title: Localization of areas of deep convection in the Nordic seas, the Labrador Sea and the Irminger Sea
metadata.name: dc.contributor.author
metadata.value: Fedorov, Aleksandr M.
metadata.lang: -
metadata.name: dc.contributor.author
metadata.value: Bashmachnikov, Igor L.
metadata.lang: -
metadata.name: dc.contributor.author
metadata.value: Belonenko, Tatyana V.
metadata.lang: -
metadata.name: dc.date.accessioned
metadata.value: 2018-10-23T15:27:42Z
metadata.lang: -
metadata.name: dc.date.available
metadata.value: 2018-10-23T15:27:42Z
metadata.lang: -
metadata.name: dc.date.issued
metadata.value: 2018-09
metadata.lang: -
metadata.name: dc.identifier.citation
metadata.value: Fedorov A. M., Bashmachnikov I. L., Belonenko T. V. Localization of areas of deep convection in the Nordic seas, the Labrador Sea and the Irminger Sea. Vestnik of Saint Petersburg University. Earth Sciences, 2018, vol. 63, issue 3, pp. 345–362.
metadata.lang: en_GB
metadata.name: dc.identifier.other
metadata.value: 10.21638/spbu07.2018.306
metadata.lang: -
metadata.name: dc.identifier.uri
metadata.value: http://hdl.handle.net/11701/14977
metadata.lang: -
metadata.name: dc.description.abstract
metadata.value: Using EN4 data-set from 1950 to 2015, the areas of the most intense deep convective mixing
  are identified as the maximum depths of the upper mixed layer during the cold season. It has
  been shown that the areas with the maximum registered convection depth of 1500–2000 m are
  found in the Greenland basin (73°–76° N, 5° W-1° E) and the Boreas basin (77° N, 1–2.5° W).
  This refines the areas of the deep convection derived from in situ data and results of hydrodynamic
  modeling. It has been shown that the previously separated in literature areas of deep
  convection in the Labrador Sea (55–59° N 50–56° W) and the Irminger Sea (57–60° N, 35–
  43° W), are in fact linked into one region by the episodic re-occurrence of the deep convection
  (1000 m and more) south of Greenland (between 56°–58° N). The intra-annual variability of
  deep convection was studied over the whole period of observations of 1950–2015. It is shown
  that the maximum depths of the upper mixed layer in all three seas was usually registered
  between December and May. The most often convection reaches the maximum depth in the
  Labrador and Irminger seas in March, and in the Greenland Sea — in April.
metadata.lang: en_GB
metadata.name: dc.description.sponsorship
metadata.value: Работа выполнена при финансовой поддержке Российского научного фонда, грант № 17–17-01151.
metadata.lang: en_GB
metadata.name: dc.language.iso
metadata.value: ru
metadata.lang: en_GB
metadata.name: dc.publisher
metadata.value: St Petersburg State University
metadata.lang: en_GB
metadata.name: dc.relation.ispartofseries
metadata.value: Vestnik of St Petersburg University. Earth Sciences;Volume 63; Issue 3
metadata.lang: -
metadata.name: dc.subject
metadata.value: North Atlantic
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: deep convection
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: EN4 data-set
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: depth of upper mixed layer
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Labrador
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Irminger
metadata.lang: en_GB
metadata.name: dc.subject
metadata.value: Greenland and Norwegian Seas
metadata.lang: en_GB
metadata.name: dc.title
metadata.value: Localization of areas of deep convection in the Nordic seas, the Labrador Sea and the Irminger Sea
metadata.lang: en_GB
metadata.name: dc.type
metadata.value: Article
metadata.lang: en_GB
resources.filename: 06-Fedorov.pdf
resources.url: https://dspace.spbu.ru/bitstream/11701/14977/1/06-Fedorov.pdf
resources.format: Adobe PDF
resources.size: 3,98 MB