(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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Online Access: | https://dx.doi.org/10.1594/pangaea.767613 https://doi.pangaea.de/10.1594/PANGAEA.767613 |
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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 |
_version_ |
1810464039901331456 |