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Mixing characteristics of the subarctic front in the Kuroshio-Oyashio confluence region

100%

Ke-Lan Z., Xi C., Ke-Feng M., Dong H., Sen H., Yan L.

Oceanologia

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2019

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tom 61

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nr 1

2

Thin chlorophyll layer concomitant of the thermohaline intrusion in the confluence of the Gulf Stream and Labrador Current (a case study)

100%

Karabashev G. S.

Oceanologia

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2019

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tom 61

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nr 4

3

Inflow of Atlantic-origin waters to the Barents Sea along glacial troughs

100%

Matishov G. G., Matishov D. G., Moiseev D. V.

Oceanologia

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2009

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tom 51

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nr 3

321-340

This paper discusses the role of glacial shelf topography in the formation of general oceanological and biological mechanisms in the Barents Sea. Analysis of geomorphological data and oceanographic observations obtained on board MMBI research vessels in 2001–08 has shown that: fluxes of Atlantic-origin waters pass along glacial troughs; the inflow of Atlantic waters to the Barents Sea from the west increased from 2001t ill 2007, although this advection began to weaken in 2008; vertical and horizontal thermohaline gradients intensified during the investigated period; a warm period similar to that of the 1930s was observed in the Barents Sea at the beginning of the 21st century.

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Impact of a dipole on the phytoplankton community in a semi-enclosed basin of the Southern Gulf of California, Mexico

100%

Duran-Campos E., Monreal-Gomez M. A., Salas de Leon D. A., Coria-Monter E.

Oceanologia

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2019

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tom 61

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nr 3

5

Distribution of phytoplankton along the thermohaline gradient in the North-Eastern Adriatic channel; winter aspect

80%

Vilicic D., Kuzmic M., Bosak S., Silovic T., Hrustic E., Buric Z.

Oceanologia

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2009

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tom 51

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nr 4

The distribution of phytoplankton and its relation to the hydrographic features in the north-eastern Adriatic was investigated in February 2008. The area of interest included a thermohaline gradient in the channel situated between the coast and the islands lying parallel to the coast. The gradient is controlled by the influx of oligotrophic karstic riverine water at the south-eastern end,subma rine springs in the middle part,an d warmer offshore waters at the north-western end of the channel. The change of temperature and salinity in the estuarine transition zone was accompanied by abundant diatoms and dinoflagellates below the halocline,with dominant chain-forming diatoms (Chaetoceros, Bacteriastrum) in abundances reaching 5×105 cells dm−3. The impact of coastal submarine springs detected by infrared remote sensing resulted in the growth of cyanobacteria in the nitrogen-depleted surface waters. The greater contribution of picoplankton, as well as of nanoplanktonic coccolithophorids and cryptophytes,in the outer channel system indicated their preference for oligotrophic conditions. Flow cytometric counts of nanophytoplankton were 10–30 times greater than inverted microscope counts. Cyanobacteria were about five times more abundant than picoeukaryotes. The study demonstrates how different techniques (remote sensing and in situ investigations) can be useful in understanding the biological and hydrographic set-up in the specific oligotrophic eastern Adriatic coastal environment.

Ograniczanie wyników

5 Oceanologia

1 Bosak S.

1 Buric Z.

1 Coria-Monter E.

1 Dong H.

1 Duran-Campos E.

1 Hrustic E.

1 Karabashev G. S.

1 Ke-Feng M.

1 Ke-Lan Z.

1 Kuzmic M.

1 Matishov D. G.

1 Matishov G. G.

1 Moiseev D. V.

1 Monreal-Gomez M. A.

1 Salas de Leon D. A.

1 Sen H.

1 Silovic T.

1 Vilicic D.

1 Xi C.

1 Yan L.

3 2019

2 2009

Mixing characteristics of the subarctic front in the Kuroshio-Oyashio confluence region

Thin chlorophyll layer concomitant of the thermohaline intrusion in the confluence of the Gulf Stream and Labrador Current (a case study)

Inflow of Atlantic-origin waters to the Barents Sea along glacial troughs

Impact of a dipole on the phytoplankton community in a semi-enclosed basin of the Southern Gulf of California, Mexico

Distribution of phytoplankton along the thermohaline gradient in the North-Eastern Adriatic channel; winter aspect