Fig. 6: Comparison of NCB in the QMT peatlands of the subtropic monsoon and paleoclimate indicator records over the past 1000 years. | Communications Earth & Environment

Fig. 6: Comparison of NCB in the QMT peatlands of the subtropic monsoon and paleoclimate indicator records over the past 1000 years.

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

Fig. 6

a 30°N solar irradiance33. b North hemisphere annual temperature anomaly35. c Central East China annual temperature anomaly26. d Winter annual temperature anomaly of east China49. e Summer annual temperature anomaly of east China36. f The dark blue line is the composite z-score of the data for different humidity indicators in eastern China, and the sky-blue shading is the margin of error. g this study, the NCB is average for the core QMT22-1 and QMT22-2, short-term error bars.

Back to article page