Warming homogenizes apparent temperature sensitivity of ecosystem respiration.

Warming-induced carbon loss through terrestrial ecosystem respiration () is likely getting stronger in high latitudes and cold regions because of the more rapid warming and higher temperature sensitivity of ( ). However, it is not known whether the spatial relationship between and temperature also holds temporally under a future warmer climate. Here, we analyzed apparent values derived from multiyear observations at 74 FLUXNET sites spanning diverse climates and biomes. We found warming-induced decline in is stronger at colder regions than other locations, which is consistent with a meta-analysis of 54 field warming experiments across the globe. We predict future warming will shrink the global variability of values to an average of 1.44 across the globe under a high emission trajectory (RCP 8.5) by the end of the century. Therefore, warming-induced carbon loss may be less than previously assumed because of homogenization in a warming world.