HIGHLIGHTS
SUMMARY
Carbon- climate feedbacks also lead to both increases and decreases in terrestrial carbon stocks: for example, warming at high latitudes leads to a more productive biosphere, but it also leads to increased plant and soil respiration (Kaushik et_al, 2020; Walker et_al, 2021; Canadell et_al, 2021; Crisp et_al, 2022). The release of nitrogen through anthropogenic energy and fertilizer use may drive increased carbon sequestration by the terrestrial biosphere (Schulte-Uebbing et_al, 2022; Y. Liu et_al, 2022; Lu et_al, 2021). Regional-scale carbon sequestration can differ substantially from the global mean and can be impacted by . . .
If you want to have access to all the content you need to log in!
Thanks :)
If you don't have an account, you can create one here.