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Estimation of the Relation between the Dispersion Features of Free Internal Waves and the Density Field Vertical Structure in the Barents and Kara Seas  id статьи: 565
Тип публикации
статья в журнале
Язык
En
Журнал
Physical Oceanography

ISSN:0928-5105
eSSN:1573-160X
Год
2020
Выходные данные
том 27
выпуск 1
страницы 18-27
EDN
Абстракт
Purpose. The aim of the paper is to investigate spatial-temporal dependences of the dispersion features of short-period free internal waves on the density field vertical structure in the Barents and Kara seas. Methods and Results. Based on the linearized equations of motion of the ideal incompressible and continuously stratified fluid, the dispersion features of free internal waves in the Barents and Kara seas were studied. Solution of the main boundary problem of the Sturm-Liouville type made it possible to obtain the own frequencies of five lowest modes and the own period of the internal waves' first mode. To calculate the density field, the World Ocean Atlas 2013 reanalysis data on temperature and salinity for 1955-2012 with resolution 0.25 degrees x 0.25 degrees were applied. The relation between the dispersion features of free internal waves and the density field vertical structure was analyzed, and dispersion characteristics of the internal waves in the Barents and Kara seas were compared. Conclusions. During the months when the density gradients are maximal, the internal waves of the highest frequency and the shortest period are observed. Among the intra-year maximums of the buoyancy depth-averaged frequency, the highest values (approximate to 0.02 s(-1)) are observed in the Barents Sea in July and August, and those of the Kara Sea-in July-September (approximate to 0.055 s-1) and in November (approximate to 0.058 s-1). In the same months, noted are the maximum values of the averaged natural frequencies and the minimum values of the averaged own period of the internal waves. Thus, for the wavelength 1000 m, the highest averaged own frequency and the smallest averaged own period of the first mode in the Barents Sea constitute 0.0025 s(-1) and 45 min., and those in the Kara Sea-0.0038 s(-1) and 30 min, respectively.
Ключевые слова
THE BARENTS SEA, THE KARA SEA, VAISALA-BRUNT FREQUENCY, INTERNAL WAVES, DISPERSION RELATIONS, OWN FREQUENCY, OWN PERIOD
Дата занесения
2020-06-02 18:10:00
Scopus
Статус есть
Квартиль Q4
WoS
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Квартиль --
РИНЦ
Статус есть
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количество баллов за публикацию
4
количество баллов каждому автору
1.33
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Финансирование:

0827-2019-0003
Фундаментальные исследования океанологических процессов, определяющих состояние и эволюцию морской среды под влиянием естественных и антропогенных факторов, на основе методов наблюдения и моделирования