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Henrik Løseth Jansen

Biographic Data

ID6376277
NAMEHenrik Løseth Jansen
GIVEN NAMESHenrik Løseth
FAMILY NAMEJansen
SIGNATUREJANSEN H L
AFFILIATIONSUniversity of Bergen
ORCID0000-0002-2882-877X
VERIFIEDYes
TOTAL WORKS4
TOTAL CITATIONS4
WORKS AS AUTHOR4
WORKS AS EDITOR0
FIRST PUBLICATION YEAR2016
LATEST PUBLICATION YEAR2018
H-INDEX1
  • An inverse approach to the course of the ‘Little Ice Age’ glacier advance and the following deglaciation at Austerdalsisen, eastern Svartisen, northern Norway

    Open Access•Henrik Løseth Jansen, Svein Olaf Dahl et al.•ARTICLE•The Holocene•2018•References: 8

    The course of the ‘Little Ice Age’ (LIA) in Scandinavia is characterized by large glacier advances that started at about AD 1300 and culminated at about AD 1750. The end of the LIA is marked as an unprecedented and ongoing glacier retreat that accelerated from the early 20th century. The course of the LIA is here presented based on fluctuations of Austerdalsisen, the largest valley outlet glacier draining the Austre Svartisen (Østisen) ice cap, N…

  • Mid- to late Holocene aeolian activity recorded in a coastal dunefield and lacustrine sediments on Andøya, northern Norway

    Open Access•Pål Ringkjøb Nielsen, Svein Olaf Dahl et al.•ARTICLE•The Holocene•2016•Cited by: 1•References: 25

    In an effort to reconstruct past aeolian activity, a foredune stratigraphy and a continuous lake sediment record from the largest dunefield on Andøya, northern Norway, have been investigated. The dunefield extends landwards in a north-eastward direction and consists of several parabolic dunes, foredunes and blowouts. The sediment record (169 cm) from the nearby lake Latjønna and the foredune stratigraphy (10 m) covers the last 6200 and 3700 cal. …

  • A high-resolution 1200-year lacustrine record of glacier and climate fluctuations in Lofoten, northern Norway

    Open Access•Pål Ringkjøb Nielsen, Nicholas L Balascio et al.•ARTICLE•The Holocene•2016•References: 46

    Here we present the first high-resolution late-Holocene glacier record from the Lofoten archipelago in northern Norway. The study is based on analyses of lacustrine sediments from the distal glacier-fed lake Kveitvikvatnet (30.1 m a.s.l.), as well as glacial-geomorphological mapping of the ~4.2-km 2 surrounding catchment. The lake sediment cores have been examined for input of glacial-derived sediments by using physical, geochemical and magnetic …

  • Holocene glacier and climate fluctuations of the maritime ice cap Høgtuvbreen, northern Norway

    Open Access•Henrik Løseth Jansen, Joachim Riis Simonsen et al.•ARTICLE•The Holocene•2016•Cited by: 3•References: 18

    Holocene fluctuations of a small outlet glacier from the ice cap Høgtuvbreen at 65° N in coastal northern Norway are reconstructed based on distal glacier-fed lake sediments, complemented by a moraine sequence dated by lichenometry. Glaciers respond to changes in accumulation-season precipitation, ablation-season temperature and redistribution of snow by wind. Hence, reconstructions of glacier fluctuations based on distal glacier-fed lakes may gi…

  • Holocene glacier and climate fluctuations of the maritime ice cap Høgtuvbreen, northern Norway

    Open Access•Henrik Løseth Jansen, Joachim Riis Simonsen et al.•ARTICLE•The Holocene•2016•Cited by: 3•References: 18

    Holocene fluctuations of a small outlet glacier from the ice cap Høgtuvbreen at 65° N in coastal northern Norway are reconstructed based on distal glacier-fed lake sediments, complemented by a moraine sequence dated by lichenometry. Glaciers respond to changes in accumulation-season precipitation, ablation-season temperature and redistribution of snow by wind. Hence, reconstructions of glacier fluctuations based on distal glacier-fed lakes may gi…

  • Mid- to late Holocene aeolian activity recorded in a coastal dunefield and lacustrine sediments on Andøya, northern Norway

    Open Access•Pål Ringkjøb Nielsen, Svein Olaf Dahl et al.•ARTICLE•The Holocene•2016•Cited by: 1•References: 25

    In an effort to reconstruct past aeolian activity, a foredune stratigraphy and a continuous lake sediment record from the largest dunefield on Andøya, northern Norway, have been investigated. The dunefield extends landwards in a north-eastward direction and consists of several parabolic dunes, foredunes and blowouts. The sediment record (169 cm) from the nearby lake Latjønna and the foredune stratigraphy (10 m) covers the last 6200 and 3700 cal. …

  • Mid- to late Holocene aeolian activity recorded in a coastal dunefield and lacustrine sediments on Andøya, northern Norway

    Open Access•Pål Ringkjøb Nielsen, Svein Olaf Dahl et al.•ARTICLE•The Holocene•2016•Cited by: 1•References: 25

    In an effort to reconstruct past aeolian activity, a foredune stratigraphy and a continuous lake sediment record from the largest dunefield on Andøya, northern Norway, have been investigated. The dunefield extends landwards in a north-eastward direction and consists of several parabolic dunes, foredunes and blowouts. The sediment record (169 cm) from the nearby lake Latjønna and the foredune stratigraphy (10 m) covers the last 6200 and 3700 cal. …

  • A high-resolution 1200-year lacustrine record of glacier and climate fluctuations in Lofoten, northern Norway

    Open Access•Pål Ringkjøb Nielsen, Nicholas L Balascio et al.•ARTICLE•The Holocene•2016•References: 46

    Here we present the first high-resolution late-Holocene glacier record from the Lofoten archipelago in northern Norway. The study is based on analyses of lacustrine sediments from the distal glacier-fed lake Kveitvikvatnet (30.1 m a.s.l.), as well as glacial-geomorphological mapping of the ~4.2-km 2 surrounding catchment. The lake sediment cores have been examined for input of glacial-derived sediments by using physical, geochemical and magnetic …

  • Holocene glacier and climate fluctuations of the maritime ice cap Høgtuvbreen, northern Norway

    Open Access•Henrik Løseth Jansen, Joachim Riis Simonsen et al.•ARTICLE•The Holocene•2016•Cited by: 3•References: 18

    Holocene fluctuations of a small outlet glacier from the ice cap Høgtuvbreen at 65° N in coastal northern Norway are reconstructed based on distal glacier-fed lake sediments, complemented by a moraine sequence dated by lichenometry. Glaciers respond to changes in accumulation-season precipitation, ablation-season temperature and redistribution of snow by wind. Hence, reconstructions of glacier fluctuations based on distal glacier-fed lakes may gi…

  • An inverse approach to the course of the ‘Little Ice Age’ glacier advance and the following deglaciation at Austerdalsisen, eastern Svartisen, northern Norway

    Open Access•Henrik Løseth Jansen, Svein Olaf Dahl et al.•ARTICLE•The Holocene•2018•References: 8

    The course of the ‘Little Ice Age’ (LIA) in Scandinavia is characterized by large glacier advances that started at about AD 1300 and culminated at about AD 1750. The end of the LIA is marked as an unprecedented and ongoing glacier retreat that accelerated from the early 20th century. The course of the LIA is here presented based on fluctuations of Austerdalsisen, the largest valley outlet glacier draining the Austre Svartisen (Østisen) ice cap, N…

Geography (4 works) · Geology (4 works) · Geology and Paleoclimatology Research (4 works) · Geomorphology (4 works) · Oceanography (4 works) · Physical geography (4 works) · Cirque glacier (3 works) · Cryosphere (3 works) · Cryospheric studies and observations (3 works) · Glacial period (3 works)

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