Climate change offers new perspectives for reservoirs near to the glacial environment. The reservoirs will benefit from increased water supply but are affected by increased sedimentation. Sediment transport was studied in Griessee. 61% of its catchment area is covered by glaciers. Particle size distribution (PSD) and suspended sediments concentration (SSC) were examined. Measurements were conducted with Niskin bottle sampler, laser in-situ scattering transmissometry (LISST) and acoustic Doppler current profiler (ADCP). They were compared with water samples. PSD and SSC show only minor fluctuations in the lake. The major part of the suspended sediments is silt, median diameters are between 5 and 10 μm. Average SSC is 80 mg/l. A minor turbidi...
Research on factors affecting sediment regime in glacierized catchments under warming climates is s...
Marine-terminating outlet glaciers discharge mass through iceberg calving, submarine melting, and me...
Detrital sediment is carried from land to the sea by three agents, rivers, glaciers, and winds. The ...
Climate change will impact the water and sediment conveyance into periglacial reservoirs. It is ther...
Fluvial processes dominate sediment flux from most cold environments and as such are particularly se...
Sustainable reservoir use is globally threatened by sedimentation. It has been generally recognized ...
Modern sedimentation in Lake Linné was studied as part of the NSF-funded Svalbard REU Project to cal...
Knowledge of Suspended Sediments Dynamics (SSD) across spatial scales is relevant for several fields...
Linnévatnet (78° 2’N, 13° 49’E), is a glacial-fed lake located in Svalbard, an archipelago north of ...
Suspended sediment concentration in meltwaters draining from Alpine glaciers vary considerably both ...
Sustainable reservoir use is globally threatened by sedimentation. It has been generally recognized ...
In the Swiss Alps, climatic changes have not only caused glacier retreat, but also likely increased ...
Sedimentation patterns in a Norwegian glacial lake were investigated with focus on climate-related h...
This study investigates sediment transport processes and sediment-landform development at two small ...
In estuaries and marine environments, primary particles are frequently transported as large floccula...
Research on factors affecting sediment regime in glacierized catchments under warming climates is s...
Marine-terminating outlet glaciers discharge mass through iceberg calving, submarine melting, and me...
Detrital sediment is carried from land to the sea by three agents, rivers, glaciers, and winds. The ...
Climate change will impact the water and sediment conveyance into periglacial reservoirs. It is ther...
Fluvial processes dominate sediment flux from most cold environments and as such are particularly se...
Sustainable reservoir use is globally threatened by sedimentation. It has been generally recognized ...
Modern sedimentation in Lake Linné was studied as part of the NSF-funded Svalbard REU Project to cal...
Knowledge of Suspended Sediments Dynamics (SSD) across spatial scales is relevant for several fields...
Linnévatnet (78° 2’N, 13° 49’E), is a glacial-fed lake located in Svalbard, an archipelago north of ...
Suspended sediment concentration in meltwaters draining from Alpine glaciers vary considerably both ...
Sustainable reservoir use is globally threatened by sedimentation. It has been generally recognized ...
In the Swiss Alps, climatic changes have not only caused glacier retreat, but also likely increased ...
Sedimentation patterns in a Norwegian glacial lake were investigated with focus on climate-related h...
This study investigates sediment transport processes and sediment-landform development at two small ...
In estuaries and marine environments, primary particles are frequently transported as large floccula...
Research on factors affecting sediment regime in glacierized catchments under warming climates is s...
Marine-terminating outlet glaciers discharge mass through iceberg calving, submarine melting, and me...
Detrital sediment is carried from land to the sea by three agents, rivers, glaciers, and winds. The ...