Characteristics of Suspended Matter in the South Ocean in the 20ºE Region Based on the Measurements of Light Volume Scattering Functions
V. I. Mankovsky, E. V. Mankovskaya✉
Marine Hydrophysical Institute of RAS, Sevastopol, Russian Federation
✉ e-mail: emankovskaya@mhi-ras.ru
Abstract
Purpose. The purpose of the work is to present and discuss the results of determining the mass concentration of suspended matter and its organic and mineral fractions by measuring the light volume scattering functions in the South Ocean in the 20ºE meridian region from 37º to 55ºS.
Methods and Results. The measurement data on the light volume scattering function were obtained in the 10^th^ cruise of the R/V “Akademik Vernadsky” in January–February, 1975 at the oceanographic section along the 20ºE meridian from 37º to 55ºS at the stations located 1º apart. The suspended matter composition was calculated based on the results of these measurements. The distribution of mass concentration of the suspended matter (total, organic and mineral) at the section was obtained. The maximum increase in the organic suspension concentration at the section was observed in the area of water rise at 53ºS: Corg = 0.830 mg/l (Ctotal = 1.062 mg/l), that indicates the highest water productivity in this region. Based on the empirical relationship with the organic suspension concentration, the chlorophyll concentration at the section was calculated. The relation between the total mass concentration of suspended matter and the scattering coefficient in surface waters in the form Ctotal = 1.496 s~520~ – 0.0676 (R = 0.95) was established. The features of the organic suspension vertical distribution in the areas of water rise and lowering, and with no signs of water vertical movement were considered.
Conclusions. Measurements of the light volume scattering functions in the South Ocean in the region of 20ºE and 37º–55ºS permitted to obtain the data on mass concentration of the total suspended matter, as well as its organic and mineral fractions. The maximum concentration of organic suspension is located in the vicinity of the average long-term position of the Polar Front, where the mass development of phytoplankton is observed regularly. The features of vertical structure of the suspension organic fraction are directly related to the water vertical dynamics. There is a close relationship between the mass concentration of total suspended matter and the scattering coefficient in the surface waters.
Keywords
light volume scattering function, suspended matter, organic suspended matter, mineral suspended matter, suspended matter concentration, South Ocean
Acknowledgements
The study was carried out within the framework of state assignment of the FRC MHI on themes No. FNNN-2021-0003 and No. FNNN-2021-0005.
Original russian text
Original Russian Text © V. I. Mankovsky, E. V. Mankovskaya, 2023, published in MORSKOY GIDROFIZICHESKIY ZHURNAL, Vol. 39, Iss. 3, pp. 371-383 (2023)
For citation
Mankovsky, V.I. and Mankovskaya, E.V., 2023. Characteristics of Suspended Matter in the South Ocean in the 20ºE Region Based on the Measurements of Light Volume Scattering Functions. Physical Oceanography, 30(3), pp. 343-354. doi:10.29039/1573-160X-2023-3-343-354
DOI
10.29039/1573-160X-2023-3-343-354
References
- Man’kovsky, V.I., 2014. Optical Characteristics of the South Atlantic Ocean Waters in the Region of 20º E and 37 – 55º S. Morskoy Gidrofizicheskiy Zhurnal, (6), pp. 61-70 (in Russian).
- Bathmann, U.V., Scharek, R., Klaas, C., Dubischar, C.D. and Smetacek, V., 1997. Spring Development of Phytoplankton Biomass and Composition in Major Water Masses of the Atlantic Sector of the Southern Ocean. Deep Sea Research Part II: Topical Studies in Oceanography, 44(1-2), pp. 51-67. doi:10.1016/S0967-0645(96)00063-X
- Bracher, A.U. and Tilzer, M.M., 2001. Underwater Light Field and Phytoplankton Absorbance in Different Surface Water Masses of the Atlantic Sector of the Southern Ocean. Polar Biology, 24(9), pp. 687-696. doi:10.1007/s003000100269
- Laubscher, R.K., Perissinotto, R. and McQuaid, C.D., 1993. Phytoplankton Production and Biomass at Frontal Zones in the Atlantic Sector of the Southern Ocean. Polar Biology, 13(7), pp. 471-481. doi:10.1007/BF00233138
- Read, J.F., Pollard, R.T. and Bathmann, U., 2002. Physical and Biological Patchiness of an Upper Ocean Transect from South Africa to the Ice Edge near the Greenwich Meridian. Deep-Sea Research Part II: Topical Studies in Oceanography, 49(18), pp. 3713-3733. doi:10.1016/S0967-0645(02)00108-X
- Strass, V.H., Naveira Garabato, A.C., Pollard, R.T. Fischer, H.I., Hense, I., Allen, J.T., Read, J.F., Leach, H. and Smetacek, V., 2002. Mesoscale Frontal Dynamics: Shaping the Environment of Primary Production in the Antarctic Circumpolar Current. Deep-Sea Research Part II: Topical Studies in Oceanography, 49(18), pp. 3735-3769. doi:10.1016/S0967-0645(02)00109-1
- Sosik, H.M. and Olson, R.J., 2002. Phytoplankton and Iron Limitation of Photosynthetic Efficiency in the Southern Ocean during Late Summer. Deep Sea Research Part I: Oceanographic Research Papers, 49(7), pp. 1195-1216. doi:10.1016/S0967-0637(02)00015-8
- Wulff, A. and Wängberg, S.-Å., 2004. Spatial and Vertical Distribution of Phytoplankton Pigments in the Eastern Atlantic Sector of the Southern Ocean. Deep-Sea Research Part II: Topical Studies in Oceanography, 51(22-24), pp. 2701-2713. doi:10.1016/j.dsr2.2001.01.002
- Demidov, A.B., Vedernikov, V.I. and Sheberstov, S.V., 2007. Spatiotemporal Variability of Chlorophyll a in the Atlantic and Indian Sectors of the Southern Ocean during February-April of 2000 according to Satellite and Expeditionary Data. Oceanology, 47(4), pp. 507-518. doi:10.1134/S000143700704008X
- Churin, D.A. and Gulyugin, S.Yu., 2017. Aspects of Dynamics of Chlorophyll-a in Relation to the Absolute Dynamic Topography of the Antarctic Part of the Atlantic. Trudy VNIRO, 169, pp. 117-125 (in Russian).
- Shifrin, K.S., 1988. Physical Optics of Ocean Water. New York: American Institute of Physics, 285 p.