One of the characteristics of global climate change is the increase in extreme climate events, e.g., droughts and floods. Forest adaptation strategies to extreme climate events are the key to predict ecosystem responses to global change. Severe floods alter the hydrological regime of an ecosystem which influences biochemical processes that control greenhouse gas fluxes. We conducted a flooding experiment in a mature grey alder (Alnus incana (L.) Moench) forest to understand flux dynamics in the soil-tree-atmosphere continuum related to ecosystem N 2 O and CH 4 turn-over. The gas exchange was determined at adjacent soil-tree-pairs: stem fluxes were measured in vertical profiles using manual static chambers and gas chromatography; soil fluxes were measured with automated chambers connected to a gas analyser. The tree stems and soil surface were net sources of N 2 O and CH 4 during the flooding. Contrary to N 2 O, the increase in CH 4 fluxes delayed in response to flooding. Stem N 2 O fluxes were lower although stem CH 4 emissions were significantly higher than from soil after the flooding. Stem fluxes decreased with stem height. Our flooding experiment indicated soil water and nitrogen content as the main controlling factors of stem and soil N 2 O fluxes. The stems contributed up to 88% of CH 4 emissions to the stem-soil continuum during the investigated period but soil N 2 O fluxes dominated (up to 16 times the stem fluxes) during all periods. Conclusively, stem fluxes of CH 4 and N 2 O are essential elements in forest carbon and nitrogen cycles and must be included in relevant models.Greenhouse gases (GHG), in particular, methane (CH 4 ) and nitrous oxide (N 2 O) contribute 16% and 6% to global warming, respectively 1 . In addition, N 2 O is a dangerous stratospheric O 3 layer depleting agent 2 . Due to the increasing emissions, both gases have high radiative forcing potential. In principle, terrestrial biosphere may be seen as a net source of GHG to the atmosphere 3 . Temperate as well as tropical forest soils (in general) seem to be a central natural emitting source of N 2 O, on the one hand, a natural sink of CH 4 on the other 4-9 . Flux estimations of N 2 O and CH 4 in forest systems are mainly based on studies of forest soil measurements, usually excluding exchange potential of vegetation 5,7,10 . Nevertheless, investigations on GHG fluxes from plants in wetland or riparian ecosystems show that plants, especially trees, can be essential sources of CH 4 and N 2 O 9,11-13 . However, recent studies uncover the relevance of tree stem surfaces playing an important role in understanding GHG dynamics in different forest ecosystems 8,9,14 .Grey alder (Alnus incana (L.) Moench)) is a fast-growing, pioneer tree species with excellent potential for short-rotation forestry in the Northern hemisphere [15][16][17][18] . Due to the symbiotic Frankia bacteria which fix atmospheric nitrogen, alder forests are important nitrogen sequestering ecosystems 19,20 . Decomposition of nutrient-rich alder litter improves soil properti...