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. 2024 Jun 7;10(23):eadl2201. doi: 10.1126/sciadv.adl2201

Fig. 7. The warm temperature anomalies caused the increase in ecosystem respiration over East Asia, outpacing the GPP increase.

Fig. 7.

(A) Regional mask for East Asia (gray). (B) Percentage precipitation anomalies between May and July, 2021 (unit: %) relative to the mean over 2015–2021. (C) Temperature anomalies between May and July. (D) Percentage change of GPP anomalies between May and July (unit: %). (E) NBE anomalies during May to July [unit: tera grams of carbon (TgC)]. (F) Monthly anomalies of NBE, GPP, and TER over the region (unit: GtC/month). (G) Annual anomalies of NBE, GPP, and TER (unit: GtC/year).