Large live biomass carbon losses from droughts in the northern temperate ecosystems during 2016-2022.

However, we found a reversal of this trend from 2016 to 2022, with total live biomass carbon clearly shifting from an increasing trend to a decreasing trend from around 2016.

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Notably, the live biomass carbon changes revealed by L-VOD showed a decreasing trend around 60°N – 65°N during 2016-2022, which coincided with the highest average annual burned area recorded in this region over the same period (Fig. 4h ).

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We find that live biomass carbon stocks have undergone a reversal from a positive to a negative trend during the study period with 2016 marking the turning point.

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