Spatial and temporal variations in global soil respiration and their relationships with climate and land cover.

At the global scale, 50% of our study area experienced an increasing trend in R s , and the regions with a significant increasing trend (8.5%) were spatially aggregated and mainly located at the high latitudes (e.g., northern Canada, northern Russia, and northern Europe), northern Mongolia, Loess Plateau and northeastern Tibetan Plateau of China, India, Amazon Basin, and Congo Basin ( Fig. 2, B and C ).

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However, central Quebec, Canada also experienced widespread SV loss and TC gain, but R s in this area showed a decreasing trend ( Fig. 2B and fig.

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