Abstract
The results of a study of the water mass structure in a poorly studied area of the eastern basin of the Tropical Atlantic (Kane Gap) according to data from the 63rd cruise of P/V “Akademik Ioffe” in 2022 are presented in the paper. Variability of the average monthly characteristics of these waters using the GLORYS12v1 reanalysis for 1993–2022 is shown. Intermediate waters in the section are represented by a mixture of Antarctic intermediate water (AAIW) and Mediterranean water (the share of the latter reaches 34%). It has been established that the North Atlantic Deep Water (NADW) is represented by two layers: the Upper NADW with a maximum of salinity and the Middle NADW with a maximum of oxygen. The bottom water layer contains a mixture of Antarctic Bottom Water (AABW), the Lower and Middle components of the NADW. This mixture, coming primarily from the Vema Fracture zone region, is properly to call Northeast Atlantic Bottom Water (NEABW). Its upper limit corresponded to the isotherm of 1.95°С and the Si/P ratio equal to 33. In this work, using the conservative PO, the proportion of AABW in NEABW, which is about 20%, was calculated. According to the GLORYS12v1 on a seasonal scale in the bottom layer, a significant negative relationship was established between the variability of potential temperature and the meridional speed of currents. Significant trend for an increase in the average annual potential temperature (by 0.06 °C) and a decrease in salinity (by 0.005 psu) in general for the period 1993–2022 was revealed.