

FOLLOWUS
1.College of Marine Geosciences, Key Laboratory of Submarine Geosciences and Prospecting Technique, Ocean University of China, Qingdao 266100, China
2.Laboratory for Marine Geology, Qingdao Marine Science and Technology Center, Qingdao 266237, China
3.State Key Laboratory of Submarine Geosciences, Second Institute of Oceanography, Ministry of Natural Resources, Hangzhou 310012, China
tangyong@sio.org.cn
hjwang@mail.ouc.edu.cn
Received:29 August 2024,
Published:01 July 2025
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ZHU Libin,TANG Yong,WANG Houjie,et al.Suspended particulate matter delivery modulated by mesoscale eddies in the southern Mozambique Channel[J].Journal of Oceanology and Limnology,2025,43(04):1106-1121.
ZHU Libin,TANG Yong,WANG Houjie,et al.Suspended particulate matter delivery modulated by mesoscale eddies in the southern Mozambique Channel[J].Journal of Oceanology and Limnology,2025,43(04):1106-1121. DOI: 10.1007/s00343-024-4234-2.
Mesoscale eddies are widespread in the global ocean
significantly influencing the physical
chemical
and biological structures of water column. Based on the CTD data and suspended particulate matter (SPM) data collected at 36 hydrographic stations during a field cruise in southern Mozambique Channel
combined with satellite altimeter observations
we identified a series of mesoscale eddies traversing the Mozambique Channel. Our hydrographic measurements
coupled with in situ chlorophyll fluorescence data
reveal that these eddies significantly influence thermohaline structure and chlorophyll distribution
which in turn affects primary productivity and SPM concentrations in the upper ocean. The cyclonic eddies facilitate the upwelling of cold subsurface water
leading to a shallowing of the pycnocline and the creation of a low-temperature anomaly with variable salinity anomalies at different depths. Conversely
anticyclonic eddies submerge warm surface water
deepening the pycnocline
and resulting in a high-temperature anomaly accompanied by distinct salinity patterns. Significantly
a coastal anticyclonic eddy was observed to intercept terrestrial material from the Delagoa Bight
redirecting it west of 36°E. This study presents unique and quasi-synchronous CTD datasets capturing mesoscale eddy impacts
and provided valuable insights into SPM variability within the often-neglected southern Mozambique Channel.
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