Stable isotope composition of water vapor in the atmospheric boundary layer above the forests of New England

Abstract

Water vapor at multiple levels was sampled from a light aircraft in the summertime atmospheric boundary layer (ABL) over forested terrain at altitudes up to 3 km. Three sampling flights were carried out under similar weather conditions during the summer to earlier fall period of 1996. The deuterium and oxygen 18 isotope ratios, δD and δ18O, of 24 water vapor and 30 surface water samples were analyzed on a mass spectrometer. The water vapor mixing ratio, Q, at each sampling level was estimated from the amount of the sample collected. The results show constant δD and δ18O in the mixed region of the ABL and sharply decreasing values near the top. Measurement of the ratio of the vertical atmospheric flux of HD16O or H218O to the flux of H216O is of particular interest in hydrology and paleoclimatology studies. This quantity, however, cannot be measured directly at the surface due to the instantaneous turbulent mixing of the evaporating water vapor with the overlying ABL. Using a δ − 1/Q mixing line method, we are able to determine such isotope flux ratios characterizing the two‐way exchange between the Earth's surface and the free atmosphere. The varying isotope flux ratios are lighter than expected, but fall into the ranges of the isotope ratios of the winter precipitation in the area. Based on the hypothesis of no fractionation between the soil water and the water vapor transpired by plants, our measurements suggest that late summer transpiration releases soil water which comes from the precipitation that fell during the previous winter. Other explanations are also discussed.