Statistical classification and sea surface temperature characteristics of mesoscale eddies in the Northwestern Pacific

YAO Xiangyu, SHI Yunlong, CHEN Shi

Journal of Marine Sciences ›› 2026, Vol. 44 ›› Issue (2) : 35-42.

PDF(3886 KB)
PDF(3886 KB)
Journal of Marine Sciences ›› 2026, Vol. 44 ›› Issue (2) : 35-42. DOI: 10.3969/j.issn.1001-909X.2026.02.004

Statistical classification and sea surface temperature characteristics of mesoscale eddies in the Northwestern Pacific

Author information +
History +

Abstract

Based on a satellite altimetry-derived eddy dataset, this study conducted a classification-based statistical and characteristic analysis of mesoscale eddies in the Northwestern Pacific. A composite analysis method was further employed to reconstruct the spatial structures of sea surface temperature anomalies (SSTAs) and sea level anomalies (SLAs) associated with different eddy categories and to investigate the distribution characteristics of mesoscale eddies in the study area. The study region was divided into three subregions: the North Equatorial Current (NEC), the Subtropical Countercurrent (STCC), and the Kuroshio Extension (KE). November to December and January to April were defined as the cold season, while May to October were defined as the warm season. Eddies were classified, counted, and analyzed according to their polarity. The results show that mesoscale eddies in the study region are generally characterized by cold-core cyclonic eddies and warm-core anticyclonic eddies. However, two types of abnormal eddies, namely warm-core cyclonic eddies and cold-core anticyclonic eddies, are also identified, accounting for approximately 22.5%of the total eddy population. The occurrence probability of abnormal eddies is higher at low latitudes than at high latitudes, and higher in the warm season than in the cold season. For normal eddies, SSTA is positively correlated with eddy amplitude, increases with latitude, and is generally stronger in the cold season than in the warm season. In contrast, abnormal eddies exhibit overall weaker SSTAs than normal eddies and show no obvious regional or seasonal differences. Composite analysis further reveals that compared with normal eddies, abnormal eddies are less circular in shape and have smaller amplitudes and weaker SSTA variations.

Key words

Northwestern Pacific / mesoscale eddy / sea surface temperature anomaly / spatial structure / abnormal eddies / seasonal variability / Subtropical Countercurrent region / Kuroshio Extension

Cite this article

Download Citations
YAO Xiangyu , SHI Yunlong , CHEN Shi. Statistical classification and sea surface temperature characteristics of mesoscale eddies in the Northwestern Pacific[J]. Journal of Marine Sciences. 2026, 44(2): 35-42 https://doi.org/10.3969/j.issn.1001-909X.2026.02.004

References

[1]
杨光. 西北太平洋中尺度涡旋研究[D]. 青岛: 中国科学院研究生院(中国科学院海洋研究所), 2013.
YANG G. A study on the mesoscale eddies in the northwestern Pacific Ocean[D]. Qingdao: Institute of Oceanology, Chinese Academy of Sciences, 2013.
[2]
DAI J, WANG H Z, ZHANG W M, et al. Observed spatiotemporal variation of three-dimensional structure and heat/salt transport of anticyclonic mesoscale eddy in Northwest Pacific[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1654-1675.
[3]
WANG Y, ZHANG J H, YU J C, et al. Anticyclonic mesoscale eddy induced mesopelagic biomass hotspot in the oligotrophic ocean[J]. Journal of Marine Systems, 2023, 237: 103831.
[4]
胡冬, 陈希, 毛科峰, 等. 黑潮延伸体邻近区域中尺度涡特征统计分析[J]. 海洋与湖沼, 2018, 49(3):497-511.
HU D, CHEN X, MAO K F, et al. Statistical characteristics of mesoscale eddies near the Kuroshio extension region[J]. Oceanologia et Limnologia Sinica, 2018, 49(3): 497-511.
[5]
HAUSMANN U, CZAJA A. The observed signature of mesoscale eddies in sea surface temperature and the associated heat transport[J]. Deep Sea Research Part I: Oceanographic Research Papers, 2012, 70: 60-72.
[6]
M K, WANG F, LI Y L, et al. Structure of sea surface temperature anomaly induced by mesoscale eddies in the north Pacific Ocean[J]. Journal of Geophysical Research: Oceans, 2022, 127(3): e2021JC017581.
[7]
刘颖洁, 田丰林, 陈戈. 南海中尺度涡旋海表温度特征统计研究[J]. 中国海洋大学学报:自然科学版, 2020, 50(5):146-156.
LIU Y J, TIAN F L, CHEN G. Statistical characterization of sea surface temperature over mesoscale eddies in the South China Sea[J]. Periodical of Ocean University of China, 2020, 50(5): 146-156.
[8]
张铷火, 陈旭, 宁珏, 等. 太平洋中纬度不同区域气旋式暖涡和反气旋式冷涡的结构研究[J]. 海洋与湖沼, 2024, 55(3):599-612.
ZHANG R H, CHEN X, NING J, et al. Structures of “abnormal” eddies in different regions of the mid-latitude Pacific Ocean[J]. Oceanologia et Limnologia Sinica, 2024, 55(3): 599-612.
[9]
BROKAW R J, SUBRAHMANYAM B, TROTT C B, et al. Eddy surface characteristics and vertical structure in the Gulf of Mexico from satellite observations and model simulations[J]. Journal of Geophysical Research: Oceans, 2020, 125(2): e2019JC015538.
[10]
JULIAN P, PENG L. Interaction between the subtropical and equatorial ocean circulations: The subtropical cell[J]. Journal of Physical Oceanography, 1994, 24 (2): 466-497.
[11]
CHELTON D B, SCHLAX M G, SAMELSON R M. Global observations of nonlinear mesoscale eddies[J]. Progress in Oceanography, 2011, 91(2): 167-216.
[12]
HE Q Y, ZHAN H G, CAI S Q, et al. A new assessment of mesoscale eddies in the South China Sea: Surface features, three-dimensional structures, and thermohaline transports[J]. Journal of Geophysical Research: Oceans, 2018, 123(7): 4906-4929.
[13]
汤博, 侯一筠, 殷玉齐, 等. 北太平洋副热带逆流区中尺度涡旋的统计特征及其分布规律[J]. 海洋与湖沼, 2019, 50(5):937-947.
TANG B, HOU Y J, YIN Y Q, et al. Statistical characte-ristics of mesoscale eddies and the distribution in the north Pacific subtropical countercurrent[J]. Oceanologia et Limnologia Sinica, 2019, 50(5): 937-947.
[14]
SANDALYUK N V, BOSSE A, BELONENKO T V. The 3-D structure of mesoscale eddies in the Lofoten Basin of the Norwegian Sea: A composite analysis from altimetry and in situ data[J]. Journal of Geophysical Research: Oceans, 2020, 125(10): e2020JC016331.
[15]
LIU Y J, ZHENG Q A, LI X F. Characteristics of global ocean abnormal mesoscale eddies derived from the fusion of sea surface height and temperature data by deep learning[J]. Geophysical Research Letters, 2021, 48(17): e2021GL094772.
[16]
GAUBE P, CHELTON D B, SAMELSON R M, et al. Satellite observations of mesoscale eddy-induced Ekman pumping[J]. Journal of Physical Oceanography, 2015, 45(1): 104-132.
[17]
NI Q B, ZHAI X M, YANG Z B, et al. Generation of cold anticyclonic eddies and warm cyclonic eddies in the tropical oceans[J]. Journal of Physical Oceanography, 2023, 53(6): 1485-1498.
[18]
SUN W J, DONG C M, TAN W, et al. Statistical characteristics of cyclonic warm-core eddies and anticyclonic cold-core eddies in the north Pacific based on remote sensing data[J]. Remote Sensing, 2019, 11(2): 208.
[19]
TIMMERMANS M L, TOOLE J, PROSHUTINSKY A, et al. Eddies in the Canada Basin, Arctic Ocean, observed from ice-tethered profilers[J]. Journal of Physical Oceanography, 2008, 38(1): 133-145.
[20]
ITOH S, YASUDA I. Water mass structure of warm and cold anticyclonic eddies in the western boundary region of the subarctic north Pacific[J]. Journal of Physical Oceanography, 2010, 40(12): 2624-2642.
[21]
SUN W J, LIU Y, CHEN G X, et al. Three-dimensional properties of mesoscale cyclonic warm-core and anticyclonic cold-core eddies in the South China Sea[J]. Acta Oceanologica Sinica, 2021, 40(10): 17-29.
[22]
HE Q Y, ZHAN H G, CAI S Q. Anticyclonic eddies enhance the winter barrier layer and surface cooling in the Bay of Bengal[J]. Journal of Geophysical Research: Oceans, 2020, 125(10): e2020JC016524.
PDF(3886 KB)

Accesses

Citation

Detail

Sections
Recommended

/