(H2O)-O-16 and HDO measurements with IASI/MetOp

In this paper we analyze distributions of water vapour isotopologues in the troposphere using infrared spectra recorded by the Infrared Atmospheric Sounding Interferometer (IASI), which operates onboard the Metop satellite in nadir geometry. The simultaneous uncorrelated retrievals of (H2O)-O-16 and HDO are performed on radiance measurements using a line-by-line radiative transfer model and an inversion procedure based on the Optimal Estimation Method (OEM). The characterizations of the retrieved products in terms of vertical sensitivity and error budgets show that IASI measurements contain up to 6 independent pieces of information on the vertical distribution of (H2O)-O-16 and up to 3.5 for HDO from the surface up to the upper troposphere (0-20 km). Although the purpose of the paper is not validation, a restricted comparison with sonde measurements shows that the retrieved (H2O)-O-16 profiles capture the seasonal/latitudinal variations of the water content, with good accuracy in the lowest layer but with larger uncertainties higher in the free and upper troposphere. Our results then demonstrate the ability of the IASI instrument to monitor atmospheric isotopologic water vapour distributions and to provide information on the partitioning of HDO as compared to (H2O)-O-16. The derivation of the delta(D) is challenging and associated with large errors in the uncorrelated retrieval approach chosen here. As a result averaging on the vertical to produce a column-averaged delta(D) is required to produce meaningful results for geophysical interpretation. As a case study, we analyse concentration distributions and spatio-temporal variations of (H2O)-O-16 and delta(D) during the October 2007 Krosa super-typhoon over South-East Asia. We show that individual delta(D) have uncertainties of 37 parts per thousand for the vertically averaged values. Using the latter, we suggest that the typhoon produces a so-called amount-effect, where the delta(D) is negatively correlated to the water amounts as a result of intense depletion of the deuterated species.