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PHOTOGRAMMETRIC MONITORING OF GLACIER MARGIN LAKES
Photogrammetric network image sequence processing disaster monitoringp
2014/4/24
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...
Glacial-Hydrological Investigations at the Vernagtferner Glacier as a Basis for a Discharge Model
Glacial-Hydrological Investigations Vernagtferner Glacier Discharge Model
2009/10/28
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...
Hydrological Background of a Glacier-Influenced Hydropower Station in Greenland
Hydrological Background Glacier-Influenced Hydropower Station Greenland
2009/10/27
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...
Hydrology of a Polythermal Glacier,Erikbreen,Northern Spitsbergen
Hydrology Polythermal Glacier
2009/10/26
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...
Indirect Estimation of the Djankuat Glacier Volume Based on Surface Topography
Indirect Estimation Djankuat Glacier Volume Surface Topography
2009/10/22
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 ...
