increased temperatures lead to higher CO2 levels primarily by reducing the solubility of CO2 in seawater, as explained by Henry's Law. As ocean temperatures rise, not only does CO2 escape more readily into the atmosphere, but there is also a significant concern regarding the release of methane from arctic underwater reserves. Methane is a much more potent greenhouse gas than CO2, creating a positive feedback loop: higher atmospheric temperatures warm the oceans, releasing more dissolved methane, which further increases atmospheric temperatures. This cycle poses a risk of reaching a tipping point that could result in exponential growth of greenhouse gases. Additionally, rising seawater temperatures lower pH levels, causing dissolved carbon compounds to shift back to CO2, further contributing to atmospheric CO2 levels. Environmentalists and geoscientists are actively seeking solutions to mitigate this reinforcing cycle.