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pro vyhledávání: '"Frank G. M. Van Tatenhove"'
Autor:
Frank G. M. Van Tatenhove
Publikováno v:
Earth Surface Processes and Landforms. 21:797-816
Changes in ice-marginal morphology near Leverett glacier, a small outlet glacier at the western margin of the Greenland ice sheet, are determined from a photogrammetrical analysis. To be able to compare two datasets from subsequent years with measure
Publikováno v:
Quaternary Research. 45:245-253
New evidence has been obtained for the age of the Umı̂vı̂t/Keglen and Ørkendalen moraine systems close to the present ice sheet margin in central West Greenland. The Umı̂vı̂t/Keglen moraine system is dated at 7500 to 650014C yr B.P., which i
Publikováno v:
Scopus-Elsevier
Annals of Glaciology, 23, 52-58. International Glaciology Society
Annals of Glaciology, 23, 52-58. International Glaciology Society
Ice-sheet modelling is an essential tool for estimating the effect of climate change on the Greenland ice sheet. The large spatial and long-term temporal scales of the ice-sheet model limits the amount of data which can be used to test model results.
Publikováno v:
Hydrological Processes, 9, 213-226. John Wiley and Sons Ltd
River discharge measurements downstream of the Russell Glacier, near Kangerlussuaq (Sondre Stroomfjord), West Greenland revealed the occurrence of short-term discharge fluctuations during the 1991 melt season. Frontal ice-cliff collapse results in te
Publikováno v:
Annals of Glaciology. 21:251-258
Fluctuations in the position and surface altitude of Leverett Glacier, a small outlet glacier at the western margin of the Greenland ice sheet, are determined from a photogrammetric analysis. During the Greenland Ice-Margin Experiment (GIMEX) 1992 ex
Publikováno v:
Quaternary Research, 44, 317-327. Academic Press Inc.
Ice sheet modeling is an essential tool for estimating the effect of climate change on the Greenland ice sheet. The large spatial and long-term temporal scale of ice sheet models limits the amount of data which can be used to test model results. A fr
Publikováno v:
Geomorphology. 6:59-67
Drumlins are relatively unknown in the Alps, the few known examples are briefly described. These all happen to be of Holocene age. The first known Lateglacial drumlins are described from the Augsttalli, a tributary to the Turtmanntal in Wallis, Switz
Publikováno v:
Geografiska Annaler. Series A, Physical Geography. 78:83