Seasonal and inter-annual temperature variability in the bottom waters over the western Black Sea shelf

Long-term changes in the state of the Bottom Shelf Water (BSW) on the Western shelf of the Black Sea are assessed using analysis of intra-seasonal and inter-annual temperature variations. For the purpose of this study the BSW is defined as such shelf water mass between the seabed and the upper mixed...

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Main Authors: G. I. Shapiro, F. Wobus, D. L. Aleynik
Format: Article
Language:English
Published: Copernicus Publications 2011-09-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/7/585/2011/os-7-585-2011.pdf
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spelling doaj-58eee53a0e3d4b7686d7834fd2b85e112020-11-25T01:29:17ZengCopernicus PublicationsOcean Science1812-07841812-07922011-09-017558559610.5194/os-7-585-2011Seasonal and inter-annual temperature variability in the bottom waters over the western Black Sea shelfG. I. ShapiroF. WobusD. L. AleynikLong-term changes in the state of the Bottom Shelf Water (BSW) on the Western shelf of the Black Sea are assessed using analysis of intra-seasonal and inter-annual temperature variations. For the purpose of this study the BSW is defined as such shelf water mass between the seabed and the upper mixed layer (bounded by the σ<sub>θ</sub> = 14.2 isopycnal) which has limited ability to mix vertically with oxygen-rich surface waters during the warm season due to formation of a seasonal pycnocline. A long-term time series of temperature anomalies in the BSW is constructed from in-situ observations taken over the 2nd half of the 20th century. The BSW is shown to occupy nearly half of the shelf area during the summer stratification period (May–November).The results reveal a warm phase in the 1960s/70s, followed by a cold phase between 1985 and 1995 and a further warming after 1995. The transition between the warm and cold periods coincides with a regime shift in the Black Sea ecosystem. While it was confirmed that the memory of winter convection is well preserved over the following months in the deep sea, the signal of winter cooling in the BSW significantly reduces during the warm season. The potential of the BSW to ventilate horizontally during the warm season with the deep-sea waters is assessed using isopycnic analysis of temperature variations. It is shown that temperature in the BSW is stronger correlated with the temperature of Cold Intermediate Waters (CIW) in the deep sea than with the severity of the previous winters, thus indicating that the isopycnal exchanges with the deep sea are more important for inter-annual/inter-decadal variability of the BSW on the western Black Sea shelf than effects of winter convection on the shelf itself.http://www.ocean-sci.net/7/585/2011/os-7-585-2011.pdf
collection DOAJ
language English
format Article
sources DOAJ
author G. I. Shapiro
F. Wobus
D. L. Aleynik
spellingShingle G. I. Shapiro
F. Wobus
D. L. Aleynik
Seasonal and inter-annual temperature variability in the bottom waters over the western Black Sea shelf
Ocean Science
author_facet G. I. Shapiro
F. Wobus
D. L. Aleynik
author_sort G. I. Shapiro
title Seasonal and inter-annual temperature variability in the bottom waters over the western Black Sea shelf
title_short Seasonal and inter-annual temperature variability in the bottom waters over the western Black Sea shelf
title_full Seasonal and inter-annual temperature variability in the bottom waters over the western Black Sea shelf
title_fullStr Seasonal and inter-annual temperature variability in the bottom waters over the western Black Sea shelf
title_full_unstemmed Seasonal and inter-annual temperature variability in the bottom waters over the western Black Sea shelf
title_sort seasonal and inter-annual temperature variability in the bottom waters over the western black sea shelf
publisher Copernicus Publications
series Ocean Science
issn 1812-0784
1812-0792
publishDate 2011-09-01
description Long-term changes in the state of the Bottom Shelf Water (BSW) on the Western shelf of the Black Sea are assessed using analysis of intra-seasonal and inter-annual temperature variations. For the purpose of this study the BSW is defined as such shelf water mass between the seabed and the upper mixed layer (bounded by the σ<sub>θ</sub> = 14.2 isopycnal) which has limited ability to mix vertically with oxygen-rich surface waters during the warm season due to formation of a seasonal pycnocline. A long-term time series of temperature anomalies in the BSW is constructed from in-situ observations taken over the 2nd half of the 20th century. The BSW is shown to occupy nearly half of the shelf area during the summer stratification period (May–November).The results reveal a warm phase in the 1960s/70s, followed by a cold phase between 1985 and 1995 and a further warming after 1995. The transition between the warm and cold periods coincides with a regime shift in the Black Sea ecosystem. While it was confirmed that the memory of winter convection is well preserved over the following months in the deep sea, the signal of winter cooling in the BSW significantly reduces during the warm season. The potential of the BSW to ventilate horizontally during the warm season with the deep-sea waters is assessed using isopycnic analysis of temperature variations. It is shown that temperature in the BSW is stronger correlated with the temperature of Cold Intermediate Waters (CIW) in the deep sea than with the severity of the previous winters, thus indicating that the isopycnal exchanges with the deep sea are more important for inter-annual/inter-decadal variability of the BSW on the western Black Sea shelf than effects of winter convection on the shelf itself.
url http://www.ocean-sci.net/7/585/2011/os-7-585-2011.pdf
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