Else Kolstrup
Uppsala University
28 Papers
306 Citations
Else Kolstrup is an academic researcher from Uppsala University. The author has contributed to research in topics: Geographic information system & Holocene. The author has an hindex of 17, co-authored 28 publications.
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Papers
Changes in palsa distribution in relation to climate change in Laivadalen, Northern Sweden, especially 1960-1997.
Frieda S. Zuidhoff,Else Kolstrup +1 more
TL;DR: In this article, changes in the distribution of palsas in Sweden's most southerly major palsa bog are outlined from 1960 to 1997 using aerial photographs taken in 1960 and 1976 as well as a study reported in a publ...
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Late Weichselian environmental change in southern Sweden and Denmark.
Björn E. Berglund,Svante Björck,Geoffrey Lemdahl,Helene Bergsten,Kjell Nordberg,Else Kolstrup +5 more
TL;DR: In this article, a synthesis of envronmental and climatic variations that are inferred to have occurred in southern Sweden (up to latitude 59°N) and Denmark during the Weichselian Late-glacial (14-9 ka BP) is presented.
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Structure and contents of a new geomorphological GIS database linked to a geomorphological map : With an example from Liden, central Sweden
TL;DR: In this paper, the authors present the structure and contents of a standardised geomorphological GIS database that constitutes the basis for processing and extracting spatial thematic data, including morphography/morphometry, hydrography, lithology, genesis, processes and age.
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Chemical denudation in arctic-alpine Latnjavagge (Swedish Lapland) in relation to regolith as assessed by radio magnetotelluric-geophysical profiles
TL;DR: In this article, chemical denudation in arctic-alpine Latnjavagge (Swedish Lappland) in relation to regolith was assessed by radio magnetotelluric-geophysical profiles.
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Three frost wedge casts from Jutland (Denmark) and TL dating of their infill
Else Kolstrup,Vagn Mejdahl +1 more
TL;DR: In this article, the characteristics of three wedges with a high proportion of primary infill of eolian sand are described in some detail, and the TL ages are: 39,000 ± 5,000, 24,000 − 3,000 and 17,000−3,000 years B.P.
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