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Polish Polar Research

Polish Polar Research

Description

The quarterly Polish Polar Research edited by the Committee on Polar Research of the Polish Academy of Sciences is an international journal publishing original research articles presenting the results of studies carried out in polar regions.

All papers are peer-reviewed and published in English.

The Editorial Advisory Board includes renowned scientist from Poland and from abroad.

Polish Polar Research is indexed in Science Citation Index Expanded, Journal Citation Reports/Science Edition, Biological Abstracts, BIOSIS Previews, Cold Regions Bibliography, Antarctic Literature, Geological Abstracts, Polish Scientific Journals Contents - Agricultural and Biological Sciences, Quarterly Review, and Zoological Record.


Journal Metrics:
Impact Factor 2022: 1.3
CiteScore metrics from Scopus 2022: 2.4
SCImago Journal Rank (SJR) 2022: 0.288
Source Normalized Impact per Paper (SNIP) 2022: 0.512



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Polish Polar Research is an open-access journal in which archive issues are freely accessible and articles are published at no cost to authors.

ISSN
ISSN 0138-0338, eISSN 2081-8262
Publishers
Polish Academy of Sciences, Committee on Polar Research


Editorial Advisory Board


Robert BIALIK (Warszawa, Poland)

Magda BŁAŻEWICZ (Łódź, Poland)

Alistair CRAME (Cambridge, UK)

Josef ELSTER (České Budějovice, Czechia)

Jacek JANIA (Sosnowiec, Poland)

Cezary KABAŁA (Wrocław, Poland)

Jerónimo LÓPEZ-MARTINEZ (Madrid, Spain)

Krzysztof MIGAŁA (Wrocław, Poland)

Jerzy NAWROCKI (Warszawa, Poland)

Maria OLECH (Kraków, Poland)

Sergej OLENIN (Klaipeda, Litva)

Sandra PASSCHIER (Montclair, USA)

Jan PAWŁOWSKI (Sopot, Poland)

Żaneta POLKOWSKA (Gdańsk, Poland)

Gerhard SCHMIEDL (Hamburg, Germany)

Peter SCHWEITZER (Vienna, Austria)

Janne SOREIDE (UNIS, Svalbard)

Lech STEMPNIEWICZ (Gdańsk, Poland)

Mateusz STRZELECKI (Wrocław, Poland)

Witold SZCZUCIŃSKI (Poznań, Poland)

Slawek TULACZYK (Santa Cruz, USA)

Jan Marcin WĘSŁAWSKI (Sopot, Poland) - President

Editor-in-Chief

Wojciech MAJEWSKI (Geosciences), Institute of Paleobiology PAS, Poland

e-mail: wmaj@twarda.pan.pl


Co-Editors:

Monika KĘDRA (Life Sciences), Institute of Oceanology PAS, Poland
e-mail: kedra@iopan.gda.pl


Michał ŁUSZCZUK (Social Science and Humanities), UMCS, Poland
e-mail: michal.luszczuk@poczta.umcs.lublin.pl


Associate Editors

Piotr JADWISZCZAK (Białystok),

e-mail: piotrj@uwb.edu.pl


Ewa ŁUPIKASZA (Sosnowiec)

e-mail: ewa.lupikasza@us.edu.pl


Krzysztof ZAWIERUCHA (Poznań)

email: k.p.zawierucha@gmail.com


Editorial Advisory Board

Robert BIALIK (Warszawa, Poland)

Magda BŁAŻEWICZ (Łódź, Poland)

Alistair CRAME (Cambridge, UK)

Josef ELSTER (České Budějovice, Czechia)

Jacek JANIA (Sosnowiec, Poland)

Cezary KABAŁA (Wrocław, Poland)

Jerónimo LÓPEZ-MARTINEZ (Madrid, Spain)

Krzysztof MIGAŁA (Wrocław, Poland)

Jerzy NAWROCKI (Warszawa, Poland)

Maria OLECH (Kraków, Poland)

Sergej OLENIN (Klaipeda, Litva)

Sandra PASSCHIER (Montclair, USA)

Jan PAWŁOWSKI (Sopot, Poland)

Żaneta POLKOWSKA (Gdańsk, Poland)

Gerhard SCHMIEDL (Hamburg, Germany)

Peter SCHWEITZER (Vienna, Austria)

Janne SOREIDE (UNIS, Svalbard)

Lech STEMPNIEWICZ (Gdańsk, Poland)

Mateusz STRZELECKI (Wrocław, Poland)

Witold SZCZUCIŃSKI (Poznań, Poland)

Slawek TULACZYK (Santa Cruz, USA)

Jan Marcin WĘSŁAWSKI (Sopot, Poland) - President

Geosciences
Wojciech MAJEWSKI
e-mail: wmaj@twarda.pan.pl
phone: (48 22) 697 88 53

Instytut Paleobiologii PAN
ul. Twarda 51/55
00-818 Warszawa, POLAND



Life Sciences
Monika KĘDRA
e-mail: kedra@iopan.gda.pl
phone: (48 58) 731 17 79

Instytut Oceanologii PAN
Powstańców Warszawy 55
81-712 Sopot, POLAND, P.O. Box 148


Social Science and Hummanities
Michał ŁUSZCZUK
e-mail: michal.luszczuk@poczta.umcs.lublin.pl
phone: (48 81) 537 68 99

Instytut Geografii Społeczno-Ekonomicznej i Gospodarki Przestrzennej UMCS
Al. Kraśnicka 2D
20-718 Lublin, POLAND
Polish Polar Research is an open access journal with all content available with no charge in full text version.


The journal content is available under the Creative Commons Attribution 4.0 International License ( http://creativecommons.org/licenses/by/4.0/).

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Content

Polish Polar Research | 2016 | vol. 37 | No 2

1 Landscape transformation under the Gåsbreen glacier recession since 1899, southwestern Spitsbergen
Krzysztof Ostafin , Wiesław Ziaja , Justyna Dudek
Polish Polar Research | 2016 | vol. 37 | No 2 | 155-172 | DOI: 10.1515/popore-2016-0010
Keywords: Arctic climate warming Glacier recession Landscape transformation Svalbard
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Abstract

Landscape changes of the Gåsbreen glacier and its vicinity since 1899 are described. Maps at 1:50 000 scale of changes of the glacier's elevation and extent for the periods 1938-1961, 1961-1990, 1990-2010, and 1938-2010 are analyzed in comparison with results of the authors' field work in the summer seasons 1983, 1984, 2000, 2005 and 2008. During all the 20th century, the progressive recession of the glacier revealed in a dramatic decrease in the thickness of its lower part, with a small reduction of its area and length. However, further shrinkage produced significant shortening and reduction in area which resulted in final decline of the Goësvatnet glacial dammed lake in 2002. Hence, the lowest (and very thick, up to 150-160 m) part of the former glacier tongue and dammed lake were transformed into a new terraced river valley south of the glacier and a typical marginal zone with glacial landforms north of the glacier. Since 1961, the equilibrium line altitude of the Gåsbreen glacier has risen from ca 350 to ca 500 m a.s.l. and now is located below the very steep rocky walls of the Mehesten mountain ridge, 1378 m a.s.l. Hence, the glacier is being fed by snow avalanches from these rocky walls and much more snow melts during the warmer summer seasons, stimulating a quicker recession of the lowest part of the glacier. This recession may be stopped only by significant climate cooling or increase in snow.
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Authors and Affiliations

Krzysztof Ostafin
Wiesław Ziaja
Justyna Dudek
2 Warming and drying of tundra and glacier summer climate in NW Spitsbergen from 1975 to 2014
Rajmund Przybylak , Andrzej Araźny
Polish Polar Research | 2016 | vol. 37 | No 2 | 173-192 | DOI: 10.1515/popore-2016-0011
Keywords: air temperature Arctic Kaffiøyra precipitation Svalbard Waldemar Glacier
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Abstract

Temperature and precipitation conditions in the Kaffiøyra region in the summer season (21 July-31 August) for the period from 1975-2014 are described based on data collected during 22 expeditions, in which meteorological measurements were carried out, and complete data series combining both original and reconstructed data. The latter ones were obtained using data from the Ny Ålesund meteorological station, which are strongly correlated with data from the Kaffiøyra region. Seasonal statistics presented for temperature and precipitation based on these two sets of data reveal only slight changes. Summer temperatures in the Kaffiøyra region in the studied period (1975-2014) showed statistically significant strong upward trends, while precipitation totals revealed a downward trend, but not statistically significant. In the studied area, based on 40-years of data, it was demonstrated that the near-surface lapse rates of summer air temperature are slightly lower in glaciated (0.58°C/100 m) than in non-glaciated areas (0.67°C/100 m). Anticyclonic/cyclonic circulation types significantly increase/decrease air temperature on the Waldemar Glacier, while their impact on precipitation is markedly smaller. In summer, close correlations were observed between air temperature and such glacier characteristics as the mass balance and the location of the equilibrium line, while precipitation does not have a great influence on them.
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Authors and Affiliations

Rajmund Przybylak
Andrzej Araźny
3 Influence of snowpack internal structure on snow metamorphism and melting intensity on Hansbreen, Svalbard
Michał Laska , Tomasz Budzik , Bartłomiej Luks
Polish Polar Research | 2016 | vol. 37 | No 2 | 193-218 | DOI: 10.1515/popore-2016-0012
Keywords: Arctic glaciology Hornsund Meltwater Snow cover Spitsbergen
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Abstract

This paper presents a detailed study of melting processes conducted on Hansbreen - a tidewater glacier terminating in the Hornsund fjord, Spitsbergen. The fieldwork was carried out from April to July 2010. The study included observations of meltwater distribution within snow profiles in different locations and determination of its penetration time to the glacier ice surface. In addition, the variability of the snow temperature and heat transfer within the snow cover were measured. The main objective concerns the impact of meltwater on the diversity of physical characteristics of the snow cover and its melting dynamics. The obtained results indicate a time delay between the beginning of the melting processes and meltwater reaching the ice surface. The time necessary for meltwater to percolate through the entire snowpack in both, the ablation zone and the equilibrium line zone amounted to c. 12 days, despite a much greater snow depth at the upper site. An elongated retention of meltwater in the lower part of the glacier was caused by a higher amount of icy layers (ice formations and melt-freeze crusts), resulting from winter thaws, which delayed water penetration. For this reason, a reconstruction of rain-on-snow events was carried out. Such results give new insight into the processes of the reactivation of the glacier drainage system and the release of freshwater into the sea after the winter period.
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Authors and Affiliations

Michał Laska
Tomasz Budzik
Bartłomiej Luks
4 Modelling of the thermal regime of permafrost during 1990–2014 in Hornsund, Svalbard
Tomasz Wawrzyniak , Marzena Osuch , Jarosław Napiórkowski , Sebastian Westermann
Polish Polar Research | 2016 | vol. 37 | No 2 | 219-242 | DOI: 10.1515/popore-2016-0013
Keywords: Arctic Hornsund permafrost evolution Permafrost modelling Spitsbergen
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Abstract

The thermal state of permafrost is a crucial indicator of environmental changes occurring in the Arctic. The monitoring of ground temperatures in Svalbard has been carried out in instrumented boreholes, although only few are deeper than 10 m and none are located in southern part of Spitsbergen. Only one of them, Janssonhaugen, located in central part of the island, provides the ground temperature data down to 100 m. Recent studies have proved that significant warming of the ground surface temperatures, observed especially in the last three decades, can be detected not only just few meters below the surface, but reaches much deeper layers. The aim of this paper is evaluation of the permafrost state in the vicinity of the Polish Polar Station in Hornsund using the numerical heat transfer model CryoGrid 2. The model is calibrated with ground temperature data collected from a 2 m deep borehole established in 2013 and then validated with data from the period 1990-2014 from five depths up to 1 m, measured routinely at the Hornsund meteorological station. The study estimates modelled ground thermal profile down to 100 m in depth and presents the evolution of the ground thermal regime in the last 25 years. The simulated subsurface temperature trumpet shows that multiannual variability in that period can reach 25 m in depth. The changes of the ground thermal regime correspond to an increasing trend of air temperatures observed in Hornsund and general warming across Svalbard.
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Authors and Affiliations

Tomasz Wawrzyniak
Marzena Osuch
Jarosław Napiórkowski
Sebastian Westermann
5 New geological interpretation of multi-channel seismic profiles from the Pacific Margin of the Antarctic Peninsula
Jan Okoń , Jerzy Giżejewski , Tomasz Janik
Polish Polar Research | 2016 | vol. 37 | No 2 | 243-268 | DOI: 10.1515/popore-2016-0014
Keywords: Antarctica Bransfield Strait Glacier valleys marine seismic South Shetland Trench Subduction zone Volcanic structure
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Abstract

The Polish Geophysical Expedition to West Antarctica in 1979-1980 was carried out by the Institute of Geophysics, Polish Academy of Sciences. Beside deep seismic soundings, 12 multi-channel seismic profiles, with a total length of ca 1000 km have been recorded north and east of the South Shetland Islands and in the Bransfield Strait, but they have never before been completely interpreted and published. All profiles have been processed with modern processing flow including time migration. Profiles crossing the South Shetland Trench revealed distinct reflector inside continental slope, which has been interpreted as border between buried accretionary prism and overlying slope sediments of glacial-marine origin. Profiles in the Bransfield Strait show traces of the Last Glacial Maximum (LGM) in the form of glacial foreground valleys, with some of them used as weak spots for young age volcanic intrusions. This paper is the first comprehensive geological interpretation of collected dataset and differences between results from other expeditions are discussed.
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Authors and Affiliations

Jan Okoń
ORCID: ORCID
Jerzy Giżejewski
Tomasz Janik
6 Cyanobacterial and algal diversity in the vicinity of two different seabird colonies in Spitsbergen
Mirosława Pietryka , Dorota Richter , Jan Matuła
Polish Polar Research | 2016 | vol. 37 | No 2 | 269-288 | DOI: 10.1515/popore-2016-0015
Keywords: Arctic Cyanobacterial and algal assembalges Influence of seabirds Spitsbergen Trophy
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Abstract

The aim of the study was to compare cyanobacterial and algal assemblages occurring in ornithocoprophilous habitats formed under the influence of two seabird colonies (mixed colony of piscivorous Uria lomvia and Rissa tridactyla and planktivorous Alle alle) nesting on the southwest side of Hornsund (Spitsbergen). Various influences of the bird colonies (e.g. surface trophy, treading) lead to the formation of ornithogenic habitats with quantitatively and qualitatively diverse cyanobacterial and algal assemblages. Only 6 species common to both habitats were identified, but due to their different proportions the similarity ended there. Cyanobacterial and algal assemblages of both ornithogenic habitats also react rather differently to the intensity of the bird colonies' influence. The assemblages located directly beneath piscivorous bird nests were characterized by a larger number of species, which decreased the farther from the colony it was. Cyanobacterial and algal assemblages located directly next to planktivorous bird nests were species poor, but species richness increased at locations farther from their direct influence. The obtained results confirmed that bird colonies characterized by different diet and behavior influenced the formation of two separate, quantitatively and qualitatively different cyanobacterial and algal assemblages. Species such as Eucapsis sp., Gleocapsopsis sp., Gloeothece sp., Woronichinia sp., Hematococcus sp. were characteristic for algae and cyanobacteria assemblages in the vicinity of piscivorous bird colonies, whereas Aphanocapsa sp., Gloeothece sp., Komvophoron minutum, Pseudanabaena sp., Gloeocystis sp. 2 occurred in the vicinity of planktivorous bird colonies.
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Authors and Affiliations

Mirosława Pietryka
Dorota Richter
Jan Matuła
7 Female sporogenesis in the native Antarctic grass Deschampsia antarctica Desv.
Marcin Domaciuk , Irena Giełwanowska , Agata Leszczuk , Ewa Szczuka , Wioleta Kellmann-Sopyła , Justyna Koc
Polish Polar Research | 2016 | vol. 37 | No 2 | 289-302 | DOI: 10.1515/popore-2016-0016
Keywords: Antarctic Callose Deschampsia antarctica Megaspore tetrad Megasporocyte meiosis
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Abstract

The development of megasporocytes and the functional megaspore formation in Deschampsia antarctica were analyzed with the use of microscopic methods. A single archesporial cell was formed directly under the epidermis in the micropylar region of the ovule without producing a parietal cell. In successive stages of development, the meiocyte was transformed into a megaspore tetrad after meiosis. Most megaspores were arranged in a linear fashion, but some tetrads were T-shaped. Only one of the 60 analyzed ovules contained a cell in the direct proximity of the megasporocyte, which could be an aposporous initial. Most of the evaluated D. antarctica ovules featured monosporic embryo sacs of the Polygonum type. Approximately 30% of ovules contained numerous megaspores that were enlarged. The megaspores were located at chalazal and micropylar poles, and some ovules featured two megaspores - terminal and medial - in the chalazal region, or even three megaspores at the chalazal pole. In those cases, the micropylar megaspore was significantly smaller than the remaining megaspores, and it did not have the characteristic features of functional megaspores. Meiocytes and megaspores of D. antarctica contained polysaccharides that were detectable by PAS-reaction and aniline blue staining. Starch granules and cell walls of megasporocytes, megaspores and nucellar cells were PAS-positive. Fluorescent callose deposits were identified in the micropylar end of the megasporocytes. During meiosis and after its completion, thick callose deposits were also visible in the periclinal walls and in a small amount in the anticlinal walls of megaspores forming linear and T-shaped tetrads. Callose deposits fluorescence was not observed in the walls of the nucellar cells.
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Authors and Affiliations

Marcin Domaciuk
Irena Giełwanowska
Agata Leszczuk
Ewa Szczuka
Wioleta Kellmann-Sopyła
Justyna Koc
8 Species composition, seasonal abundance and population structure of chaetognaths in Admiralty Bay (Antarctic)
Luiza Bielecka , Bartłomiej Jerzak , Ilona Złoch
Polish Polar Research | 2016 | vol. 37 | No 2 | 303-324 | DOI: 10.1515/popore-2016-0017
Keywords: Antarctic Body size Chaetognatha population structure Taxa composition
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Abstract

Although chaetognaths inhabiting polar ecosystems are relatively well known, there are few reports on their functioning in the Antarctic coastal plankton community. The presented results provide the first comprehensive description of population structure of chaetognaths in the neritic zone west of the Antarctic Peninsula. The studies were performed on samples collected in Admiralty Bay, from December 1994 to June 1995. Following six chaetognath species were determined: Eukrohnia hamata, E. bathypelagica, E. fowleri, Pseudosagitta gazellae, P. maxima and Solidosagitta marri. The representatives of Eukrohnia were observed almost throughout the research period, whereas those of Pseudosagitta and Solidosagitta were found only during first four months of our investigation. Eukrohnia hamata showed a strong dominance in respect to abundance (max. 445 ind./1000 m3). The mean abundance of all taxa significantly fluctuated in the study period and across weeks. Generally, all species were represented by the first three maturity stages (I-III), individuals stage IV occurred sporadically, and mature specimens (stage V) were not recorded at all. Morphometric analysis of the most abundant species showed distinct differences in their total length and body proportions. Our findings may suggest that chaetognath populations in Admiralty Bay are migrant, dependent on the inflow of water from the Bransfield Strait, but to prove this statement further, round year study is necessary.
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Authors and Affiliations

Luiza Bielecka
Bartłomiej Jerzak
Ilona Złoch
9 Area, depth and elevation of cryoconite holes in the Arctic do not influence Tardigrada densities
Krzysztof Zawierucha , Tobias R. Vonnahme , Miloslav Devetter , Małgorzata Kolicka , Marta Ostrowska , Sebastian Chmielewski , Jakub Z. Kosicki
Polish Polar Research | 2016 | vol. 37 | No 2 | 325-334 | DOI: 10.1515/popore-2016-0009
Keywords: Arctic cryoconite holes ecology Glaciers Svalbard Tardigrada
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Abstract

Water bears (Tardigrada) are known as one of the most extremophile animals in the world. They inhabit environments from the deepest parts of the oceans up to the highest mountains. One of the most extreme and still poorly studied habitats which tardigrades inhabit are cryoconite holes. We analysed the relation between area, depth, elevation and tardigrades densities in cryoconite holes on four glaciers on Spitsbergen. The mean (±SD) of cryoconite area was 1287.21±2400.8 cm2, while the depth was on average 10.8±11.2 cm, the elevation 172.6±109.66 m a.s.l., and tardigrade density 24.9±33.0 individuals per gram of wet material (n = 38). The densities of tardigrades on Hans Glacier reached values of up to 168 ind. cm3, 104 ind. g-1 wet weight, and 275 ind. g-1 dry weight. The densities of tardigrades of the three glaciers in Billefjorden were up to 82 ind. cm2, 326 ind. g-1 wet weight and 624 ind. g-1 dry weight. Surprisingly, although the model included area, depth and elevation as independent variables, it cannot explain Tardigrada density in cryoconite holes. We propose that due to the rapid melting of the glacier surface in the Arctic, the constant flushing of cryoconite sediments, and inter-hole water-sediment mixing, the functioning of these ecosystems is disrupted. We conclude that cryoconite holes are dynamic ecosystems for microinvertebrates in the Arctic.
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Authors and Affiliations

Krzysztof Zawierucha
Tobias R. Vonnahme
Miloslav Devetter
Małgorzata Kolicka
Marta Ostrowska
Sebastian Chmielewski
Jakub Z. Kosicki

Instructions for authors


The quarterly Polish Polar Research invites original scientific papers dealing with all aspects of polar research. The journal aims to provide a forum for publication of high-quality research papers, which are of international interest.

We warmly welcome review papers and proposals for thematic Special Issues.

Articles must be written in English. Authors are requested to have their manuscript read by a person fluent in English before submission. They should not be longer than 30 typescript pages, including tables, figures and references. However, upon request, longer manuscripts may be considered for publication. All papers are peer-reviewed. With a submitted manuscript, authors should provide e-mail addresses of at least three suggested reviewers.


Submission of the manuscript should be supported with a declaration that the work described has not been published previously nor is under consideration by another journal.

For text submission, Word file format is preferred. Please use the PPRes style template when preparing the final version of your paper. Pay special attention to writing correctly the list of references with doi. Manuscripts which are not prepared in line with the template will be returned to the authors. Please submit your manuscripts using our online submission system.

The journal does not have article processing charges (APCs) nor article submission charges. No honorarium will be paid to authors for publishing papers.





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