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  1. 24 Polish Polar Research

  2. 8 Oceanologia

  3. 5 Acta Palaeontologica Polonica

  4. 4 Quaestiones Geographicae

  5. 2 Fragmenta Floristica et Geobotanica

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  1. 5 Zajaczkowski M.

  2. 4 Rachlewicz G.

  3. 4 Szczucinski W.

  4. 3 Ewertowski M.

  5. 3 Krajewski K. P.

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  1. 1 2022

  2. 1 2020

  3. 1 2018

  4. 3 2017

  5. 1 2016

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1
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Punk’s not dead, even at the Czech Arctic Scientific Station in Svalbard

100%
Lycka Z., Elster J.
Oceanologia
|
2020
|
tom 62
|
nr 4PB
2
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

Wind wave climate of West Spitsbergen: seasonal variability and extreme events

86%
Wojtysiak K., Herman A., Moskalik M.
Oceanologia
|
2018
|
tom 60
|
nr 3
3
Artykuł dostępny w postaci pełnego tekstu - kliknij by otworzyć plik
Content available

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

86%
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.
4

Papposphaera heldalii sp. nov. (Haptophyta, Papposphaeraceae) from Svalbard

86%
Thomsen H. A., Egge J. K.
Acta Protozoologica
|
2016
|
tom 55
|
nr 1
5

Selected methods in mass balance estimation of Waldemar Glacier, Spitsbergen

86%
Sobota I.
Polish Polar Research
|
2007
|
tom 28
|
nr 4
249-268
Traditional mass balance measurements by stake readings and snow surveying have been conducted annually since 1996 on the Waldemar Glacier (= Waldemarbreen) in northwest Spitsbergen, Svalbard. Several indirect methods were also used for estimating its mass balance. These methods were divided into two major groups: climatological and geodetic. A comparison of the latest map (2000) with that of 1978 and climatological records enable us to calculate the change in the mass balance of Waldemarbreen over 34 years. These methods include air temperature and degree-day (PDD) models. The average mass balance of Waldemarbreen, computed by climatological methods, was -0.42 m a-1 of water equivalent (w.e.) for the period 1970-2004, and -0.51 m w.e. for 1996-2004. These balances were compared with the glaciological balance for the period 1996-2004, -0.53 m w.e.. The mass balance was also computed using geodetic method, giving -0.52 m of w.e. from 1978 to 2000. It is suggested that, from these results, the approach used for Waldemarbreen might be also useful for estimation the mass balances of other small Svalbard glaciers which terminate on land.
6

Benthic Harpacticoida [Crustacea, Copepoda] from the Svalbard archipelago

86%
Kotwicki L.
Polish Polar Research
|
2002
|
tom 23
|
nr 2
185-191
7

Shallow sublittoral macrozoobenthos in Kongsfjord, West Spitsbergen, Svalbard

86%
Kaczmarek H., Wlodarska-Kowalczuk M., Legezynska J., Zajaczkowski M.
Polish Polar Research
|
2005
|
tom 26
|
nr 2
137-155
The shallow water benthic fauna was collected in Kongsfjord, West Spitsbergen. Sampling was conducted along two main environmental gradients: vertical gradient (depth 5-50 m) and horizontal gradient (sedimentation regime) along the fjord axis. A small rectangular dredge was used. Altogether 169 taxa were identified and four macrofaunal associations were distinguished. Bottom type and distance from the tidal glaciers seem to be the main factors responsible for species distribution. The Soft Bottom I Association occupying the fine mud of the Kongsbreen glacial bay consisted mostly of Crustacea with high dominance of scavenging amphipod Onisimus caricus. Bivalves prevailed in the Soft Bottom II Association, located further away from the main glacier outflows. The barren rocky shelf, deprived of vegetation by a sea urchin Strongylocentrotus droebachiensis was inhabited by the Rocky Shelf Association dominated by decapods. The last distinguished association (the Kelp Association) occurred on the hard bottom overgrown with macroalgae. The gastropod Margarites helicinus and amphipods Ischyrocerus spp. made up 60% of the individuals collected there.
8

Amblystegium boreale [Musci, Amblystegiaceae], a forgotten moss from Svalbard

86%
Ochyra R.
Fragmenta Floristica et Geobotanica
|
1995
|
tom 40
|
nr 2
9

Paracrenhydrosoma oceaniae sp.nov. [Copepoda: Harpacticoida], from Kongsfjorden, Northwest Svalbard [Arctic]

86%
Kotwicki L., Fiers F.
Annales Zoologici
|
2005
|
tom 55
|
nr 3
Both sexes of a new species of Cletodidae belonging to the Acrenhydrosomalineage are described from material collected at Kongsfjorden (Svalbard) and attributed to the genus Paracrenhydrosoma Gee, 1999. Paracrenhydrosoma oceaniae sp. nov. is easily distinguished from its congeners by the reduced setal formula of the natatorial legs, lacking the inner subdistal seta on segment 3 of legs 3 and 4. Several other characteristics viz. antennular and antennal armature, and the free leg 5 exopodite in both sexes, are indications of its basal position in the genus.
10

Soil contamination in high Arctic areas of human impact, Central Spitsbergen, Svalbard

86%
Gulinska J., Rachlewicz G., Szczucinski W., Baralkiewicz D., Kozka M., Bulska E., Burzyk M.
Polish Journal of Environmental Studies
|
2003
|
tom 12
|
nr 6
Thirty-one metals and fifteen PAHs were examined in soils of central Spitsbergen, high Arctic. One of the world's northernmost human settlements and natural tundra were sampled to estimate the local human impact and its range. The contamination caused by local sources is significant only in the closest vicinity, and is usually at least an order of magnitude lower than European limits. The metal concentrations are closely related to bedrock geology and they are at similar levels as elsewhere in Svalbard. The long-dis­tance transport of contaminants was not found at a significant level.
11

The near-surface ice thermal structure of the Waldemarbreen, Svalbard

72%
Sobota I.
Polish Polar Research
|
2009
|
tom 30
|
nr 4
317-338
12

The level of infection with gastro-intestinal nematodes in Svalbard reindeers from Hornsund area, Spitsbergen

72%
Popiolek M., Szczesna J., Kotusz J., Kusznierz J., Witkowski A.
Polish Polar Research
|
2007
|
tom 28
|
nr 4
277-282
Eighty five faecal samples of the Svalbard reindeer inhabiting the coastal terrace of the northern side of Hornsund were collected in July 2005 and analyzed coprologically. The standard flotation method revealed a 97.6% prevalence of infection at an average intensity of 20 eggs in a single subsample. The quantitative, modified McMaster method helped to estimate the mean number of eggs in a gram of faeces (EPG) at 134.7. In the studied sampleseggs of nematodes representing two species, i.e. Ostertagia gruehneri (97.6%, on average 20 eggs in a sample) and Marshallagia marshalli (2.3%, single eggs), were identified.
13

Monothalamous foraminifera from West Spitsbergen fjords, Svalbard: a brief overview

72%
Majewski W., Pawlowski J., Zajaczkowski M.
Polish Polar Research
|
2005
|
tom 26
|
nr 4
269-285
During the 2004 summer season, 14 sediment samples were collected in Kongs- fjorden and Isfjorden, West Spitsbergen, from 6 down to 345 m water-depth (mwd). The samples yielded abundant assemblage of monothalamous foraminifera, belonging to almost 40 morphotypes. Our qualitative (>125µm) and quantitative data (125-500µm) allowed to distinguish three water-depth related assemblages in both Kongsfjorden and Adventfjorden (branch of Isfjorden), indicating that soft-walled monothalamous foraminifera show similar habitat gradation along fjord axis as calcareous and robust agglutinated taxa. Among the monothalamous foraminifera, the subtidal assemblage (6 mwd) was dominated by various unidentified allogromiids. The second, shallow-water assemblage (44-110 mwd) was dominated by Psammophaga sp. 1-3, Hippocrepinella crassa, Hippocrepinella cf. hirudinea, and large Gloiogullmia sp. 2. The deep-water (150-345 mwd) monothalamous assemblage was dominated by Psammophaga sp. 4, pear-shaped Hippocrepina sp., Hippocrepina indivisa, and long Cylindrogullmia sp. 2, as well as large agglutinated species Hyperammina subnodosa with attached Tholosina bulla, Hyperammina fragilis and Lagenammina sp.
14

Differences in taxonomic composition of summer phytoplankton in two fjords of West Spitsbergen, Svalbard

72%
Wiktor J., Wojciechowska K.
Polish Polar Research
|
2005
|
tom 26
|
nr 4
259-268
Fjords of West Spitsbergen are very dynamic in terms of hydrology. Here we tested whether the qualitative analysis of the taxonomic composition of phytoplankton may be useful as a fast method to assess the origin of the waters and whether it can give any additional information to hydrological data. Phytoplankton samples were collected along transects in Hornsund and Kongsfjord. Among total of 109 taxa identified, only 49 were common in both fjords. The assemblages in Hornsund implied that inflow of the cold waters of the Sørkapp Current had occurred some time before samples collection, while in Kongsfjord the taxonomic composition was typical for the summer and did not show any recent, unusual hydrological phenomenon. Concluding, the method can be useful in the surveys in which hydrological data are collected infrequently.
15

Foraminifers from the Treskelodden Formation [Carboniferous-Permian] of south Spitsbergen

72%
Blazejowski B.
Polish Polar Research
|
2009
|
tom 30
|
nr 3
193-230
16

Changes of Arctic landscape due to human impact, north part of Billefjorden area, Svalbard

72%
Tomczyk A. M., Ewertowski M.
Quaestiones Geographicae
|
2010
|
tom 29
|
nr 1
17

Tidewater glaciers of Svalbard: Recent changes and estimates of calving fluxes

72%
Blaszczyk M., Jania J. A., Hagen J. O.
Polish Polar Research
|
2009
|
tom 30
|
nr 2
85-142
18

Paraglacial modifications of glacial sediments over millennial to decadal time-scales in the high Arctic (Billefjorden, central Spitsbergen, Svalbard)

72%
Rachlewicz G.
Quaestiones Geographicae
|
2010
|
tom 29
|
nr 3
19

Depositional processes within the frontal ice-cored moraine system, Ragnar glacier, Svalbard

72%
Ewertowski M., Kasprzak L., Szuman I., Tomczyk A. M.
Quaestiones Geographicae
|
2010
|
tom 29
|
nr 1
20

Application of DC resistivity soundings and geomorphological surveys in studies of modern Arctic glacier marginal zones, Petuniabukta, Spitsbergen

72%
Gibas J., Rachlewicz G., Szczucinski W.
Polish Polar Research
|
2005
|
tom 26
|
nr 4
239-258
C resistivity soundings and geomorphological surveys have been carried out in the marginal zones and adjacent outwash plains of two glaciers in central Spitsbergen, Norwegian Arctic: Ebbabreen and Horbyebreen. The study has revealed complex relationships between landforms, buried glacier ice and permafrost. From this work it is possible to distinguish between moraine ridges which are ice-cored and those which are not. The latter occur in areas which have possibly been affected by glacier surge. The active layer thickness was found to be 0.4 to 2.5 m for diamicton deposits (moraines) and 0.3 to 1.6 m in outwash glacifluvial sediments. The sediment infill thickness in valleys was determined to be as much as 20 m, thereby demonstrating that sandurs have important role in sediment storage in a glacial system. Typical resistivity values for sediment types in both the active layer and in permafrost were also determined.
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