Circulation and Mesoscale Eddies in the Sea of Japan from Satellite Altimetry Data

IF 0.9 4区 地球科学 Q4 METEOROLOGY & ATMOSPHERIC SCIENCES
I. A. Zhabin, E. V. Dmitrieva, S. N. Taranova, V. B. Lobanov
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Abstract

The spatial distribution and seasonal variability of mesoscale eddies in the Sea of Japan have been investigated based on the regional database created from the AVISO Mesoscale Eddies Trajectory Atlas (1993–2020). The database contains information about the trajectories and parameters of mesoscale eddies in the Sea of Japan. The eddy detection method is based on the analysis of altimetric maps of absolute dynamic topography. A total of 578 eddies with a lifetime of more than 90 days have been identified (273 anticyclonic and 305 cyclonic). The average lifetime of eddies is 202 days for anticyclonic and 143 days for cyclonic and mean radius of 58 km for anticyclonic and 61 km for cyclonic. The mean speed of anticyclones and cyclones along their trajectories is 2.8 and 3.7 cm/s; the mean orbital velocities of geostrophic currents are 19.0 and 15.1 cm/s, respectively. The maximum number of cases of formation and destruction of anticyclones falls in July–September during the period with high values of water inflow through the Korea Strait. Most of the cyclonic eddies are generated between January and June and decay during the cold half of the year (October–March). A joint analysis of maps of the mean surface circulation in the Sea of Japan (satellite altimetry data) and the spatial distribution of mesoscale eddy shows that the stable eddies of the Sea of Japan are associated with the quasi-stationary meanders of the East Korea East Korea Warm Curent, Subpolar Front, and Tsushima current. The position of meanders is mainly determined by the interaction of the currents with the bottom topography.

Abstract Image

从卫星测高数据看日本海的环流和中尺度涡流
摘要 根据 AVISO 中尺度涡旋轨迹图集(1993-2020 年)建立的区域数据库,研究了日本海中尺度涡旋的空间分布和季节变化。该数据库包含日本海中尺度涡旋的轨迹和参数信息。漩涡探测方法基于对绝对动态地形测高图的分析。共发现了 578 个寿命超过 90 天的漩涡(273 个反气旋漩涡和 305 个气旋漩涡)。漩涡的平均寿命为:反气旋 202 天,气旋 143 天;平均半径为:反气旋 58 公里,气旋 61 公里。反气旋和气旋沿其轨迹的平均速度分别为 2.8 和 3.7 厘米/秒;地气流的平均轨道速度分别为 19.0 和 15.1 厘米/秒。反气旋形成和破坏的最多时间为 7-9 月,这一时期通过朝鲜海峡的入水量较大。大部分气旋涡旋产生于 1 月至 6 月,并在冷半年(10 月至 3 月)衰减。对日本海平均表层环流图(卫星测高数据)和中尺度涡旋空间分布的联合分析表明,日本海的稳定涡旋与东朝鲜东暖流、副极地锋和对马海流的准静止蜿蜒有关。蜿蜒流的位置主要取决于海流与海底地形的相互作用。
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来源期刊
CiteScore
1.40
自引率
28.60%
发文量
56
审稿时长
6-12 weeks
期刊介绍: Izvestiya, Atmospheric and Oceanic Physics is a journal that publishes original scientific research and review articles on vital issues in the physics of the Earth’s atmosphere and hydrosphere and climate theory. The journal presents results of recent studies of physical processes in the atmosphere and ocean that control climate, weather, and their changes. These studies have possible practical applications. The journal also gives room to the discussion of results obtained in theoretical and experimental studies in various fields of oceanic and atmospheric physics, such as the dynamics of gas and water media, interaction of the atmosphere with the ocean and land surfaces, turbulence theory, heat balance and radiation processes, remote sensing and optics of both media, natural and man-induced climate changes, and the state of the atmosphere and ocean. The journal publishes papers on research techniques used in both media, current scientific information on domestic and foreign events in the physics of the atmosphere and ocean.
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