

FOLLOWUS
1.College of Meteorology and Oceanography, National University of Defense Technology, Changsha 410073, China
2.Naval Research Academy, Tianjin 300061, China
WANG Huizan, wanghuizan@126.com
收稿:2019-05-31,
录用:2019-8-1,
网络首发:2020-12-02,
纸质出版:2020-11
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Characterizing the capability of mesoscale eddies to carry drifters in the northwest Pacific[J]. 海洋湖沼学报(英文), 2020,38(6):1711-1728.
Huizan WANG, Ding LIU, Weimin ZHANG, et al. Characterizing the capability of mesoscale eddies to carry drifters in the northwest Pacific[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1711-1728.
Characterizing the capability of mesoscale eddies to carry drifters in the northwest Pacific[J]. 海洋湖沼学报(英文), 2020,38(6):1711-1728. DOI: 10.1007/s00343-019-9149-y.
Huizan WANG, Ding LIU, Weimin ZHANG, et al. Characterizing the capability of mesoscale eddies to carry drifters in the northwest Pacific[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1711-1728. DOI: 10.1007/s00343-019-9149-y.
Mesoscale eddies are common oceanic phenomena. Although many related studies have been conducted
the ability for mesoscale eddies to carry real particles remains poorly addressed. We considered the drifters as real particles to characterize the capability of mesoscale eddies to carry particles. Firstly
mesoscale eddies in the northwest Pacific (99°E-180°E
0°-66°N) were identified using sea level anomaly (SLA) data from 1993 to 2015. Secondly
three important parameters (the carrying days
the number of circles the drifter revolving around the eddy center
and the carrying distances) were calculated by colocalizing eddy data with drifters. Finally
statistical analysis and composite analysis were conducted
reflecting the capability of mesoscale eddies to carry particles. The mechanisms on the carrying capability of eddies were also discussed. Results show that (1) the motion of carried drifters reflects the upper limit of rotational speed of eddies that the drifters revolve around the eddy center by ≤ 90° for one day in most cases; (2) the drifters tend to be carried for a longer time when their minimal distances to the eddy center measured with normalized distance are small; (3) there are two types of eddies (cyclonic and anticyclonic eddies) in different subregions of northwest Pacific
and each has a different carrying capability (on average
similar in the tropical ocean and Subtropical Countercurrent
cyclonic eddies tend to have stronger carrying capability in Southern Kuroshio Extension
and anticyclonic eddies tend to have stronger carrying capability in Northern Kuroshio Extension and Subarctic Gyre); (4) on average
the carried drifters tend to travel for a longer time around the normalized eddy radii ranging from 0.41 to 0.76; (5) the carrying days are related to the Rossby number of the eddy (in general when the Rossby number is smaller
the carrying days are longer).
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