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1

Ground penetrating radar sounding on an active rock glacier on James Ross Island, Antarctic Peninsula region

100%
Fukui K., Sone T., Strelin J., Torielli C., Mori J.
Polish Polar Research
|
2007
|
tom 28
|
nr 1
This study used ground penetrating radar soundings to examine a tongue-shaped rock glacier (64°04'S 58°25'W) on James Ross Island, Antarctic Peninsula, in January 2005. The rock glacier studied has multiple well-developed transverse ridges and approximately 800 m long from the talus of its head to its frontal slopes and is 300 m wide in the middle. The longitudinal ground penetrating radar profile identified debris bands which dip up-glacier, similar to the thrust structures in the compression zone of a valley glacier. Transverse ground penetrating radar profiles indicated a layered structure which is inclined towards the central part of the rock glacier and which resembles the transverse foliation of a valley glacier. Consequently, the internal structure of the rock glacier is revealed as being similar to the "nested spoons" common in the interior of valley glaciers. We concluded that this rock glacier has been created by the deformation of a glacier ice core and a thick and continuous debris mantle.
2

Snow distribution patterns on Svalbard glaciers derived from radio-echo soundings

86%
Grabiec M., Puczko D., Budzik T., Gajek G.
Polish Polar Research
|
2011
|
tom 32
|
nr 4
3

First Cenozoic glaciers in West Antarctica

86%
Birkenmajer K., Gazdzicki A., Krajewski K. P., Przybycin A., Solecki A., Tatur A., Yoon H. I.
Polish Polar Research
|
2005
|
tom 26
|
nr 1
3-12
One of the most significant global climatic events in the Cenozoic was the transition from greenhouse to icehouse conditions in Antarctica. Tectonic evolution of the region and gradual cooling at the end of Eocene led to the first appearance of ice sheets at the Eocene/Oligocene boundary (ca. 34 Ma). Here we report geological record of mountain glaciers that preceded major ice sheet formation in Antarctica. A terrestrial- valley-type tillite up to 65 metres thick was revealed between two basaltic lava sequences in the Eocene- Oligocene Point Thomas Formation at Hervé Cove - Breccia Crag in Admiralty Bay- King George Island- South Shetland Islands. K-Ar dating of the lavas suggests the age of the glaciation at 45-41 Ma (Middle Eocene). It is the oldest Cenozoic record of alpine glaciers in West Antarctica- providing insight into the onset of glaciation of the Antarctic Peninsula and South Shetland Islands.
4

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

72%
Sobota I.
Polish Polar Research
|
2009
|
tom 30
|
nr 4
317-338
5

Distribution of snow accumulation on some glaciers of Spitsbergen

72%
Grabiec M., Leszkiewicz J., Glowacki P., Jania J.
Polish Polar Research
|
2006
|
tom 27
|
nr 4
309-326
We describe the spatial variability of snow accumulation on three selected glaciers in Spitsbergen (Hansbreen, Werenskioldbreen and Aavatsmarkbreen) in the winter seasons of 1988/89, 1998/99 and 2001/2002 respectively. The distribution of snow cover is determined by the interrelationships between the direction of the glacier axes and the dominant easterly winds. The snow distribution is regular on the glaciers located E-W, but is more complicated on the glaciers located meridionally. The western part of glaciers is more predisposed to the snow accumulation than the eastern. This is due to snowdrift intensity. Statistical relationships between snow accumulation, deviation of accumulation from the mean values and accumulation variability related to topographic parameters such as: altitude, slope inclination, aspect, slope curvature and distance from the edge of the glacier have been determined. The only significant relations occured between snow accumulation and altitude (r = 0.64-0.91).
6

Influence of positive degree-days and sunshine duration on the surface ablation of Hansbreen, Spitsbergen glacier

72%
Szafraniec J.
Polish Polar Research
|
2002
|
tom 23
|
nr 3-4
227-240
7

Maximum limits of the Baltic ice-sheet during the Pomeranian Phase in the Drawskie Lakeland

72%
Klysz P.
Quaestiones Geographicae
|
2003
|
tom 22
8

Submarine evidence of the Aavatsmark and Dahl Glaciers fluctuations in the Kaffioyra region, NW Spitsbergen

72%
Grzes M., Krol M., Sobota I.
Polish Polar Research
|
2009
|
tom 30
|
nr 2
143-160
9
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Surface wave generation due to glacier calving

72%
Massel S. R., Przyborska A.
Oceanologia
|
2013
|
tom 55
|
nr 1
10

Post-'Little Ice Age' retreat rates of glaciers around Billefjorden in Central Spitsbergen, Svalbard

72%
Rachlewicz G., Szczucinski W., Ewertowski M.
Polish Polar Research
|
2007
|
tom 28
|
nr 3
Twelve glaciers, representing various types, were investigated between 2000 and 2005, in a region adjacent to the northern reaches of Billefjorden, central Spitsbergen (Svalbard). On the basis of measurements taken using reference points, DGPS and GPS systems, analyses of aerial photographs and satellite images, geomorphological indicators and archival data their rates of deglaciation following the "Little Ice Age" (LIA) maximum were calculated variously on centennial, decadal and annual time scales. As most Svalbard glaciers have debris-covered snouts, a clean ice margin was measured in the absence of debris-free ice front. The retreat rates for both types of ice fronts were very similar. All studied glaciers have been retreating since the termination of the Little Ice Age at the end of 19th century. The fastest retreat rate was observed in the case of the Nordenskioldbreen tidewater glacier (mean average linear retreat rate 35 m a-1). For land-terminating glaciers the rates were in range of 5 to 15 m a-1. Presumably owing to climate warming, most of the glacier retreat rates have increased several fold in recent decades. The secondary factors influencing the retreat rates have been identified as: water depth at the grounding line in the case of tidewater glaciers, surging history, altitude, shape and aspect of glacier margin, and bedrock relief. The retreat rates are similar to glaciers from other parts of Spitsbergen. Analyses of available data on glacier retreat rates in Svalbard have allowed us to distinguish four major types: very dynamic, surging tidewater glaciers with post-LIA retreat rates of between 100 and 220 ma-1, other tidewater glaciers receding of a rate of 15 to 70 m a-1, land terminating valley polythermal glaciers with an average retreat of 10 to 20 m a-1 and small, usually cold, glaciers with the retreat rates below 10 m a-1.
11

Preliminary determination of concentration and distribution of suspension and roily oil emulsion in Kongsfiord, Spitsbergen

72%
Gurgul H., Staron W.
Polish Polar Research
|
2000
|
tom 21
|
nr 1
12

Mosses of postglacial corries situated in Polish part of Karkonosze Mts - the state of current knowledge

72%
Fudali E.
Biological Bulletin of Poznań
|
2001
|
tom 38
|
nr 2
13

Winter snow accumulation and discharge from the Waldemar Glacier Northwestern Spitsbergen in 1996-1998

72%
Grzes M., Sobota I.
Polish Polar Research
|
2000
|
tom 21
|
nr 1
14

Ablation and discharge of the Waldemar Glacier, North-Western Spitsbergen in summer 1998

72%
Sobota I.
Polish Polar Research
|
2000
|
tom 21
|
nr 1
15

First record of testate amoebae on glaciers and description of a new species Puytoracia jenswendti nov. sp. (Rhizaria, Euglyphida)

58%
Santibanez P., Kohshima S., Scheihing R., Silwa R., Jaramillo J., Labarca P., Casassa G.
Acta Protozoologica
|
2011
|
tom 50
|
nr 1
16

Glacier distribution and direction in Svalbard, Axel Heiberg Island and throughout the Arctic: General northward tendencies

58%
Evans I. S.
Polish Polar Research
|
2011
|
tom 32
|
nr 3
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