Extended Data Fig. 7: Warming effects on cumulative amount of nitrogen losses during the initial 8 years of experiment based on the DeNitrification–DeComposition model.
From: Progressive decline in soil nitrogen stocks with warming in a Tibetan permafrost ecosystem

The green, purple and red areas indicate the primary pathways of N losses included plant N uptake, N leaching and gaseous N emissions from 2014 to 2021. The gaseous N refers to N2O, N2, nitric oxide and ammonia in the DNDC model.