Wyniki wyszukiwania

1

Investigating the role of atmospheric variables on sea level variations in the Eastern Central Red Sea using an artificial neural network approach

100%

Zubier K. M., Eyouni L. S.

Oceanologia

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2020

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tom 62

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nr 3

2

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Upwelling dynamics in the Baltic Sea studied by a combined SAR-infrared satellite data and circulation model analysis

100%

Gurova E., Lehmann A., Ivanov A.

Oceanologia

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2013

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tom 55

|

nr 3

3

Verification of a certain numerical model with the real storm surge of December 1976 in the Baltic Sea

100%

Chilicka Z.

Oceanologia

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1984

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tom 19

4

The effects of cyanobacterial blooms on MODIS-L2 data products in the Southern Caspian Sea

84%

Naghdi K., Moradi M., Kabiri K., Rahimzadegan

Oceanologia

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2018

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tom 60

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nr 3

5

Water column conditions in a coastal lagoon near Jeddah, Red Sea

84%

Albarakati A. M. A., Ahmad F.

Oceanologia

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2012

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tom 54

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nr 4

6

Extreme sea levels at selected stations on the Baltic Sea coast

84%

Wolski T., Wisniewski B., Giza A., Kowalewska-Kalkowska H., Boman H., Grabbi-Kaiv S., Hammarklint T., Holfort J., Lydeikaite Z.

Oceanologia

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2014

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tom 56

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nr 2

7

Effect of drag coefficient formula choice on wind stress climatology in the North Atlantic and the European Arctic

84%

Wrobel-Niedzwiecka I., Drozdowska V., Piskozub J.

Oceanologia

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2019

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tom 61

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nr 3

8

Horizontal distribution of phytoplankton and zooplankton from the littoral towards open waters under wind stress

84%

Zurek R., Bucka H.

Oceanological and Hydrobiological Studies

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2004

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tom 33

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nr 3

9

Meteorological influences on the surface hydrographic patterns of the North Aegean Sea

67%

Sylaios G.

Oceanologia

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2011

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tom 53

|

nr 1

Hydrographic data from the North Aegean Sea were used to examine the summer variability of surface water masses during the period 1998–2001. Attention was placed on the surface hydrographic features of the area, such as the Black Sea Water (BSW) plume expansion, the frontal characteristics of the BSW with the Levantine Intermediate Water (LIW) and the variability of submesoscale hydrographic features (such as the Samothraki Anticyclone). Strong southerly wind stresses were found responsible for relaxing the horizontal density gradients across the BSW-LIW frontal zone and displacing this front to the north of Lemnos Island, thus suppressing the Samothraki Anticyclone towards the Thracian Sea continental shelf. Under northerly winds, the BSW-LIWfront returns to its regular position (south of Lemnos Island), thus allowing the horizontal expansion of the Samothraki gyre up to the Athos Peninsula. Present results indicate the importance of medium-term wind stress effects on the generation of Samothraki Anticyclone suppression/expansion events.

10

Physical aspects of extreme storm surges and falls on the Polish coast

67%

Wisniewski B., Wolski T.

Oceanologia

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2011

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tom 53

|

nr (1-TI)

Extreme sea levels – storm-generated surges and falls – on the Polish coast are usually the effects of three components: the volume of water in the southern Baltic (the initial level preceding a given extreme situation), the action of tangential wind stresses in the area (wind directions: whether shore- or seaward; wind velocities; and wind action duration), and the sea surface deformation produced by deep, mesoscale baric lows moving rapidly over the southern and central Baltic that generate the so-called baric wave. Among these factors, the baric wave is particularly important for, i.e. the water cushion underneath the baric depression, moving along the actual atmospheric pressure system over the sea surface.

11

Simulation of nutrient transport from different depths during an upwelling event in the Gulf of Finland

67%

Vali G., Zhurbas V., Laanemets J., Elken J.

Oceanologia

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2011

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tom 53

|

nr (1-TI)

Numerical simulation experiments with a high-resolution circulation model were carried out to study nutrient transport from different depths to the surface 10-m layer during an upwelling event along the northern coast of the Gulf of Finland in July 1999. The initial nutrient distribution is based on field measurements performed in the north-western part of the Gulf. Wind forcing covering the period of the upwelling along the northern coast was turned through 180◦ to simulate an upwelling along the southern coast. The simulation results showed that the main phosphorus transport to the upper 10-m layer occurred from depths shallower than 30 m for the upwelling events along both the northern and the southern coasts. Nitrogen transport to the upper 10-m layer was the largest from depths of 40–55 m for the upwelling along the northern and 40–65 m for the upwelling along the southern coast. Simulated cumulative volume transports to the upper 10-m layer from different depths showed that the contribution from deeper layers was larger in the case of the upwelling along the southern coast. The reduction of wind stress had a bigger influence on water transport from the deeper layers.

Ograniczanie wyników

Investigating the role of atmospheric variables on sea level variations in the Eastern Central Red Sea using an artificial neural network approach

Upwelling dynamics in the Baltic Sea studied by a combined SAR-infrared satellite data and circulation model analysis

Verification of a certain numerical model with the real storm surge of December 1976 in the Baltic Sea

The effects of cyanobacterial blooms on MODIS-L2 data products in the Southern Caspian Sea

Water column conditions in a coastal lagoon near Jeddah, Red Sea

Extreme sea levels at selected stations on the Baltic Sea coast

Effect of drag coefficient formula choice on wind stress climatology in the North Atlantic and the European Arctic

Horizontal distribution of phytoplankton and zooplankton from the littoral towards open waters under wind stress

Meteorological influences on the surface hydrographic patterns of the North Aegean Sea

Physical aspects of extreme storm surges and falls on the Polish coast

Simulation of nutrient transport from different depths during an upwelling event in the Gulf of Finland