Dec. 2020, Volume 2 Issue 4
Cover Illustration
Although the ever-increasing atmospheric CO
2 is considered as a key driver of modern global warming, the low heat capacity of atmosphere and strong convection processes in the troposphere both limit heat retention. Given the higher heat capacity and CO
2 concentration in soil compared to the atmosphere, the direct contributions of soil to the greenhouse effect may be significant. By experimentally manipulating CO
2 concentrations both in the soil and the atmosphere, Zhang et al. (pages 308316) demonstrated that the soil-retained heat and the slower soil heat transmission decrease the amount of heat energy leaking from the earth. Furthermore, the soil air temperature was affected by soil CO
2 concentration. This study indicates that soil and soil CO
2, together with atmospheric CO
2, play a crucial role in the greenhouse effect. The spatial and temporal heterogeneity of soils and soil CO
2 should be further investigated, given their potentially significant influence on global climate change.