Mapping of Climate Change in the Bottom Waters of the Subarctic Atlantic during in situ Observations View Full Text


Ontology type: schema:ScholarlyArticle     


Article Info

DATE

2022-05

AUTHORS

A. K. Ambrosimov, A. A. Klyuvitkin

ABSTRACT

The results of continuous year-long in situ observations of the circulation of currents and temperatures in the bottom Arctic regions of the energy-active zone of the Iceland Basin are presented. Data were obtained at flooded buoy stations at a section of 59.5° N at depths of about 50 m from the bottom during 2016–2017. The intra-annual variability of bottom currents and temperature was investigated. It was shown that during the entire period there was monotonous stationary movement of water at all stations, as well as an increase in temperature in bottom waters entering the basin, as well as in those leaving. At the same time, the annual temperature growth rate of the outlet stream was 1.5 times higher than the temperature increase of the inlet stream. More... »

PAGES

315-320

Identifiers

URI

http://scigraph.springernature.com/pub.10.1134/s1028334x2205004x

DOI

http://dx.doi.org/10.1134/s1028334x2205004x

DIMENSIONS

https://app.dimensions.ai/details/publication/pub.1148660063


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