Fig. 4: The relationship between the temperature sensitivity of forest soil microbial CH4 oxidation and mean annual temperature across 84 forest sites.
From: Higher temperature sensitivity of forest soil methane oxidation in colder climates
The fitted solid line was estimated from a mixed-effects model, with the shaded region corresponding to the 95% confidence interval. The temperature sensitivity of forest soil microbial CH4 oxidation was quantified using the partial derivative of the soil microbial CH4 oxidation rate with respect to temperature (parameter a values, see “Methods”).
