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Addendum to “Stokes transport in layers in the water column based on long-term wind statistics: assessment using long-term wave statistics”

100%

Myrhaug D., Wang H., Holmedal L. E.

Oceanologia

|

2019

|

tom 61

|

nr 4

2

Stokes transport in layers in the water column based on long-term wind statistics

100%

Myrhaug D., Wang H., Holmedal L. R.

Oceanologia

|

2018

|

tom 60

|

nr 3

3

On the sound scattering at 30 kHz and its relationship to the large-scale circulation pattern in the Greenland Sea

100%

Ostrowski M.

Oceanologia

|

1990

|

tom 29

4

Average nutrient and chlorophyll distributions in the Western Mediterranean: RADMED project

100%

Garcia-Martinez M. C., Vargaz-Yanez M., Moya F., Santiago R., Munoz M., Reul A., Ramirez T., Balbin R.

Oceanologia

|

2019

|

tom 61

|

nr 1

5

Observed variability in physical and biogeochemical parameters in the Central Arabian Gulf

84%

Rakib F., Al-Ansari E. M. A. S., Husrevoglu Y. S., Yigiterhan O., Al-Maslamani I., Aboobacker V. M., Vethamony P.

Oceanologia

|

2021

|

tom 63

|

nr 2

6

Variability of temperature and salinity over the last decade in selected regions of the Southern Baltic Sea

84%

Rak D., Wieczorek P.

Oceanologia

|

2012

|

tom 54

|

nr 3

Changes in the basic physical properties of selected areas of the Baltic Proper were analysed on the basis of the results of a 12-year series of high-resolution measurements collected during cruises of r/v ‘Oceania’. The high-resolution CTD sections covered three main basins: the Bornholm Basin, Słupsk Furrow and Gdańsk Basin. Positive temperature trends of 0.11 and 0.16◦C year−1 were observed in the surface and deep layers respectively. The salinity trend was also positive. The rise in the air temperature has probably caused the increase in surface water temperature, while advection has been of greater significance in the deep layer. The increase in salinity coincides with the more frequent occurrence of small and medium-size inflows through the Danish Straits, even though large inflows are evidently less frequent than used to be the case. The seasonal variability of temperature in the water column was analysed. The phase shift in the seasonal evolution with depth is described. The maximum temperature shift in the waters investigated varies from 32 to 38 days.

7

Dynamic features of successive upwelling events in the Baltic Sea - a numerical case study

84%

Myrberg K., Andrejev O., Lehmann A.

Oceanologia

|

2010

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tom 52

|

nr 1

77-99

Coastal upwelling often reveals itself during the thermal stratification season as an abrupt sea surface temperature (SST) drop. Its intensity depends not only on the magnitude of an upwelling-favourable wind impulse but also on the temperature stratification of the water column during the initial stage of the event. When a ‘chain’ of upwelling events is taking place, one event may play a part in forming the initial stratification for the next one; consequently, SST may drop significantly even with a reduced wind impulse. Two upwelling events were simulated on the Polish coast in August 1996 using a three-dimensional, baroclinic prognostic model. The model results proved to be in good agreement with in situ observations and satellite data. Comparison of the simulated upwelling events show that the first one required a wind impulse of 28 000 kg m−1 s−1 to reach its mature, full form, whereas an impulse of only 7500 kg m−1 s−1 was sufficient to bring about a significant drop in SST at the end of the second event. In practical applications like operational modelling, the initial stratification conditions prior to an upwelling event should be described with care in order to be able to simulate the coming event with very good accuracy.

8

Distributions of photosynthetic and photoprotecting pigment concentrations in the water column in the Baltic Sea: an improved mathematical description

84%

Ston-Egiert J., Majchrowski R., Ostrowska M.

Oceanologia

|

2019

|

tom 61

|

nr 1

9

Kongsfjorden and Hornsund hydrography - comparative study based on a multiyear survey in fjords of West Spitsbergen

84%

Prominska A., Cisek M., Walczowski W.

Oceanologia

|

2017

|

tom 59

|

nr 4

A recent study has shown increased warming in the fjords of west Spitsbergen. Their location is critical, as they are situated along the main northward pathway of Atlantic Water (AW) which is a great source of heat to the Arctic Ocean and the fjords. In the light of ongoing warming, we aim to discuss differences between the fjords under northward transformation of oceanic waters. We compared summer hydrographic conditions in two fjords located in two opposite ends of west Spistbergen: Hornsund in the south and Kongsfjorden in the north. The study is based on high resolution CTD measurements collected during Arctic cruises between 2001 and 2015. The emphasis was put not only on differences in water temperature, salinity and water masses but also the freshwater content (FWC), AW transport and heat delivery to the fjords. In general, the water in Kongsfjorden is on average 18C warmer and its salinity is higher by 0.5 compared to Hornsund. It is also characterized by two times greater transport of AW and heat delivery to the fjord. On the other hand, Hornsund reveals two times higher FWC. Both fjords undergo a gradual warming due to an increased presence of Atlantic origin waters. The ongoing warming is accompanied by an increase in variability of temperature and salinity dependent on the domination of the Sørkapp Current (SC) or the West Spitsbergen Current (WSC) on the West Spitsbergen Shelf (WSS). Nonetheless, Hornsund remains more Arctic-type fjord compared to Kongsfjorden, due to stronger blocking by SC.

10

Dissolved oxygen variability in the Southern Baltic Sea in 2013—2018

84%

Rak D., Walczowski W., Dzierzbicka-Glowacka L., Shchuka S.

Oceanologia

|

2020

|

tom 62

|

nr 4PA

11

Live autochthonous benthic diatoms on the lower depths of Arctic continental shelf. Preliminary results

84%

Druzhkova E., Oleinik A., Makarevich P.

Oceanologia

|

2018

|

tom 60

|

nr 1

An autochthonous community of benthic diatoms was discovered in June 2015 in the upper sediment layer at depths of 170, 205, and 245 m in the central Barents Sea. At least three benthic microalgae species (Gyrosigma fasciola, Pleurosigma angulatum, and Pleurosigma sp. 1) were detected in the sediment but not the upper water column. Analyses revealed that these benthic microalgae represent a depleted fragment of Arctic littoral microphytobenthos. Compared with the littoral flora, the deep-water assemblage is less diverse and displays low abundance. The data reported here challenge the generally accepted belief that the presence of certain microalgae at significant depths results from vertical or horizontal transfer.

12

Estimation of zooplankton mortality caused by an Arctic glacier outflow

84%

Zajaczkowski M. J., Legezynska J.

Oceanologia

|

2001

|

tom 43

|

nr 3

341-351

The outflow of freshwater from underwater channels in the Kongsbreen tidal glacier in Kongsfjorden, Svalbard, 79◦ N, was measured as 138.8 m3 s−1 at the peak of the melting season. Experiments on local marine plankton mortality show that when exposed to salinities below 9 PSU, all copepods die within 15 minutes. We estimate that during 100 days of the melting season, as many as 85 tonnes wet weight (WW) of plankton is removed from the water column due to osmotic shock, which makes up 15% of the standing zooplankton biomass of the fjord. The dead zooplankton sinks after exposure to low salinities and is probably an important food source for scavenging benthic fauna in the fjord. This mechanism could be responsible for the high numbers of Onisimus caricus near the glacier front.

13

On the buoyant sub-surface salinity maxima in the Gulf of Riga

84%

Liblik T., Skudra M., Lips U.

Oceanologia

|

2017

|

tom 59

|

nr 2

Thermohaline structure in the Gulf of Riga (GoR) was investigated by a multiplatform measurement campaign in summer 2015. Stratification of the water column was mainly controlled by the temperature while salinity had only a minor contribution. Buoyant salinity maxima with variable strength were observed in the intermediate layer of the Gulf of Riga. The salinity maxima were likely formed by a simultaneous upwelling—downwelling event at the two opposite sides of the Irbe strait. The inflowing salty water did not reach the deeper (> 35 m) parts of the gulf and, therefore, the near-bottom layer of the gulf remained isolated throughout the summer. Thus, the lateral water exchange regime in the near bottom layer of the Gulf of Riga is more complicated than it was thought previously. We suggest that the occurrence of this type of water exchange resulting in a buoyant inflow and lack of lateral transport into the near-bottom layers might contribute to the rapid seasonal oxygen decline in the Gulf of Riga

14

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

84%

Albarakati A. M. A., Ahmad F.

Oceanologia

|

2012

|

tom 54

|

nr 4

15

Can poor foraging habitat [an inundated opencast sulphur mine] be attractive to the great crested grebe [Podiceps cristatus]?

84%

Gwiazda R.

Oceanological and Hydrobiological Studies

|

2009

|

tom 38

|

nr 3

135-139

16

Influence of the parametrization of water optical properties on the modelled sea surface temperature in the Baltic Sea

84%

Stramska M., Zuzewicz A.

Oceanologia

|

2013

|

tom 55

|

nr 1

17

Coastal hydrodynamics beyond the surf zone of the South Baltic Sea

84%

Ostrowski R., Stella M., Szmytkiewicz P., Kapinski J., Marcinkowski T.

Oceanologia

|

2018

|

tom 60

|

nr 3

18

Annual cycle of phytoplankton community through the water column: Study applied to the implementation of bivalve offshore aquaculture in the Southeastern Bay of Biscay

84%

Muniz O., Revilla M., Rodriguez J. G., Laza-Martinez A., Fontan A.

Oceanologia

|

2019

|

tom 61

|

nr 1

19

Tintinnids near pack-ice between South Shetland and the South Orkney Islands (26 Dec. 1998-18 Jan. 1989)

84%

Wasik A., Mikolajczyk E.

Acta Protozoologica

|

1990

|

tom 29

|

nr 3

20

Deposition, return flux, and burial rates of nitrogen and phosphorus in the sediments of two high-Arctic fjords

84%

Koziorowska K., Kulinski K., Pempkowiak J.

Oceanologia

|

2018

|

tom 60

|

nr 4

Ograniczanie wyników

Addendum to “Stokes transport in layers in the water column based on long-term wind statistics: assessment using long-term wave statistics”

Stokes transport in layers in the water column based on long-term wind statistics

On the sound scattering at 30 kHz and its relationship to the large-scale circulation pattern in the Greenland Sea

Average nutrient and chlorophyll distributions in the Western Mediterranean: RADMED project

Observed variability in physical and biogeochemical parameters in the Central Arabian Gulf

Variability of temperature and salinity over the last decade in selected regions of the Southern Baltic Sea

Dynamic features of successive upwelling events in the Baltic Sea - a numerical case study

Distributions of photosynthetic and photoprotecting pigment concentrations in the water column in the Baltic Sea: an improved mathematical description

Kongsfjorden and Hornsund hydrography - comparative study based on a multiyear survey in fjords of West Spitsbergen

Dissolved oxygen variability in the Southern Baltic Sea in 2013—2018

Live autochthonous benthic diatoms on the lower depths of Arctic continental shelf. Preliminary results

Estimation of zooplankton mortality caused by an Arctic glacier outflow

On the buoyant sub-surface salinity maxima in the Gulf of Riga

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

Can poor foraging habitat [an inundated opencast sulphur mine] be attractive to the great crested grebe [Podiceps cristatus]?

Influence of the parametrization of water optical properties on the modelled sea surface temperature in the Baltic Sea

Coastal hydrodynamics beyond the surf zone of the South Baltic Sea

Annual cycle of phytoplankton community through the water column: Study applied to the implementation of bivalve offshore aquaculture in the Southeastern Bay of Biscay

Tintinnids near pack-ice between South Shetland and the South Orkney Islands (26 Dec. 1998-18 Jan. 1989)