Jakob Heyman

Biographic Data

ID3818068
NAMEJakob Heyman
GIVEN NAMESJakob
FAMILY NAMEHeyman
SIGNATUREHEYMAN J
AFFILIATIONSStockholm University
ORCID0000-0001-8062-5366
VERIFIEDYes
TOTAL WORKS8
TOTAL CITATIONS0
AUTHOR COUNT8
EDITOR COUNT0
FIRST PUBLICATION YEAR2008
LATEST PUBLICATION YEAR2016
H-INDEX0

  • Deglaciation of Fennoscandia

    Open AccessArjen P Stroeven, Clas Hättestrand et al.ARTICLEQuaternary Science Reviews2016

    To provide a new reconstruction of the deglaciation of the Fennoscandian Ice Sheet, in the form of calendar-year time-slices, which are particularly useful for ice sheet modelling, we have compiled and synthesized published geomorphological data for eskers, ice-marginal formations, lineations, marginal meltwater channels, striae, ice-dammed lakes, and geochronological data from radiocarbon, varve, optically-stimulated luminescence, and cosmogenic…

  • Glacial geomorphology of the Altai and Western Sayan Mountains, Central Asia

    Open AccessRobin Blomdin, Jakob Heyman et al.ARTICLEJournal of Maps2016

    In this article, we present a map of the glacial geomorphology of the Altai andWestern Sayan Mountains, covering an area of almost 600,000 km2. Although numerous studies provide evidence for restricted Pleistocene glaciations in this area, others have hypothesized the past existence of an extensive ice sheet. To provide a framework for accurate glacial reconstructions of the Altai and Western Sayan Mountains, we present a map at a scale of 1:1,00…

  • Glacial geomorphology of the Maidika region, Tibetan Plateau

    Open AccessMiranda S Lindholm, Jakob HeymanARTICLEJournal of Maps2016

    We present a glacial geomorphological map at a scale of 1:200, 000 of the Maidika region in the southeastern part of the central Tibetan Plateau covering 13, 600 km2. Based on the 90 m resolution SRTM elevation model, the 30 m resolution ASTER GDEM elevation model, and the Landsat ETM+ satellite imagery of 30/15 m resolution, we have mapped glacial valleys, marginal moraines, glacial lineations, and hummocky terrain. Glacial landforms occur frequ…

  • Paleo-climate of the central European uplands during the last glacial maximum based on glacier mass-balance modeling

    Open AccessBarbara M Heyman, Jakob Heyman et al.ARTICLEQuaternary Research2013

    During the last glacial maximum (LGM), glaciers existed in scattered mountainous locations in central Europe between the major ice masses of Fennoscandia and the Alps. A positive degree-day glacier mass-balance model is used to constrain paleo-climate conditions associated with reconstructed LGM glacier extents of four central European upland regions: the Vosges Mountains, the Black Forest, the Bavarian Forest, and the Giant Mountains. With reduc…

  • Glacial geomorphology of the Tian Shan

    Open AccessArjen P Stroeven, Clas Hättestrand et al.ARTICLEJournal of Maps2013

    The glacial geomorphology of the Tian Shan has been mapped, with the study area covering almost 638,000 km2. The map, designed to be printed at A0 size due to the elongated shape of the mountain range, is presented at a scale of 1:1,100,000. Five glacial landform categories are presented; glacial valleys, marginal moraines, glacial lineations, hummocky terrain and meltwater channels. These landform categories were mapped using the Shuttle Radar T…

  • Glacial geomorphology of the Shaluli Shan area, southeastern Tibetan Plateau

    Open AccessPing Fu, Jakob Heyman et al.ARTICLEJournal of Maps2012

    We present a glacial geomorphological map covering 1.04 × 105 km2 of the Shaluli Shan (Shan = Mountain), southeastern Tibetan Plateau. Using a 90 m digital elevation model from the Shuttle Radar Topography Mission and 15/30 m Landsat Enhanced Thematic Mapper Plus satellite imagery, we have mapped glacial valleys, marginal moraines, hummocky terrain, glacial lineations and ice-scoured terrain. Lineations and scoured areas largely overlap on the lo…

  • Glacial geomorphology of the central Tibetan Plateau

    Open AccessBjörn Morén, Jakob Heyman et al.ARTICLEJournal of Maps2011

    Please click here to download the map associated with this article. The glacial geomorphology of the central Tibetan Plateau was mapped over 285,000 km2. Here we present a map covering 135,000 km at a scale of 1:660,000. The glacial geomorphology was mapped using 15 and 30 m resolution Landsat 7 ETM+ satellite imagery, a 90 m resolution SRTM digital elevation model, and satellite and aerial images displayed in Google Earth. Four landform categori…

  • Glacial geomorphology of the Bayan Har sector of the NE Tibetan Plateau

    Open AccessJakob Heyman, Clas Hättestrand et al.ARTICLEJournal of Maps2008

    Please click here to download the map associated with this article. We here present a detailed glacial geomorphological map covering 136,500 km2 of the Bayan Har sector of the northeastern Tibetan Plateau—an area previously suggested to have nourished the most extensive Quaternary glaciers of the Tibetan Plateau. The map, presented at a scale of 1:650,000, is based on remote sensing of a 90 m SRTM digital elevation model and 15/30 m Landsat ETM+ …