Abstract
Streams and rivers emit substantial amounts of nitrous oxide (N(2)O) and are therefore an essential component of global nitrogen (N) cycle. Permafrost soils store a large reservoir of dormant N that, upon thawing, can enter fluvial networks and partly degrade to N(2)O, yet the role of waterborne release of N(2)O in permafrost regions is unclear. Here we report N(2)O concentrations and fluxes during different seasons between 2016 and 2018 in four watersheds on the East Qinghai-Tibet Plateau. Thawing permafrost soils are known to emit N(2)O at a high rate, but permafrost rivers draining the East Qinghai-Tibet Plateau behave as unexpectedly minor sources of atmospheric N(2)O. Such low N(2)O fluxes are associated with low riverine dissolved inorganic N (DIN) after terrestrial plant uptake, unfavorable conditions for N(2)O generation via denitrification, and low N(2)O yield due to a small ratio of nitrite reductase: nitrous oxide reductase in these rivers. We estimate fluvial N(2)O emissions of 0.432 - 0.463 Gg N(2)O-N yr(-1) from permafrost landscapes on the entire Qinghai-Tibet Plateau, which is marginal (~0.15%) given their areal contribution to global streams and rivers (0.7%). However, we suggest that these permafrost-affected rivers can shift from minor sources to strong emitters in the warmer future, likely giving rise to the permafrost non-carbon feedback that intensifies warming.