0000000001234614

AUTHOR

Alexander Prokop

showing 6 related works from this author

PRISM - Permafrost, Rock, Ice and Snow monitoring in the Austre Lovén glacier basin (Spitsberg)

2017

International audience

[SHS.GEO] Humanities and Social Sciences/Geography[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[ SDU.STU.GL ] Sciences of the Universe [physics]/Earth Sciences/Glaciology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences[SHS.GEO]Humanities and Social Sciences/Geography[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/GlaciologyComputingMilieux_MISCELLANEOUS[SDU.STU.GL] Sciences of the Universe [physics]/Earth Sciences/Glaciology[ SHS.GEO ] Humanities and Social Sciences/Geography
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Monitoring the snow cover on the slopes of a polar glacier basin using terrestrial laser scanning

2012

COM; International audience

[SHS.GEO] Humanities and Social Sciences/Geography[SHS.GEO]Humanities and Social Sciences/GeographyComputingMilieux_MISCELLANEOUS[ SHS.GEO ] Humanities and Social Sciences/Geography
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A terrestrial laser scanning survey to derive snow volume and water equivalent on the slopes of Austre Lovén glacier basin (Svalbard - 79°N)

2013

COM; International audience; Steep slopes represent 35% of Austre Lovén glacier basin, a small valley glacier in Svalbard (79°N). Slopes and their dynamics do have an important impact on polar glaciers. They also are of high hydrological importance in the water budget of basins. One major issue in studying slopes is the fact that they are hard to instrument and both equipment and staff have to deal with the steepness of the field and the exposure to avalanches and rock fall. In order to minimize this exposure without giving up the required spatial and temporal precision, terrestrial laser scanning (TLS) is used. A monitoring program is now starting using TLS. TLS allows for remote high qual…

[SHS.GEO] Humanities and Social Sciences/Geography[SHS.GEO]Humanities and Social Sciences/Geography[ SHS.GEO ] Humanities and Social Sciences/Geography
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Spatial variability of snow cover in the slopes of a small arctic glacier catchment using Lidar data

2017

International audience; In the Arctic, because glaciers are subject to dramatic changes due to climate shift, a major concern is to estimate the contribution of glacier basins outflows to sea level rise. Snow on the Austre Lovénbreen (a small alpine type glacier in Spitsbergen – 4,6km 2) has been well studied since 2007 thanks to a good measurement network and numerous field campaigns. It has been possible to estimate the runoff coming from the glacier itself. However, the glacier covers only 43% of the Austre Lovén catchment. Of the remaining 57%, 23% are constituted by the moraine area, and 34 % are the surrounding slopes, which are also important snow storages. This paper focusing on slo…

[SHS.GEO] Humanities and Social Sciences/Geography[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[ SDU.STU.GL ] Sciences of the Universe [physics]/Earth Sciences/Glaciology[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciences[SHS.GEO]Humanities and Social Sciences/Geography[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology[SDU.STU.GL] Sciences of the Universe [physics]/Earth Sciences/Glaciology[ SHS.GEO ] Humanities and Social Sciences/Geography
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Investigating snowcover volumes and icings dynamics in the moraine of an Arctic catchment using UAV/ photogrammetry and LiDAR

2016

International audience; Means for assessing the contribution of the terminal moraine into the water budget of an Arctic glacier is investigated: on the one hand the terminal moraine represents a significant fraction (22%)of the catchment area of the glacier under investigation – Austre Lovenbreen, in the Brøgger peninsula, Spitsbergen – and on the other hand icings formation (or aufeis) each winter illustrates the contribution of subglacial water flow. While over the glacier, with a smooth surface readily interpolated, the winter and summer mass balances are assessed with only a few sparsely distributed stakes, such an approach is not valid with the rough topography of the glacier moraine: …

Arctic[SHS.GEO] Humanities and Social Sciences/Geography[SDU.STU] Sciences of the Universe [physics]/Earth Sciences[SDU.STU]Sciences of the Universe [physics]/Earth Sciences[ SDU.STU ] Sciences of the Universe [physics]/Earth Sciencesgeomorphology[SHS.GEO]Humanities and Social Sciences/GeographyUAVsSnowcoverpro- glacial morainephotogrammetryStructure from Motion[ SHS.GEO ] Humanities and Social Sciences/Geography
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Witnessing and measuring the impacts of cryosphere changes in the High Arctic

2016

International audience

cryosphere changesHigh Arctic[SHS.GEO] Humanities and Social Sciences/Geography[SHS.GEO]Humanities and Social Sciences/GeographyComputingMilieux_MISCELLANEOUS[ SHS.GEO ] Humanities and Social Sciences/Geography
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