An estimation of the ¹⁸O / ¹⁶O ratio of UT/LMS ozone based on artefact CO in air sampled during CARIBIC flights

Three assumptions were made for discussing the 90 Sr dis- tribution in the waters off Japan in May–June 2011: (i) the Sr peak in direct oceanic release into the Pacific Ocean took

This may be a consequence of the very high sea-ice di ff usivities (SID) that have been allowed in the ensemble leading to increased brine rejection and AABW production. + 0.83 in

Thus, a new mixing line (HH2-E mixing line) was re-calculated between the sampling location after the floodgate and estuarine water (Fig.. However, the DIN and isotopic trends did

1, at high-altitude, such as those covered by Interball-2 and Cluster, because of the finite lat- itudinal extent of the heating region, the conjugate action of ion heating

Comparison of a CH 4 peak of an air sample with the signals gained from an injection of pure Kr measured with the Bern system at CO 2 tuning conditions (a) Beam intensities in mV

The rate constants determined over the 227 K–400 K range show very low scatter and are significantly greater, by 20% at room temperature and by 15% at 227 K, than the

The use of wavelet analysis allows the identification of the various scales controlling the influence of the meteorological variables on 222 Rn dispersion in the surface layer that

specimens from Antarctica from the mollusk dataset does yield a steeper slope (Table 4) of 0.0402 ± 0.0050 (1 s.e.) on the absolute reference frame, however it does not change