Short-term Flooding Increases CH and NO Emissions from Trees in a Riparian Forest Soil-stem Continuum

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 NO and CH 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 NO and CH during the flooding. Contrary to NO, the increase in CH fluxes delayed in response to flooding. Stem NO fluxes were lower although stem CH 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 NO fluxes. The stems contributed up to 88% of CH emissions to the stem-soil continuum during the investigated period but soil NO fluxes dominated (up to 16 times the stem fluxes) during all periods. Conclusively, stem fluxes of CH and NO are essential elements in forest carbon and nitrogen cycles and must be included in relevant models.