Now showing items 41-50 of 64
Comparison of lamination stratigraphies of cores recovered from the proximal basin of Lake Linne, Svalbard, Norway
Bennett's research was directed at correlating the lamination stratigraphy of adjacent cores recovered from a proximal basin in Lake Linne'. His work showed that small changes in position and bathymetry can cause changes ...
Mechanisms and Processes of Suspended Sediment Transport and Deposition in High Arctic Proglacial Lake Linne'vatnet, Spitsbergen, Svalbard
Ben's research was directed at better understanding how and under what conditions sediment was distributed and deposited in Lake Linne' during the 2005/2006 sedimentation year.
Snowmelt 2008 in Linnédalen
Leo used daily images from our automated camera to quantify the amount and rate of snow melt in the Linne' Valley during the spring of 2008.
Evidence for Accelerated Surface Melting Rates on the Linne' Glacier, Svalbard
Emily studied the factors that influence glacier ablation (and surface lowering)during the 2006 melt season
Seasonal Dynamics of a High Arctic Lake, Lake Linne, Spitsbergen Island, Svalbard
Melanie, studied the thermal evolution of Lake Linne' from summer 2003 to summer 2004 and related the observed changes in the lake to measured weather conditions
The Nature of Laminations in Cores from Kongressvatnet, Svalbard, Norway
Emme studied a thin section of a core recovered from Lake Kongress in order to characterize the lamination stratigraphy. Her work suggests that the varves are chemical in nature.
Characterization of Climatic Influences on Modern Sedimentation in an Arctic Lake, Svalbard, Norway
Nick, was the first student to study the sediment traps recovered from Lake Linne' and to relate the measured textural changes from trap to trap and to measured weather parameters in the valley
Caroline Alden's thesis
Should be 13 Word Doc files in zip archive
Unsustainable glacier ablation at 78 N latitude, Linne’breen, Svalbard
Caleb's project was to compare the glacier margin positions documented by aerial photographs and to place the observed glacier retreat in the context of measure changes in mass balance.
Mary Lyon Hall 20
All building footprints were obtained from Facilities Management and are updated annually as necessary.