Ocean Acidification: The Other CO2 Problem

A detailed analysis of decreasing ocean pH, its effects on calcifying organisms, and the long-term prognosis for marine ecosystems.

Ocean Acidification: The Other CO2 Problem

The Chemistry of Acidification

Since the beginning of the Industrial Revolution, the pH of surface ocean waters has fallen by 0.1 pH units. Since the pH scale is logarithmic, this change represents approximately a 30 percent increase in acidity.

Surface pH Calculator

Data & Modeling

YearAtmospheric CO2 (ppm)Estimated Surface pHAragonite Saturation (Ω)
18502808.20~3.4
20204128.10~2.9
2100 (RCP 8.5)900+7.80<1.5

Common Misconceptions

A frequent error in media interpretation is confusing localized transient effects with global secular trends. The figures demonstrated here isolate the multi-decadal signal from seasonal noise.

Frequently Asked Questions

Is this reversible?

On human timescales, highly unlikely. The thermal inertia of the ocean means impacts will persist for centuries even if emissions cease immediately.

How accurate are these figures?

Based on the latest AR6 synthesis and prevailing primary literature. Uncertainties are inherent in coupled non-linear climate models.