Nitrous oxide fluxes were measured at the Lägeren CarboEurope IP flux site over the multi-species mixed forest dominated by European beech and Norway spruce. Measurements were carried out during a four-week period in October?November 2005 during leaf senescence. Fluxes were measured with a standard ultrasonic anemometer in combination with a quantum cascade laser absorption spectrometer that measured N₂O, CO₂, and H₂O mixing ratios simultaneously at 5 Hz time resolution. To distinguish insignificant fluxes from significant ones it is proposed to use a new approach based on the significance of the correlation coefficient between vertical wind speed and mixing ratio fluctuations. This procedure eliminated roughly 56% of our half-hourly fluxes. Based on the remaining, quality checked N₂O fluxes we quantified the mean efflux at 0.8 ± 0.4 ?mol m^?2 h^?1 (mean ± standard error). Most of the contribution to the N₂O flux occurred during a 6.5-h period starting 4.5 h before each precipitation event. No relation with precipitation amount could be found. Visibility data representing fog density and duration at the site indicate that wetting of the canopy may have as strong an effect on N₂O effluxes as does below-ground microbial activity. It is speculated that above-ground N₂O production from the senescing leaves at high moisture (fog, drizzle, onset of precipitation event) may be responsible for part of the measured flux. In comparison with the annual CO₂ budget of ?342 g C m^?2 yr^?1 it is estimated that concurrent N₂O fluxes offset at least 5% of the greenhouse forcing reduction via net CO₂ uptake.