Войти
Features of Currents on the Black Sea Northwestern Shelf Based on the Numerical Simulation Results  id статьи: 1016
Тип публикации
статья в журнале
Язык
En
Журнал
PHYSICAL OCEANOGRAPHY

ISSN:0928-5105
eSSN:1573-160X
Год
2021
Выходные данные
том 28
выпуск 4
страницы 426-437
EDN
Абстракт
Purpose. The work is aimed at studying the features of currents on the Black Sea northwestern shelf based of the reanalysis results, and at analyzing the reasons of these features. Methods and Results. To analyze the currents on the northwestern shelf, applied were the results of physical reanalysis of the Black Sea fields performed by the authors earlier, namely, the arrays of hydrodynamic fields on a regular grid with the 21-year duration (1992-2012). Surface currents on the northwestern shelf of the Black Sea are directed mainly to the southwest. Throughout the whole year (except for the summer months when the wind effect weakens), an intensive compensatory current directed to the south is formed along the western coast. The waters near the western coast are highly horizontally stratified that is caused by fresh water inflowing with the river runoffs. In winter seasons, the stratification is most pronounced, whereas in summer, the horizontal density gradient decreases. The horizontal density stratification leads to the following: starting from the depth similar to 20 m, the pressure gradient changes its sign and the along-coastal jet countercurrent directed to the north, occurs. Conclusions. The performed studies have shown that the water circulation on the Black Sea northwestern shelf is determined mainly by the following factors: the wind-induced water flows across the shelf boundary and strong horizontal water stratification near the western coast resulted from the river runoffs. As the currents on the sea surface are directed mainly to the southwest, the compensatory current directed to the south is formed near the western coast. Due to the strong horizontal stratification resulted from the river runoffs, a countercurrent directed to the north is formed in the subsurface layer near the western coast. In case the seawater flows to the shelf are extremely high, the countercurrent may be absent.
Ключевые слова
Black sea, Circulation, Countercurrent, Northwestern shelf, Reanalysis
Дата занесения
2021-10-08 10:14:24
Scopus
Статус есть
Квартиль Q4
WoS
Статус есть
Квартиль --
РИНЦ
Статус есть
Импакт-фактор --
количество баллов за публикацию
6
количество баллов каждому автору
3
история начисления баллов за квартал:
Финансирование:

0827-2021-0002