Chlorophyll Pigment Concentration and Sea Surface Temperature of the Black Sea

Year 2018, Volume: 2 Issue: 1, 13 - 17, 20.03.2018

Mehmet Tahir Kavak

https://doi.org/10.31015/jaefs.18003

Abstract

As an enclosed sea, the Black Sea has countless economic activities (mainly tanker traffic and fisheries) and recreational activities, with the consequence of being threatened by dramatic dangers and pollution. Optical remote sensing can provide a novel look at physical processes and then driving mechanisms. It is worthwhile to know how the temperature and other marine parameters change on seasonal and long-term scales. In the paper CZCS (Coastal Zone Color Scanner) and AVHRR (Advanced Very High Resolution Radiometer) satellite were used to study the relationship between photosynthesis and SST since phytoplankton forms the very lowest clement in the marine ecosystem.  Satellite derived data could provide information on the amount of sea life present in any given area throughout the world. The information could also be useful in connection with studies of global changes m temperature and what effect they could have on the total abundance of marine life. Present work which used CD-ROM set from NASA did not found evidence of correlation between chlorophyll pigment concentration and SST of the Black Sea with 99.95% certainty, three channel algorithm or the use of fluorescence or chlorophyll absorption peak in the red suggested for future work.

Keywords

Phytoplankton, CZCS, AVHRR, Black Sea

References

• [1] Hood, R. Abbot, M.R. Huyer, A. Korso, P.M. (1990). Surface patterns in temperature, flow, phytoplankton biomass, and species composition in the coastal transition zone off northern California. Journal of Geophsical Research, 95 (10): 18,081-18,094.
• [2] Robinson C, LeB. Williams PJ. (1993). Temperature and Antarctic Plankton community respiration. Journal of Plankton Research, 15 (9):1035–1051.
• [3] Nykjaer L, Van Camp L. (1989). Remote Sensing of the Northwest African upwelling area. Analysis and interpretation of simultaneous pairs of GAC derived sea surface temperature and CZCS derived chlorophyll-like pigment concentration images. Final report, vol.1,2,3 Unimar Sciences ApS., under JRC contract N?3326-87-12 ed ISP DK. In Institute for Remote Sensing Applications JRC annual report.
• [4] Ackleson, S. Balch, W.M. Holligan, P.M. (1988). White Waters of the Gulf of Maine. Oceanography, 1(2):18-22.
• [5] Thomas M.H.B. (1980). Coastal and Marine Applications of Remote Sensing. In: A. P. C, editor: Published by the Remote Sensing Society, 28p.
• [6] Barale V, Schlittenhardt P. (1994). Remote Sensing From Research to Operational Applications in the New Europe. In: Vaughan R, editor: Springer Hungarica. Proceedings of the 13th EARSeL Symposium, Dundee, Scotland, U.K., 28 June-I July, 1993”. Edited by R. A. VAUGHAN. (Springer Hungarica, Budapest and EARSeL, Paris: EARSeL, 422p.
• [7] Barale, V. Murray, C.N. (1995) The surface colour field of enclosed marine basins: Pigment patterns of the Black Sea. Remote Sensing Reviews, 12:61.
• [8] Tran, A.V. Simith, E. Hyon, J. Evans, R. Brown, O. (1993). Feldman G. Satellite-Derived Multichannel Sea Surface Temperature and Phytoplankton Pigment Concentration Data: A CD-ROM Set Containing Monthly Mean Distributions for the Global Oceans. In: Laboratory JP, editor. Pasadena, CA.
• [9] La Violette, P.E. (1994). Monitoring the Coastal and Marine Environmental with Satellite Data. Sistema Terra 3:57.
• [10] Singh, S.M. (1992). Ocean colour from space: Radiative transfer. In: Cracknell AP, editor. Space Oceanography: World Scientific; 139.
• [11] Bowers, D.G. Harker, G.E.L. Stephan, B. (1996). Absorption spectra of inorganic particles in the Irish Sea and their relevance to remote sensing of chlorophyll. International Journal of Remote Sensin, 17:2449.