Jan Magne Cederstrøms bilde

Jan Magne Cederstrøm

  • E-postjan.cederstrom@uib.no
  • Telefon+47 976 41 319
  • Besøksadresse
    Allégaten 41
    5007 Bergen
    3F16c - 3139
  • Postadresse
    Postboks 7803
    5020 Bergen
Vitenskapelig artikkel
  • Vis forfatter(e) (2024). A 7000-year record of extreme flood events reconstructed from a threshold lake in southern Norway. Quaternary Science Reviews.
  • Vis forfatter(e) (2023). Revised Minoan eruption volume as benchmark for large volcanic eruptions. Nature Communications.
  • Vis forfatter(e) (2021). Semi‐automatic Ice Rafted Debris quantification with Computed Tomography. Paleoceanography and Paleoclimatology. 10 sider.
  • Vis forfatter(e) (2021). Rapid tephra identification in geological archives with computed tomography: Experimental results and natural applications. Frontiers in Earth Science. 1-12.
  • Vis forfatter(e) (2020). Tephra horizons identified in the western North Atlantic and Nordic Seas during the Last Glacial Period: Extending the marine tephra framework. Quaternary Science Reviews.
Vitenskapelig foredrag
  • Vis forfatter(e) (2023). Reconstructing glacier advances on the sub-Antarctic Kerguelen (49°S, 69°E) Islands for the last millennium.
  • Vis forfatter(e) (2023). Airborne ground penetrating radar surveying.
  • Vis forfatter(e) (2023). A 11-meter-long flood record from Vangsvatnet, Voss, western Norway – preliminary results.
  • Vis forfatter(e) (2022). New measurements of ice thickness on Jostedalsbreen ice cap reveal vulnerability to future fragmentation.
  • Vis forfatter(e) (2021). Semi-automated quantification of Ice Rafted Debris in sediment archives with Computed Tomography.
  • Vis forfatter(e) (2019). Harnessing the potential of CT scanning to identify cryptotephra in sediment cores: a controlled experiment.
Populærvitenskapelig artikkel
  • Vis forfatter(e) (2020). Fra medisin til geologi. geoforskning.no.
  • Vis forfatter(e) (2023). Holocene flood frequency at Vangsvatnet, western Norway, reconstructed from lake sediments and historical evidence.

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