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1

The main factors forming the climate of the Hornsund [Spitsbergen].

100%
Niedzwiedz T.
Zeszyty Naukowe Uniwersytetu Jagiellońskiego. Prace Geograficzne
|
1993
49-63
2

Uwagi w sprawie notatki P. Klysza pt. Problem powstawania walow lodowo-morenowych na przykladzie lodowcow w rejonie fiordu Hornsund [Spitsbergen]

75%
Kozarski S.
Przegląd Geograficzny. Polska Akademia Nauk
|
1995
|
tom 67
|
nr 3-4
373-375
3

Observations of the Arctic charr, Salvelinus alpinus [L., 1758] from the Hornsund [Vest Spitsbergen] in 1985-1987

75%
Radziun K.
Acta Ichthyologica et Piscatoria. Supplementum
|
1993
|
tom 23
7-22
4
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Aerosol optical properties over Svalbard: a comparison between Ny-Alesund and Hornsund

75%
Pakszys P., Zielinski T.
Oceanologia
|
2017
|
tom 59
|
nr 4
This paper presents the CAMS model based aerosol optical properties calculated for two Spitsbergen fjords, Kongsfjorden (Ny-Ålesund) and Hornsund (Polish Polar Station in Hornsund) measured between 2010 and 2015. A small decrease in Aerosol Optical Depth (AOD) is shown throughout the study period leading to an alteration of the state of the polar atmosphere. However, the potential differences observed between the stations were not statistically significant. While during the studied period no significant differences in chemical composition between the stations were observed, increasing mean values of Black Carbon (BC) were found to be associated with an increasing number of wild forest fires in remote areas producing smoke plumes, which are further transported over vast distances and reach Spitsbergen.
5

Problem powstania walow lodowo-morenowych na przykladzie lodowcow w rejonie fiordu Hornsund [Spitsbergen]

75%
Klysz P.
Przegląd Geograficzny. Polska Akademia Nauk
|
1995
|
tom 67
|
nr 1-2
121-132
6

Recent benthic Ostracoda from Hornsund, south Spitsbergen, Svalbard Archipelago

75%
Mackiewicz A.
Polish Polar Research
|
2006
|
tom 27
|
nr 1
71-90
This paper includes a check-list of Recent Svalbard marine ostracods based on published sources and on diploma theses as well as some new studies. This is the first study of this group of crustaceans from Hornsund. A total of 41 species belonging to 12 families were collected at 55 sampling stations from dredged sediments. Seven species are reported for the first time from the Svalbard Archipelago. Polycope orbicularis Sars is the most abundant species in the present fauna. Species compositions of Hornsund and the Liefde- fjorden are seen to have the highest similarity (S = 50.6).
7

Radiocarbon dating of marine bivalve shells from Holocene moraines at inner Hornsund, South Spitsbergen

75%
Birkenmajer K., Olsson I. U.
Bulletin of the Polish Academy of Sciences. Earth Sciences
|
1997
|
tom 45
|
nr 1
8

The first documented record of Sphagnum riparium [Bryophyta: Sphagnaceae] from Spitsbergen

63%
Wojtun B.
Polish Polar Research
|
2007
|
tom 28
|
nr 4
269-276
Sphagnum riparium (Bryophyta) is recorded and described from the Wedel Jarlsberg Land on Spitsbergen, the Arctic Svalbard Archipelago. It is the northernmost known population of the species in the Northern Hemisphere. The distribution of the two known Sphagnum species in the Hornsund area, viz. S. riparium and S. squarrosum is mapped and described.
9
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

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

63%
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
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

The impact of a non-uniform land surface on the radiation environment over an Arctic fjord – a study with a 3D radiative transfer model for stratus clouds over the Hornsund fjord, Spitsbergen

63%
Rozwadowska A., Gorecka I.
Oceanologia
|
2012
|
tom 54
|
nr 4
11

Length growth of Arctic charr, Salvelinus alpinus [L., 1758] in the Hornsund region

63%
Krzykawski S.
Acta Ichthyologica et Piscatoria. Supplementum
|
1993
|
tom 23
67-81
12
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Ecosystem maturation follows the warming of the Arctic fjords

63%
Weslawski J. M., Buchholz F., Gluchowska M., Weydmann A.
Oceanologia
|
2017
|
tom 59
|
nr 4
Two fjords in West Spitsbergen (Hornsund 77°N and Kongsfjorden 79°N) differ with regard to their exposure towards increasingly warm Atlantic water inflow. Hornsund remains in many respects cooler than Kongsfjorden (on average 2°C SST in summer) and is less influenced by warmer and more saline Atlantic waters. Reported changes in the physical environment (temperature rise, freshwater inflow, salinity drop, turbidity, fast-ice reduction, coastal change) are discussed in the context of biological observations in the pelagic and benthic realms with special reference to krill (Euphausiacea). We conclude that well-documented changes in the physical environment have had little effect on the fjord biota and that both organisms and their ecological functions in the fjords are well adapted to the scale of ongoing change. The observed changes fit the definition of ecosystem maturation, with greater diversity, a more complex food web and dispersed energy flow at the warmer site.
13

Preliminary studies on bone fluoride content in the Arctic charr, Salvelinus alpinus [L.] from the Hornsund region

63%
Protasowicki M.
Acta Ichthyologica et Piscatoria. Supplementum
|
1993
|
tom 23
133-135
14

Morphological characteristics of Arctic charr, Salvelinus alpinus [L., 1758] from the Hornsund area of Vest Spitsbergen

63%
Heese T.
Acta Ichthyologica et Piscatoria. Supplementum
|
1993
|
tom 23
23-29
15
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Aerosol physical properties in Spitsbergen's fjords: Hornsund and Kongsfjorden during AREX campaigns in 2014 and 2015

63%
Markuszewski P., Rozwadowska A., Cisek M., Makuch P., Petelski T.
Oceanologia
|
2017
|
tom 59
|
nr 4
We present results of measurements of aerosol physical properties conducted on board of r/v Oceania during two cruises to the Spitsbergen region in 2014 (AREX 2014) and 2015 (AREX 2015). Measurements of aerosol size distribution, aerosol scattering coefficient and black carbon concentrations were made in two different Spitsbergen fjords: Hornsund and Kongsfjorden. The aerosol size distribution was measured in the size range from 0.09 μm to 47 μm using two aerosol size distribution spectrometers and a standard condensation particle counter. For the scattering coefficient an integrating nephelometer was used. Black carbon concentration was measured by an aethalometer. Temporal variabilities in physical properties of aerosol observed during the AREX 2014 and AREX 2015 campaigns were much higher than the differences between both fjords. The basic factors influencing aerosol conditions were advection and local generation of marine aerosol. In 2015 an episode of smoke advection was observed in both fjords causing an increase in the mean black carbon concentration from 7–12 ng m−3 to about 60 ng m−3, and an aerosol scattering coefficient at 550 nm from 2–4 Mm−1 to 12–17 Mm−1. Moreover, under certain conditions statistically significant gradients in aerosol optical properties were observed along the fjord axis reflecting an impact of mountains surrounding the fjords.
16

Quantitative microbiological survey in Hornsund, SW Spitsbergen. Reconaissance study in summer 1985

63%
Zajaczkowska B., Zajaczkowski M.
Bulletin of the Polish Academy of Sciences. Biological Sciences
|
1989
|
tom 37
|
nr 4-6
17
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Principal component and cluster analysis for determining diversification of bottom morphology based on bathymetric profiles from Brepollen (Hornsund, Spitsbergen)

63%
Moskalik T., Tegowski J., Grabowiecki P., Zulichowska M.
Oceanologia
|
2014
|
tom 56
|
nr 1
18

Organic compounds in rainfall at Hornsund, SW Spitsbergen: qualitative results

63%
Krawczyk W. E., Skret U.
Polish Polar Research
|
2005
|
tom 26
|
nr 1
65-76
Research on the chemistry of atmospheric precipitation in the Hornsund region of Svalbard has been extended by analysis of the organic contents. In rainfall samples collected in September 2003, the organics were separated by solid phase extraction (SPE), eluted and analysed on gas chromatograph coupled to a mass selective detector (GC/MS). Rainfall pH was in the range 4.72-5.45, the low values suggesting possible pollution. Concentrations of inorganic ions, expressed as total dissolved salts (TDS), were 5.40-13.18 mg L-1. Non-sea-salt (nss) sulphates were in the range 5-11 µeq L-1. In all samples, long-chain alkanes with chain length up to C36, and their methyl derivatives were detected. Among aromatic compounds biphenyl, dibenzofuran and its methyl derivatives were found. Polycyclic aromatic hydrocarbons (PAHs) were represented by naphthalene, phenanthrene, fluorene, acenaphthene, fluoranthene and pyrene. There were no PAHs with higher numbers of rings. The synoptic meteorological conditions in September 2003 indicate that all organic and inorganic pollutants were of local origin.
19

Preliminary osteological studies on the Arctic charr, Salvelinus alpinus [L., 1758] from the Hornsund region [Spitsbergen]

63%
Sobocinski A., Radziun K.
Acta Ichthyologica et Piscatoria. Supplementum
|
1993
|
tom 23
37-46
20

Parasitic fauna of Arctic charr, Salvelinus alpinus [L., 1758] from the Hornsund region [Spitsbergen]

63%
Sobecka E., Piasecki W.
Acta Ichthyologica et Piscatoria. Supplementum
|
1993
|
tom 23
99-106
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