(Table 2) Observations of anticyclonic lenses of Mediterranean water in the Central North Atlantic ...

Analyses of spatial structure of hydrophysical fields and its vertical evolution in the Northeast Atlantic in a layer from the surface down to 2-2.5 km are carried out based on results of measurements in a testing area (31°-36°N, 20°-26°W) southeast of the Azores in autumn 1993. A description of an...

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Main Author: Aleinik, Dmitry L
Format: Dataset
Language:English
Published: PANGAEA 1998
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.767613
https://doi.pangaea.de/10.1594/PANGAEA.767613
id ftdatacite:10.1594/pangaea.767613
record_format openpolar
spelling ftdatacite:10.1594/pangaea.767613 2024-09-15T18:23:47+00:00 (Table 2) Observations of anticyclonic lenses of Mediterranean water in the Central North Atlantic ... Aleinik, Dmitry L 1998 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.767613 https://doi.pangaea.de/10.1594/PANGAEA.767613 en eng PANGAEA Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label Latitude of event Longitude of event DEPTH, water Depth, top/min Depth, bottom/max Radius Salinity change Temperature, difference Salinity Temperature, water Observation Multiple investigations Archive of Ocean Data ARCOD dataset Supplementary Dataset Dataset 1998 ftdatacite https://doi.org/10.1594/pangaea.767613 2024-08-01T10:51:52Z Analyses of spatial structure of hydrophysical fields and its vertical evolution in the Northeast Atlantic in a layer from the surface down to 2-2.5 km are carried out based on results of measurements in a testing area (31°-36°N, 20°-26°W) southeast of the Azores in autumn 1993. A description of an anti-cyclonic lens (ACL) of Mediterranean water (MW), which was found in the eastern part of the testing area from data of sets of sequential surveys, is presented. Analysis of CTD and XBT measurements in an area west of the lens allows to conclude that despite some contraction of width of the Azores Current directed eastward (from 60-80 km to 50-60 km) its total eastward volume transport for a period of time from October to November does not vary much. It is shown that intermediate salinity maxima in the northern part of the testing area formed by advection of MW and meddy destruction weakens while intersecting the Azores frontal zone (AFZ) from north to south, displacing itself to larger depth, and increases in ... : Supplement to: Aleinik, Dmitry L (1998): The structure and evolution of a meddy and Azores frontal zone in autumn 1993. Translated from Okeanologiya, 1998, 38(3), 349-360, Oceanology, 38(3), 312-322 ... Dataset North Atlantic Northeast Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
Latitude of event
Longitude of event
DEPTH, water
Depth, top/min
Depth, bottom/max
Radius
Salinity change
Temperature, difference
Salinity
Temperature, water
Observation
Multiple investigations
Archive of Ocean Data ARCOD
spellingShingle Event label
Latitude of event
Longitude of event
DEPTH, water
Depth, top/min
Depth, bottom/max
Radius
Salinity change
Temperature, difference
Salinity
Temperature, water
Observation
Multiple investigations
Archive of Ocean Data ARCOD
Aleinik, Dmitry L
(Table 2) Observations of anticyclonic lenses of Mediterranean water in the Central North Atlantic ...
topic_facet Event label
Latitude of event
Longitude of event
DEPTH, water
Depth, top/min
Depth, bottom/max
Radius
Salinity change
Temperature, difference
Salinity
Temperature, water
Observation
Multiple investigations
Archive of Ocean Data ARCOD
description Analyses of spatial structure of hydrophysical fields and its vertical evolution in the Northeast Atlantic in a layer from the surface down to 2-2.5 km are carried out based on results of measurements in a testing area (31°-36°N, 20°-26°W) southeast of the Azores in autumn 1993. A description of an anti-cyclonic lens (ACL) of Mediterranean water (MW), which was found in the eastern part of the testing area from data of sets of sequential surveys, is presented. Analysis of CTD and XBT measurements in an area west of the lens allows to conclude that despite some contraction of width of the Azores Current directed eastward (from 60-80 km to 50-60 km) its total eastward volume transport for a period of time from October to November does not vary much. It is shown that intermediate salinity maxima in the northern part of the testing area formed by advection of MW and meddy destruction weakens while intersecting the Azores frontal zone (AFZ) from north to south, displacing itself to larger depth, and increases in ... : Supplement to: Aleinik, Dmitry L (1998): The structure and evolution of a meddy and Azores frontal zone in autumn 1993. Translated from Okeanologiya, 1998, 38(3), 349-360, Oceanology, 38(3), 312-322 ...
format Dataset
author Aleinik, Dmitry L
author_facet Aleinik, Dmitry L
author_sort Aleinik, Dmitry L
title (Table 2) Observations of anticyclonic lenses of Mediterranean water in the Central North Atlantic ...
title_short (Table 2) Observations of anticyclonic lenses of Mediterranean water in the Central North Atlantic ...
title_full (Table 2) Observations of anticyclonic lenses of Mediterranean water in the Central North Atlantic ...
title_fullStr (Table 2) Observations of anticyclonic lenses of Mediterranean water in the Central North Atlantic ...
title_full_unstemmed (Table 2) Observations of anticyclonic lenses of Mediterranean water in the Central North Atlantic ...
title_sort (table 2) observations of anticyclonic lenses of mediterranean water in the central north atlantic ...
publisher PANGAEA
publishDate 1998
url https://dx.doi.org/10.1594/pangaea.767613
https://doi.pangaea.de/10.1594/PANGAEA.767613
genre North Atlantic
Northeast Atlantic
genre_facet North Atlantic
Northeast Atlantic
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.767613
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