Potential decline in carbon carrying capacity under projected climate-wildfire interactions in the Sierra Nevada.

Despite the increasing temperature and moisture stress early in our simulations, our results, similar to other studies 19 , showed a trend of continued C uptake and increasing TEC into the 22 nd century (Fig. 2 ).

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Relative to baseline, increasing temperature under projected climate resulted in an increasing trend of upslope movement in snowline elevation (threshold elevation below which mean monthly temperature ≥0 °C for all year) over the century (Fig. 3 ), decreasing the area maintaining snow cover by 20–84% across transects under mean projected late-century (2090–2100) climate.

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