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Petrography of the sand fraction, particle size analysis, and detrital zircon U/Pb isotope data, and pebble count data were collected from Byrd Glacier moraines and central/western Ross Sea till in or...
InJanuary2007,26samplesoftillfrom6differentmorainesalongtheReedy Glacier,EastAntarcticawerecollectedwiththegoalofdifferentiatingbetweenthese samplesandtillcollectedfromthebaseoftheWhillans,Kamb,andB...
The growing number of glacial margin lakes that have developed due to glacier retreat, have caused an increase of dangerous Glacial Lake Outburst Floods (GLOFs) in several regions over the last deca...
A review is given of the phenomenon of glacier outburst floods. Geographical distribution, modes of occurrence of glacier-dammed lakes and modes of lakeemptying are discussed. Techniques of monitori...
The report gives a review on the glacial-hydrological work carried out since 1974 in the project "Runoff within and from glaciers" of Sonderforschungsbereich 81 of the Technical University Munich wi...
For planning a hydropower station at Paakitsup Akuliarusersua in West Greenland, some unusual hydrological studies were required. The basin is situated about 45 km north-east of Ilulissat/Jakobshavn...
One hundred samples were collected from the surface of the Upper Fremont Glacier at equally spaced intervals defined by an 8,100 m 2 snow grid to assess the significance of lateral variability in ma...
Glacial and glaciohydrologic processes that control the glaciofluvial sediment delivery from Erikbreen, a polythermal glacier on the north coast of Spitsbergen (79"407N, 12"30'E), were studied durin...
Austre Okstindbreen, the largest glacier of the Okstindan area, Norway, covers about 14 km2 within a drainage basin of 22.5 km2. Each year, about one third of the discharge of the glacier river resu...
Marked vertical variations of ions and oxygen isotopes were present in the snowpack at the glacier Austre Okstindbreen during the pre-melting phase in 1995 at sites between 825 m and 1,470 m above s...
The relationship between the thickness of a glacier stream and its surface slope is discussed. Morphometrical features of the glacier surface serve as a basis for estimating the maximum thickness the ...
Superficial moraines grew in size during the entire 32-year-long period of direct monitoring of water and ice balance of the Djankuat Glacier in the Caucasus. The total area of debris cover on the g...
Vertical variations of oxygen isotopes in the snow which accumulates during the winter at the Norwegian glacier Austre Okstindbreen are not entirely eliminated after 1-2 months of ablation in the foll...
Estimation of sediment load from glacierized basins is very important for planning, designing, installation and operation of hydro-power projects, including management of reservoirs. In the present ...

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