Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2019, Vol. 16, No. 1, pp. 158-170
Analysis of satellite observations of chlorophyll concentration in the Peter the Great Gulf (Japan Sea)
V.V. Navrotsky
1 , V.A. Dubina
1, 2 , E.P. Pavlova
3 , F.F. Khrapchenkov
1 1 V.I. Il'ichev Pacific Oceanological Institute FEB RAS, Vladivostok, Russia
2 Far Eastern State Technical Fisheries University, Vladivostok, Russia
3 V.I. ll'ichev Pacific Oceanological Institite FEB RAS, Vladivistok, Russia
Accepted: 10.01.2019
DOI: 10.21046/2070-7401-2019-16-1-158-170
Results of daily satellite snapshots of chlorophyll concentration (CHL) in the Peter the Great Gulf area were analyzed for the period 2008–2017. Grouping of the snapshots is performed subject to prevailing of one of the four factors affecting chlorophyll concentration: shore proximity, current, eddies, convection. Seasonal tendency, revealed in chlorophyll spatial distributions, is considered in relation to seasonal changes of role of different physical mechanisms in delivery of necessary for primary production biogens into the photic layer. In most cases the pictures are formed by simultaneous action of several factors, but by frequency and CHL magnitude, the prevailing factor in the considered area was shore proximity. To explain the observed seasonal differences in chlorophyll distributions and their interrelations with physical processes, results of experiments in the near-shore region with depths of 20–40 m were used. In the satellite data maximum values of CHL in the near-shore region are not observed in the periods of maximum runoff from land, but it is observed in the periods of strong thermocline and maximum intensity of internal waves (IW) in the near-bottom layer. IW breaking leads to sharp amplification of mixing and bottom sediments resuspension. Internal waves are generated by interaction of tides, eddies, and currents over the continental slope with changeable steepness and curvature, and they carry energy of these large-scale motions to shores. Eddies of different scales and tidal currents are, at the same time, the main mechanisms of the near-shore waters ventilation and chlorophyll and phytoplankton redistribution over the area with additional input of local horizontal turbulence of different origin. Effect of upwelling along the shelf boundary, which most frequently appears in papers as the main object in study of shelf productivity, in our conditions reveals itself only indirectly against the background of other factors in absentia of seasonal thermocline.
Keywords: satellites, chlorophyll, shelf, continental slope, near-shore region, tide, eddies, upwelling, internal waves
Full textReferences:
- Kukarin V. F., Lyapidevskii V. Yu., Navrotsky V. V., Khrapchenkov F. F., Evolyutsiya vnutrennikh voln bol’shoi amplitudy v zone zapleska (Evolution of large amplitude internal waves in the “swash” zone), Fundamental’naya i prikladnaya gidrofizika, 2013, Vol. 6, No. 2, pp. 35–45.
- Lavrova O. Yu., Sabinin K. D., Proyavleniya inertsionnykh kolebanii na sputnikovykh izobrazheniyakh morskoi poverkhnosti (Manifestations of inertial oscillations in satellite images of the sea surface), Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2016, Vol. 13, No. 4, pp. 60–73.
- Ladychenko S. Yu., Lobanov V. B., Sinopticheskie vikhri v raione zaliva Petra Velikogo po sputnikovym dannym (Synoptic eddies in the Peter the Great Gulf according to satellite data), Issledovanie Zemli iz kosmosa, 2013, No. 4, pp. 3–15.
- Navrotsky V. V., Izergin V. L., Pavlova E. P., Generatsiya vnutrennikh voln vblizi granitsy shelfa (Generation of internal waves near the shelf boundary), Doklady Akademii Nauk, 2003, Vol. 388, No. 2, pp. 249–253.
- Navrotsky V. V., Lyapidevskii V. Yu., Pavlova E. P., Khrapchenkov F. F., Vnutrennie volny i peremeshivanie v shelfovoi zone morya (Internal waves and mixing in the shelf zone of sea), Izvestiya TINRO, 2010, Vol. 162, No. 3, pp. 24–37.
- Navrotsky V. V., Pavlova E. P., Vnutrennie volny i ikh biologicheskie effekty v shelfovoi zone morya (Internal wave and their biological effects in the shelf zone of sea), Vestynik DVO RAN, 2012, No. 6, pp. 22–31.
- Ponomarev V. I., Fayman P. A., Dubina V. A., Ladychenko S. Yu., Lobanov V. B., Synopticheskaya vikhrevaya dinamika nad severo-zapadnym sklonom i shelfom Yaponskogo morya (modelirovanie i resultaty distantsionnykh nablyudenii) (Synoptic vortical dynamics over the nord-western continental slope and shelf of the Japanese Sea (modeling and results of remote observations)), Sovremennye problemy distantsionnogo zondirovaniya Zemli iz kosmosa, 2011, Vol. 8, No. 2, pp. 482–485.
- Romankevich E. A., Vetrov A. A., Peresypkin V. I., Organicheskoe veshchestvo Mirovogo okeana (Organic matter in the World ocean), Geologiya i geofizika, 2009, Vol. 50, No. 4, pp. 401–411.
- Bourgault D., Kelley D. E., Galbraith P. S., Turbulence and boluses on an internal beach, J. Marine Research, 2008, Vol. 66, pp. 563–588.
- Boyce D. G., Dowd M., Lewis M. R., Worm B., Estimating global chlorophyll changes over the past century, Progress in Oceanography, 2014, Vol. 122, pp. 163–173.
- Callendar W., Klymak J. M., Foreman M. G. G., Tidal generation of large submesoscale eddy dipoles, Ocean Science, 2011, Vol. 7, pp. 487–502.
- Correa-Ramirez M. A., Hormazabal S. E., Morales C. E., Spatial patterns of annual and interannual surface chlorophyll-a variability in the Peru–Chile Current System, Progress in Oceanography, 2012, Vol. 92–95, pp. 8–17.
- Gregg W. W., Conkright M. E., Ginoux P., O’Reilly J. E., Casey N. W., Ocean primary production and climate: Global decadal changes, Geophysical Research Letters, 2003, Vol. 30, No. 15, p. 1809, DOI: 10.1029/2003GL016889.
- Masunaga E., Homma H., Yamazaki H., Fringer O. B., Nagai T., Kitade Y., Okayasu A., Mixing and sediment resuspension associated with internal bores in a shallow bay, Continental Shelf Research, 2015, Vol. 110, pp. 85–99.
- Moore C. D., Koseff J. R., Hult E. L., Characteristics of bolus formation and propagation from breaking internal waves on shelf slopes, J. Fluid Mechanics, 2016, Vol. 791, pp. 260–283.
- Moum J. N., Klymak J. M., Nash J. D., Perlin A., Smith W. D., Energy transport by nonlinear internal waves, J. Physical Oceanography, 2007, Vol. 37, pp. 1968–1988, DOI: 10.1175/JPO3094.1.
- Navrotsky V. V., Mixing caused by internal waves and turbulence: a comparative analysis, J. Marine Systems, 1999, Vol. 21, No. 1–4, pp. 131–145, DOI: 10.1016/S0924-7963(99)00010-X.
- Navrotsky V. V., Lozovatsky J. D., Pavlova E. P., Fernando H. J. S., Observations of internal waves and termocline splitting near a shelf break of the Sea of Japan (East Sea), Continental Shelf Research, 2004, Vol. 24, pp. 1375–1395, DOI: 10.1016/j.csr.2004.03.008.
- Navrotsky V. V., Lyapidevskii V. Yu., Pavlova E. P., Features of internal waves in a shoaling termocline, Intern. J. Geosciences, 2013, Vol. 4, pp. 871–879, DOI: 10.4236/ijg.2013.45081.
- Piontkovski A., Al-Jufaili S., Coastal upwellings and Mesoscale Eddies of the Western Arabian Sea: Some Biological Implications, Intern. J. Oceans and Oceanography, 2013, Vol. 7, No. 2, pp. 93–115.
- Whitney F. A., Crawford W. R., Harrison P. J., Physical processes that enhance nutrient transport and primary productivity in the coastal and open ocean of the subarctic NE Pacific, Deep-Sea Research II, 2005, Vol. 52, pp. 681–706.