ISSN 2070-7401 (Print), ISSN 2411-0280 (Online)
Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa
CURRENT PROBLEMS IN REMOTE SENSING OF THE EARTH FROM SPACE

  

Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2014, Vol. 11, No. 3, pp. 28-41

Variability of the June reflectance maximum in the Black Sea according to the decadal satellite data

G.S. Karabashev1 , M.A. Evdoshenko1 
1 P.P. Shirshov Institute of Oceanology RAS, Moscow, Russia
A study is made of the coccolithophore blooms occurring in the Black Sea from late May to early July. The blooms enable one to monitor the vital activity of algae in aquatic environment by satellite means thanks to the multiple enhancement of the sea surface reflectance. We used the data of ocean color scanners SeaWiFS and MODIS-Aqua from 2001 to 2012 placing more emphasis on variations of reflectance in 2012, the year of extraordinary powerful blooming. According to comparative analysis of reflectance changes within the four ecologically-different testing regions, the blooming covers solely the deep-water basin, features considerable spatial inhomogeneity, and peaks in the east of the sea. It is shown that the manifestations of blooming relax faster in the longwave range of the visible spectrum than in its middle part which is most probably due to the difference of thicknesses of layers where the ascending radiances of shorter and longer wavelength originate. Our findings refine the patterns of coccolithophore blooming in the Black Sea and must be taken into account when interpreting the early-summer images of the basin.
Keywords: remote sensing, coccolithophore bloom, the Black Sea, long-term variability, the June anomaly of reflectance
Full text

References:

  1. Gertman I.F. Poverhnosti razdela v strukture dejatel'nogo sloja morja (Interfaces in the active layer structure of the sea), Gidrometeorologija i gidrohimija morej SSSR. Vol. 4. Chernoe more. No. 1. Gidrometeorologicheskie uslovija, Leningrad: Gidrometeoizdat, 1991, pp. 170-175.
  2. Karabashev G.S., Sheberstov S.V., Jakubenko V.G. Ijun'skij maksimum normalizovannoj jarkosti i ego svjaz' s gidrologicheskimi uslovijami i cveteniem kokkolitoforid v Chernom more (The June maximum of the normalized radiance and its relation to hydrological regime and coccolithophore blooming in the Black Sea), Okeanologija, 2006, Vol. 46, No. 3, pp. 331-343.
  3. Kopelevich O.V., Burenkov V.I., Vazjulja S.V., Sheberstov S.V. Problemy indikacii kokkolitoforidnyh cvetenij po sputnikovym dannym (Problems of indication of coccolithophore blooms from the satellite data), Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2012, Vol. 9, No. 5, pp. 241-250.
  4. Makeeva L.P. Oblachnost' i solnechnoe sijanie (Cloudiness and sunshine) Gidrometeorologija i gidrohimija morej SSSR. Vol. 4. Chernoe more. No. 1. Gidrometeorologicheskie uslovija, Saint Petersburg: Gidrometeoizdat, 1991, pp. 57-68.
  5. Man'kovskij V.I., Man'kovskaja U.V., Solov'ev M.V. Gidroopticheskie harakteristiki Chernogo morja. Spravochnik (The hydrooptical characteristics of the Black Sea. Handbook), Sevastopol': MGI NAN Ukrainy, 2009, 90 p.
  6. Titov V.B. Formirovanie verhnego konvektivnogo sloja i holodnogo promezhutochnogo sloja v Chernom more v zavisimosti ot surovosti zim (Origination of the upper convective layer and cool intermediate layer in the Black Sea depending on the severity of winters), Okeanologija, 2004, Vol. 44, No. 3, pp. 354-357.
  7. Jasakova O.N., Stanichnyj S.V. Anomal'noe cvetenie Emiliania huxleyi (Prymnesiophyceae) v Chjornom more v 2012 g (Anomalous blooming of Emiliania huxleyi (Prymnesiophyceae) in the Black Sea in 2012), Mors'kij ekologіchnij zhurnal, 2012, Vol. 11, No. 4, p. 54.
  8. Burenkov V.I., Kopelevich O.V., Pautova L.V., Prokhorenko O.V., Rusakov V.Yu., Sheberstov S.V. Possible causes of the increased content of suspended particles in the northeastern part of the Black Sea in June, Oceanology, 2005, Vol. 45, Suppl. 1, pp. 39-S50.
  9. Cokacar T., Oguz.T., Kubilay N. Satellite-detected early summer coccolithophore blooms and their interannual variability in the Black Sea, Deep-Sea Res., 2004, Vol. 51, No. 8, pp. 1017-1031.
  10. Iglesias-Rodriguez, M.D., Brown, C. W., Doney, S. C., Kleypas, J., Kolber D., Kolber Z., Hayes P.K., Falkowski P.G. Representing key phytoplankton functional groups in ocean carbon cycle models: coccolithophorids, Global Biogeochem. Cycles, 2002, Vol. 16, No. 4, pp. 47-1–47-20, doi:10.1029/2001GB001454.
  11. Kara A.B., Wallcraft A.J., Hurlburt H.E. A new solar radiation penetration scheme for use in ocean mixed layer studies: an application to the Black Sea using a fine-resolution Hybrid Coordinate Ocean Model (HYCOM) , Journal of Physical Oceanography, 2005. Vol. 35, No. 1, pp. 13-23, doi: http://dx.doi.org/10.1175/JPO2677.1
  12. Tyrrell T., Merico A. Emiliania huxleyi: bloom observations and the conditions that induce them // Coccolithophores. From Molecular Processes to Global Impact, Berlin-Heidelberg-New York: Springer-Verlag, 2004, pp. 76-97.