Fig. 7: The conceptual model of the QMT peatland development and carbon accumulation influenced by winter temperature and precipitation over the 1000 BP. | Communications Earth & Environment

Fig. 7: The conceptual model of the QMT peatland development and carbon accumulation influenced by winter temperature and precipitation over the 1000 BP.

From: A millennium of cold and humid climate decreased carbon accumulation in the subtropical monsoon peatland

Fig. 7: The conceptual model of the QMT peatland development and carbon accumulation influenced by winter temperature and precipitation over the 1000 BP.The alt text for this image may have been generated using AI.

The picture on the left shows the initial developmental stage, and the picture on the right shows the carbon accumulation stage. (+) indicates a positive effect impact and (−) indicates a negative effect impact. TOC is the total organic carbon. CAR is the carbon accumulation rate.

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