SOME FEATURES OF THE BLACK SEA SEASONAL THERMOHALINE VARIABILITY: MODERN VIEW
Results of statistical processing and physical analyses of the historical and recent hydrographic data set are presented. Seasonal thermohaline (hydrographic) variabilities of the Black Sea main baroclinic layer (0–200 m) are considered. In the upper 50-m layer, seasonal thermohaline variability is...
| Main Author: | |
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| Format: | Article |
| Language: | English |
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Lomonosov Moscow State University
2010-06-01
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| Series: | Geography, Environment, Sustainability |
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| Online Access: | https://ges.rgo.ru/jour/article/view/253 |
| _version_ | 1797878532173463552 |
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| author | Valentin Tuzhilkin |
| author_facet | Valentin Tuzhilkin |
| author_sort | Valentin Tuzhilkin |
| collection | DOAJ |
| description | Results of statistical processing and physical analyses of the historical and recent hydrographic data set are presented. Seasonal thermohaline (hydrographic) variabilities of the Black Sea main baroclinic layer (0–200 m) are considered. In the upper 50-m layer, seasonal thermohaline variability is generated mainly by the heat and freshwater fluxes across the sea surface. In the main pycnocline between depths of 50 and 200 m it is caused by the flux of the wind-stress relative vorticity. Thermohaline effects of these processes are described. |
| first_indexed | 2024-04-10T02:33:41Z |
| format | Article |
| id | doaj.art-7d8a3b5d7fd5423f8ba614007d022f82 |
| institution | Directory Open Access Journal |
| issn | 2071-9388 2542-1565 |
| language | English |
| last_indexed | 2024-04-10T02:33:41Z |
| publishDate | 2010-06-01 |
| publisher | Lomonosov Moscow State University |
| record_format | Article |
| series | Geography, Environment, Sustainability |
| spelling | doaj.art-7d8a3b5d7fd5423f8ba614007d022f822023-03-13T07:52:30ZengLomonosov Moscow State UniversityGeography, Environment, Sustainability2071-93882542-15652010-06-0132425010.24057/2071-9388-2010-3-2-42-50249SOME FEATURES OF THE BLACK SEA SEASONAL THERMOHALINE VARIABILITY: MODERN VIEWValentin TuzhilkinResults of statistical processing and physical analyses of the historical and recent hydrographic data set are presented. Seasonal thermohaline (hydrographic) variabilities of the Black Sea main baroclinic layer (0–200 m) are considered. In the upper 50-m layer, seasonal thermohaline variability is generated mainly by the heat and freshwater fluxes across the sea surface. In the main pycnocline between depths of 50 and 200 m it is caused by the flux of the wind-stress relative vorticity. Thermohaline effects of these processes are described.https://ges.rgo.ru/jour/article/view/253the black seatemperaturesalinityseasonal variability |
| spellingShingle | Valentin Tuzhilkin SOME FEATURES OF THE BLACK SEA SEASONAL THERMOHALINE VARIABILITY: MODERN VIEW Geography, Environment, Sustainability the black sea temperature salinity seasonal variability |
| title | SOME FEATURES OF THE BLACK SEA SEASONAL THERMOHALINE VARIABILITY: MODERN VIEW |
| title_full | SOME FEATURES OF THE BLACK SEA SEASONAL THERMOHALINE VARIABILITY: MODERN VIEW |
| title_fullStr | SOME FEATURES OF THE BLACK SEA SEASONAL THERMOHALINE VARIABILITY: MODERN VIEW |
| title_full_unstemmed | SOME FEATURES OF THE BLACK SEA SEASONAL THERMOHALINE VARIABILITY: MODERN VIEW |
| title_short | SOME FEATURES OF THE BLACK SEA SEASONAL THERMOHALINE VARIABILITY: MODERN VIEW |
| title_sort | some features of the black sea seasonal thermohaline variability modern view |
| topic | the black sea temperature salinity seasonal variability |
| url | https://ges.rgo.ru/jour/article/view/253 |
| work_keys_str_mv | AT valentintuzhilkin somefeaturesoftheblackseaseasonalthermohalinevariabilitymodernview |