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in pH levels between water strata are because of elevated CO2 from respiration and decomposition under the thermocline. Resulting from CO2’s influence on the pH of water, stratification could cause pH ranges to differ across a cline.Stratification is usually brought on by temperature variations inside a physique of water, where each layer of water does not mix with the layers above or under ³⁷. These layers are separated by clines, often called thermoclines (temperature divides) or chemoclines (chemistry gradients). Stratification can cause pH ranges inside a body of water to differ above and under the cline. The Alaska Water High quality

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