Atmospheric Chemistry and Physics (May 2012)
The stable isotopic composition of molecular hydrogen in the tropopause region probed by the CARIBIC aircraft
Abstract
More than 450 air samples that were collected in the upper troposphere – lower stratosphere (UTLS) region by the CARIBIC aircraft (Civil Aircraft for the Regular Investigation of the atmosphere Based on an Instrument Container) have been analyzed for molecular hydrogen (H<sub>2</sub>) mixing ratios (χ(H<sub>2</sub>)) and H<sub>2</sub> isotopic composition (deuterium content, δ<sub>D</sub>). <br><br> More than 120 of the analyzed samples contained air from the lowermost stratosphere (LMS). These show that χ(H<sub>2</sub>) does not vary appreciably with O<sub>3</sub>-derived height above the thermal tropopause (TP), whereas δ<sub>D</sub> does increase with height. The isotope enrichment is caused by H<sub>2</sub> production and destruction processes that enrich the stratospheric H<sub>2</sub> reservoir in deuterium (D); the exact shapes of the profiles are mainly determined by mixing of stratospheric with tropospheric air. Tight negative correlations are found between δ<sub>D</sub> and the mixing ratios of methane (χ(CH<sub>4</sub>)) and nitrous oxide (χ(N<sub>2</sub>O)), as a result of the relatively long lifetimes of these three species. The correlations are described by δ<sub>D</sub>[‰]=−0.35 · χ(CH<sub>4</sub>)[ppb]+768 and δ<sub>D</sub>[‰]=−1.90· χ(N<sub>2</sub>O)[ppb]+745. These correlations are similar to previously published results and likely hold globally for the LMS. <br><br> Samples that were collected from the Indian subcontinent up to 40° N before, during and after the summer monsoon season show no significant seasonal change in χ(H<sub>2</sub>), but δ<sub>D</sub> is up to 12.3‰ lower in the July, August and September monsoon samples. This δ<sub>D</sub> decrease is correlated with the χ(CH<sub>4</sub>) increase in these samples. The significant correlation with χ(CH<sub>4</sub>) and the absence of a perceptible χ(H<sub>2</sub>) increase that accompanies the δ<sub>D</sub> decrease indicates that microbial production of very D-depleted H<sub>2</sub> in the wet season may contribute to this phenomenon. <br><br> Some of the samples have very high χ(H<sub>2</sub>) and very low δ<sub>D</sub> values, which indicates a pollution effect. Aircraft engine exhaust plumes are a suspected cause, since the effect mostly occurs in samples collected close to airports, but no similar signals are found in other chemical tracers to support this. The isotopic source signature of the H<sub>2</sub> pollution seems to be on the low end of the signature for fossil fuel burning.
