Science and earth science

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 2021: 0.900
CiteScore metrics from Scopus 2021: 2.2
SCImago Journal Rank (SJR) 2021: 0.323
Source Normalized Impact per Paper (SNIP) 2021: 0.58

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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

Angelika BRANDT (Hamburg),

Claude DE BROYER (Bruxelles),

Peter CONVEY (Cambridge, UK),

J. Alistair CRAME (Cambridge, UK),

Rodney M. FELDMANN (Kent, OH),

Jane E. FRANCIS (Cambridge, UK),

Andrzej GAŹDZICKI (Warszawa)

Aleksander GUTERCH (Warszawa),

Jacek JANIA (Sosnowiec),

Jiří KOMÁREK (Třeboň),

Wiesława KRAWCZYK (Sosnowiec),

German L. LEITCHENKOV (Sankt Petersburg),

Jerónimo LÓPEZ-MARTINEZ (Madrid),

Sergio A. MARENSSI (Buenos Aires),

Jerzy NAWROCKI (Warszawa),

Ryszard OCHYRA (Kraków),

Maria OLECH (Kraków)

Sandra PASSCHIER (Montclair, NJ),

Jan PAWŁOWSKI (Genève),

Gerhard SCHMIEDL (Hamburg),

Jacek SICIŃSKI (Łódź),

Michael STODDART (Hobart),

Witold SZCZUCIŃSKI (Poznań),

Andrzej TATUR (Warszawa),

Wim VADER (Tromsø),

Tony R. WALKER (Halifax, Nova Scotia),

Jan Marcin WĘSŁAWSKI (Sopot) - 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

Editorial Advisory Board

Angelika BRANDT (Hamburg),

Claude DE BROYER (Bruxelles),

Peter CONVEY (Cambridge, UK),

J. Alistair CRAME (Cambridge, UK),

Rodney M. FELDMANN (Kent, OH),

Jane E. FRANCIS (Cambridge, UK),

Andrzej GAŹDZICKI (Warszawa)

Aleksander GUTERCH (Warszawa),

Jacek JANIA (Sosnowiec),

Jiří KOMÁREK (Třeboň),

Wiesława KRAWCZYK (Sosnowiec),

German L. LEITCHENKOV (Sankt Petersburg),

Jerónimo LÓPEZ-MARTINEZ (Madrid),

Sergio A. MARENSSI (Buenos Aires),

Jerzy NAWROCKI (Warszawa),

Ryszard OCHYRA (Kraków),

Maria OLECH (Kraków)

Sandra PASSCHIER (Montclair, NJ),

Jan PAWŁOWSKI (Genève),

Gerhard SCHMIEDL (Hamburg),

Jacek SICIŃSKI (Łódź),

Michael STODDART (Hobart),

Witold SZCZUCIŃSKI (Poznań),

Andrzej TATUR (Warszawa),

Wim VADER (Tromsø),

Tony R. WALKER (Halifax, Nova Scotia),

Jan Marcin WĘSŁAWSKI (Sopot) - 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 | Accepted article - Special Issue: Processes controlling the development of periglacial and paraglacial landscapes in rapidly changing polar regions – 50th anniversary of the Stanislaw Baranowski Polar Station of the University of Wroclaw. Guest Editors: Matt C. Strzelecki, Marek Kasprzak, Piotr Owczarek and Łukasz Stachnik

1 Energy mass balance and temperature-index melt modelling of Werenskioldbreen, Svalbard

Dariusz Ignatiuk

Polish Polar Research | Accepted article - Special Issue: Processes controlling the development of periglacial and paraglacial landscapes in rapidly changing polar regions – 50th anniversary of the Stanislaw Baranowski Polar Station of the University of Wroclaw. Guest Editors: Matt C. Strzelecki, Marek Kasprzak, Piotr Owczarek and Łukasz Stachnik

Keywords: Arctic Spitsbergen degree-day factor melt modelling glacier mass balance

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Abstract

Studying the reaction of glaciers to climate warming and the interactions of ice masses with the atmosphere is cognitively highly significant and contributes to understanding the climate change. The results from the modelling of glacier surface ablation by the temperature–index and energy balance models as well as the results of meteorological and glaciological studies on Werenskioldbreen (south Spitsbergen, Svalbard) in 2011 have been analysed to improve the understanding of the glacier system’s functioning in the High Arctic. The energy balance modelling results showed that the radiation balance (58%) and sensible heat (42%) are the main factors influencing surface ablation on the glacier. The energy balance model offers a better fit to the measured ablation than the temperature–index model. These models have to be validated and calibrated with data from automatic weather stations, which provide the relevant gradient and calibration and validation. Presented models are highly suited for calculating ablation in Svalbard and other areas of the Arctic.

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Authors and Affiliations

Dariusz Ignatiuk

e-mail:

ORCID:

University of Silesia in Katowice, Bankowa 12, 40-007 Katowice, Poland

2 The origin of pine pollen grains captured from air at Calypsobyen, Svalbard

Małgorzata Jędryczka , Beata Żuraw , Piotr Zagórski , Jan Rodzik , Karolina Mędrek , Irena Agnieszka Pidek , Weronika Haratym , Joanna Kaczmarek , Magdalena Sadyś

Keywords: Arctic Spitsbergen pollen dispersal Pinus spp. long distance transport

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Abstract

Spitsbergen is the largest island in the Svalbard Archipelago (Norway) that has been permanently populated. The harsh Arctic climate prevents development of large vascular plants such as trees. A two-year aerobiological survey was conducted within the framework of two consecutive polar expeditions (2014 and 2015) in Spitsbergen (Calypsobyen, Bellsund). The air quality was measured continuously from June/July to August using a 7-day volumetric air sampler, Tauber trap and moss specimens. Collected air samples and gravimetric pollen deposits were processed following transfer to sterile laboratory conditions and analyzed with the aid of light microscopy. Days when pine pollen grains were detected in the air were selected for further analysis. Clusters of back-trajectories, computed using the Hybrid Single Particle Lagrangian Integrated Trajectory model in combination with ArcGIS software as well as the Flextra trajectory model, showed the movement of air masses to the sampling location at Hornsund, and thus indicated the likely origin of pollen grains. The GlobCover 2009 and CORINE Land Cover 2012 datasets were employed to establish the distribution of coniferous forests in the areas of interest. Conclusions were drawn based on the analyses of the circulation of air masses, using visualization of global weather conditions forecast to supercomputers. For the first time we have demonstrated that pine pollen grains occurring in pine-free Spitsbergen, could originate from numerous locations, including Scandinavia, Iceland, Siberia and northern Canada. Pollen grains were transported via air masses for distances exceeding ~2000 km. Both air samples and gravimetric pollen deposits revealed the same pattern of Pinus pollen distribution.

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Authors and Affiliations

Małgorzata Jędryczka

e-mail:

ORCID:

Beata Żuraw

e-mail:

ORCID:

Piotr Zagórski

Jan Rodzik

Karolina Mędrek

Irena Agnieszka Pidek

e-mail:

ORCID:

Weronika Haratym

e-mail:

ORCID:

Joanna Kaczmarek

e-mail:

ORCID:

Magdalena Sadyś

e-mail:

ORCID:

Institute of Plant Genetics, Polish Academy of Science, Strzeszyńska 34, 60-479 Poznań, Poland
Department of Hydrobiology and Protection of Ecosystems, University of Life Sciences in Lublin, Dobrzańskiego 37, 20-295 Lublin, Poland
Institute of Earth and Environmental Sciences, Maria Curie-Skłodowska University, al. Kraśnicka 2D, 20-718 Lublin, Poland
Paderewski Private Grammar School, Symfoniczna 1, 20-853 Lublin, Poland
Rothamsted Research, West Common, Harpenden, AL5 2JQ, UK

3 Forming of water chemistry in active layer, Steinvik River catchment, SW Spitsbergen

Michał Rysiukiewicz , Henryk Marszałek , Mirosław Wąsik

Keywords: Arctic Svalbard river catchment shallow groundwater chemical composition

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Abstract

The objective of this work is to demonstrate for the first time the results of hydrogeochmical studies carried out in the Steinvik River catchment, in order to provide detailed information regarding the chemical composition of groundwater in the Hornsund region, SW Spitsbergen. The water chemistry in the non-glaciated Steinvik River catchment is largely controlled by hydrological processes related to thaw of the near surface permafrost. Groundwater runoff is generated from the fast flow through well-permeable active layer. Recharge from melting snow, permafrost and rain, together with short residence time of groundwater, favors the forming of low-mineralized water, reaching 41 and 50 μS/cm for surface and groundwater, respectively, with the dominance of HCO3−, Cl−, Mg2+, Ca2+ and Na+ ions. In some water samples, increased concentrations of aluminum (up to 268 μg/L ) were found. The highest concentrations of phosphate, nitrite and ammonium in water seem to be related to the presence of bird colonies. Groundwater of active layer in the studied catchment belongs to young meteoric water with the age limited to one summer season.

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Authors and Affiliations

Michał Rysiukiewicz

e-mail:

ORCID:

Henryk Marszałek

e-mail:

ORCID:

Mirosław Wąsik

e-mail:

ORCID:

Department of Applied Hydrogeology, Institute of Geological Sciences, Wrocław University, Pl. Maksa Borna 9, 50-204 Wrocław, Poland

4 Permeability of active layer sediments and groundwater runoff in Brattegg River catchment, SW Spitsbergen

Mirosław Wąsik , Henryk Marszałek , Michał Rysiukiewicz

Keywords: Arctic Svalbard active layer aquifer groundwater runoff

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Abstract

This paper presents the permeability of the permafrost active layer determined in the Brattegg River catchment (SW Spitsbergen) for the 6-years interval of 2005–2010. The field permeability measurements technique of weathered rocks on various geomorphological forms allows to assess the value of their hydraulic conductivity ( k). High variability of k values, ranging from 6.37 10 ⁻⁹ to 4.0 10 ⁻³ m s ⁻¹, indicates the permeability of rocks from very low in clay to very high in gravel-rock rubble. Among the geomorphological forms, the best permeability was observed in boulder covers and rock debris, and the lowest one in patterned ground. The obtained results were used to determine the groundwater runoff ( q), assuming the unit thickness of the active layer aquifer. The q value from the Brattegg River catchment was calculated at 130 L s−1, which is from 15% to 47% of the average surface runoff.

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Authors and Affiliations

Mirosław Wąsik

e-mail:

ORCID:

Henryk Marszałek

e-mail:

ORCID:

Michał Rysiukiewicz

e-mail:

ORCID:

Institute of Geological Sciences, Department of Applied Hydrogeology, Wrocław University, Plac M. Borna 9, 50-204 Wrocław, Poland

5 Climate indices of environmental change in the High Arctic: Study from Hornsund, SW Spitsbergen, 1979–2019

Krzysztof Migała , Elżbieta Łepkowska , Marzena Osuch , Łukasz Stachnik , Tomasz Wawrzyniak , Dariusz Ignatiuk , Piotr Owczarek

Keywords: Arctic Svalbard climate change climate variables polar region

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Abstract

An analysis of a suite of climatological indices was undertaken on the basis of long-term (1979–2019) climatological data from the Polish Polar Station in Hornsund, SW Spitsbergen. It was followed by an attempt to assess the scale of their impact on the local environment. The temperature and precipitation indices were based on percentiles of the variables calculated for a population of daily values from the climate normals for 1981–2010. A greater share of both cyclonic and anticyclonic circulations from the S and SW sectors, forcing the advection of warm air masses from the south, was decisive for the trends of change in comparison with the long-term mean. Both extreme precipitation and drought events depend on the 500 hPa geopotential height and precipitable water anomalies, determined by the baric field over the North Atlantic. Climate changes impact on the dynamics of local geoecosystems by causing faster glacier ablation and retreat, permafrost degradation, intensification of the hydrological cycle in glaciated and unglaciated catchments, and changes in the condition and growth of tundra vegetation.

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Authors and Affiliations

Krzysztof Migała

e-mail:

ORCID:

Elżbieta Łepkowska

e-mail:

ORCID:

Marzena Osuch

e-mail:

ORCID:

Łukasz Stachnik

e-mail:

ORCID:

Tomasz Wawrzyniak

e-mail:

ORCID:

Dariusz Ignatiuk

e-mail:

ORCID:

Piotr Owczarek

e-mail:

ORCID:

Institute of Geography and Regional Development, University of Wroclaw, Plac Uniwersytecki 1, 50-137 Wroclaw, Poland
Institute of Earth Sciences, Faculty of Natural Sciences, University of Silesia in Katowice, ul. Będzińska 60, 41-200 Sosnowiec, Poland
Institute of Geophysics, Polish Academy of Sciences, ul. Księcia Janusza 6 , 01-452 Warszawa, Poland

6 Can topographic features of debris cones (SW Spitsbergen) be geoindicators of environmental changes?

Agnieszka Latocha-Wites , Krzysztof Parzóch

Keywords: Arctic Svalbard slope morphology geomorphic processes debris flow

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Abstract

Evidence of recent geomorphic processes within debris cones, their spatial distribution and diversification on cones surface are interpreted in the context of contemporary slope morphogenesis. The detailed inventory of relief features on debris cones in the SW Spitsbergen revealed their great spatial diversity. It is linked with a dominance of different morphological processes in adjacent areas. Spatial and temporal diversity of process-relief assemblages on cones is strongly related with local factors, like bedrock lithology, slope aspect and inclination, local circulation and climatic conditions. However, the potential role of debris cones and their topographic features as geoindicators archiving information about the environmental impact of global changes, cannot be explicitly estimated. Local constraints obscure the regional expression of any global trends, which could be detected on the basis of process-relief assemblages on debris cones in polar regions.

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Authors and Affiliations

Agnieszka Latocha-Wites

e-mail:

ORCID:

Krzysztof Parzóch

e-mail:

ORCID:

Institute of Geography and Regional Development, University of Wroclaw, Pl. Uniwersytecki 1, 50-137 Wroclaw, Poland

7 Hydrodynamics and hydrogeochemistry of Werenskiold Glacier forefield, SW Spitsbergen

Magdalena Modelska , Sebastian Buczyński

Keywords: Arctic Svalbard groundwater surface water runoff temperature chemical composition

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Abstract

In the 2008 ablation season, subglacial springs discharge, flow rate and profiling of the proglacial river, physical-chemical parameters (pH, temperature, electrical conductivity) and chemical composition (HCO3−, SO42−, Cl−, NO3−, NO2−, PO43−, Ca2+, Mg2+, Na+, K+, Fetot, Mn2+, Al3+, Zn2+, Pb2+ and SiO2) of water in the Werenskiold Glacier forefield were measured. Chemical composition of groundwater as well as water of lakes, the main watercourse, subglacial outflows and water representing direct meltwater recharge were studied to determine their origin, the depth of circulation and recharge systems. The results indicate that the main source of water in the glacial river were the subglacial outflows in the central part of the glacier. They generated 77% of the total amount of water in the glacier forefield. Direct inflow of groundwater from glacier moraine to proglacial river was marginally low and the water circulation system was shallow, fast and variable. There were no evidences for an important role of deeper than suprapermafrost water circulation systems. The water temperature, especially in the lakes, exceeding the mean daily air temperature during the ablation period, is due to the heating of the ground moraine rocks. A clear difference between groundwater chemical composition and surface water as well as subglacial runoff in terms of major ions, together with the homogeneity of chemical composition of the proglacial river from spring to mouth confirmed the marginal role of groundwater runoff in the drainage of the catchment area. It was confirmed that the chemical composition of groundwater and moraine lakes in the glacier forefield was shaped by geological factors, i.e., mainly chemical weathering of sulphides, carbonates and secondary sulphates. The possibility of secondary iron hydroxide precipitation and a high probability of complex aluminosilicate transformations were also demonstrated.

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Authors and Affiliations

Magdalena Modelska

Sebastian Buczyński

University of Wrocław, Institute of Geological Sciences, Plac M. Borna 9, 50-204 Wrocław, Poland

8 Conceptual model for talus slope development in Brattegg Valley (SW Spitsbergen) based on sedimentology of debris deposits in periglacial zone

Krzysztof Senderak

Keywords: Arctic Svalbard slope processes deglaciation sedimentology

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Abstract

The talus slopes occur in all climatic zones on the Earth. These forms are sensitive to climate fluctuations, therefore they may be indicators of changes in the environment and contain the record of the geomorphological events after the deglaciation period. Both in the past and nowadays, slopes in area of the High Arctic have been developing in the specific conditions of periglacial zone. This is caused by simultaneously occurring different processes of weathering and deposition. The article presents the methodological approach and the results of the sedimentological measurements and geomorphological studies of the eight talus cones located in SW Spitsbergen. The study was conducted in the non-glaciated valley near the Stanislaw Baranowski Polar Station in Spitsbergen. The aim of the investigation was to determine the modern mechanisms of material transport on talus slopes and their impact on relief of slope surface in the polar environment. The obtained results and literature data allowed to indicate four separate zones of talus slope environment and develop a conceptual model for talus slope development in the Brattegg Valley, SW Spitsbergen.

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Authors and Affiliations

Krzysztof Senderak

e-mail:

ORCID:

Institute of Geography and Regional Development, University of Wroclaw, Pl. Uniwersytecki 1, 50-137 Wroclaw, Poland

9 Relict and contemporary soils on uplifted marine terraces of Kvartsittsletta, SW Spitsbergen

Bartosz Korabiewski

Keywords: Arctic Svalbard arctic soil Cryosols Cambisols soil processes permafrost

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Abstract

The soils of Arctic regions are of great interest due to their high sensitivity to climate change. Kvartsittsletta coast in the vicinity of the Baranowski Research Station of the University of Wrocław constitutes a sequence of differently aged sea terraces covered with different fractions of beach material. It is a parent material for several developing soil types. Despite the low intensity of the modern soil-forming processes, the soil cover is characterized by high diversity. Soil properties are formed mainly by geological and geomorphological factors, which are superimposed by the influence of climate and living organisms.
The degree of development of soil is usually an indicator of its relative age. This article highlights the dominant influence of lithology and microrelief over other soil-forming factors, including the duration for which the parent material was exposed to external factors. The soils on the highest (oldest) terrace steps of the Kvartsittsletta rarely showed deep signs of soil-forming processes other than cryoturbations. On the youngest terraces, deep-reaching effects of soil processes associated with a relatively warm climate, including the occurrence of cambic horizons, were observed. Their presence in Arctic regions carries important environmental information and may be relevant to studies of climate change.

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Authors and Affiliations

Bartosz Korabiewski

Department of Physical Geography, Institute of Geography and Regional Development, University of Wrocław, Plac Uniwersytecki 1, 50-137 Wrocław, Poland

10 Contemporary landscape transformation in a small Arctic catchment (Bratteggdalen, Svalbard)

Aleksandra Wołoszyn , Marek Kasprzak

Keywords: Arctic Spitsbergen small catchment geomorphology environmental changes

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Abstract

Small Arctic catchments that are sensitive to climate change reinforced by Arctic amplification remain poorly studied. Since the end of the Little Ice Age (LIA) glaciers on Svalbard have been retreating, and thus, many catchments have transformed from glaciated or partly glaciated to ice-free conditions. Our study focuses on changes that have occurred since the end of the LIA in a small High Arctic mountain catchment, Bratteggdalen. In this study, we traced changes in the Bratteggbreen glacier areal extent since 1976 with parallel vegetation analysis using Landsat and Sentinel data. The geomorphology of Bratteggdalen was mapped and basic morphometric analyses, such as long profile, hypsometric curve, slope and aspect orientation analyses were carried out. We also present a map of landforms in Bratteggdalen based on a fieldwork in 2018 and an analysis of orthophotomaps. Through this research, we enhance the knowledge of small catchments in polar regions.

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Authors and Affiliations

Aleksandra Wołoszyn

e-mail:

ORCID:

Marek Kasprzak

e-mail:

ORCID:

Institute of Geography and Regional Development, University of Wrocław, pl. Uniwersytecki 1, 50-137 Wrocław, Poland

11 Editorial: Processes controlling development of periglacial and paraglacial landscapes in rapidly changing polar regions: Part 1

Mateusz C. Strzelecki , Marek Kasprzak , Piotr Owczarek , Łukasz Stachnik

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Authors and Affiliations

Mateusz C. Strzelecki

e-mail:

ORCID:

Marek Kasprzak

e-mail:

ORCID:

Piotr Owczarek

e-mail:

ORCID:

Łukasz Stachnik

e-mail:

ORCID:

Alfred Jahn Cold Regions Research Centre, Institute of Geography and Regional Development, University of Wroclaw, pl. Uniwersytecki 1, 50-137 Wroclaw, Poland

12 Editorial: Processes controlling development of periglacial and paraglacial landscapes in rapidly changing polar regions: Part 2

Mateusz C. Strzelecki , Marek Kasprzak , Piotr Owczarek , Łukasz Stachnik

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Authors and Affiliations

Mateusz C. Strzelecki

e-mail:

ORCID:

Marek Kasprzak

e-mail:

ORCID:

Piotr Owczarek

e-mail:

ORCID:

Łukasz Stachnik

e-mail:

ORCID:

Alfred Jahn Cold Regions Research Centre, Institute of Geography and Regional Development, University of Wroclaw, pl. Uniwersytecki 1, 50-137 Wroclaw, Poland

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.