Zobrazeno 1 - 10
of 26
pro vyhledávání: '"Ida Lønne"'
Autor:
Ida Lønne
Publikováno v:
Geomorphology. 276:180-202
High-Arctic terrestrial slopes have received limited systematic research interest, but increased vulnerability related to regional warming has driven the call for better knowledge of the dynamics of these systems. Studies of sediment transport from a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f974254e3c9b3a47ad15b5f119485de8
https://doi.org/10.1016/j.geomorph.2016.10.004
https://doi.org/10.1016/j.geomorph.2016.10.004
Autor:
Ida Lønne
Publikováno v:
Quaternary Science Reviews. 132:74-100
Svalbard is a key area for the investigation of glacial surges, and almost two centuries worth of field observations exists from this region. Studies have shown that the course of a surge and the associated formation of landforms are strongly influen
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ded6afec8d16e5d1bb3827046c8e352
https://doi.org/10.1016/j.quascirev.2015.11.009
https://doi.org/10.1016/j.quascirev.2015.11.009
Autor:
Ida Lønne
Publikováno v:
Geografiska Annaler: Series A, Physical Geography. 96:177-194
Glacial surges in valbard are protracted and characterized by individual dynamic evolution, in contrast to many other areas, which calls for a subdivision of the classic two‐phased surge cycle. A d...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a41ffc7176d0882ed621f10be78e2fa8
https://doi.org/10.1111/geoa.12040
https://doi.org/10.1111/geoa.12040
Autor:
Ida Lønne
Publikováno v:
Geomorphology. 207:190-202
Glacial surges are periods of fast flow, often limited in space and time, and driven by internal conditions which are not fully explained. The quantity and variety of documented case-studies and settings demonstrate that the critical variables are di
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b29157c1f1aa74838ce8019706d12d9b
https://doi.org/10.1016/j.geomorph.2013.11.005
https://doi.org/10.1016/j.geomorph.2013.11.005
Autor:
Ida Lønne, Wojciech Nemec
Publikováno v:
Geological Society, London, Special Publications. 354:33-56
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c127b6dcfd7fc6420810922aaba587b
https://doi.org/10.1144/sp354.3
https://doi.org/10.1144/sp354.3
Autor:
Wojciech Nemec, Ida Lønne
Publikováno v:
Geological Society, London, Special Publications. 354:57-75
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4321f397d2bd515bd5296d64c74c6819
https://doi.org/10.1144/sp354.4
https://doi.org/10.1144/sp354.4
Formation and disintegration of a high-arctic ice-cored moraine complex, Scott Turnerbreen, Svalbard
Publikováno v:
Boreas. 30:272-284
Englacial debris structures, morphology and sediment distribution at the frontal part and at the proglacial area of the Scott Turnerbreen glacier have been studied through fieldwork and aerial photograph interpretation. The main emphasis has been on
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::568ad22fbd750bc51a3430640ec23f87
https://doi.org/10.1111/j.1502-3885.2001.tb01046.x
https://doi.org/10.1111/j.1502-3885.2001.tb01046.x
Autor:
Ida Lønne
Publikováno v:
Boreas. 34:308-323
Raised marine beach gravel at 62 m a.s.l. in Bolterdalen indicates that the inner part of Adventfjorden, central Spitsbergen, was ice-free shortly before 10 025±160yr BP. A glacier advanced across the regressive, frozen beach terraces and into shall
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8f22398e9a4730a5008b9fc2ec56753a
https://doi.org/10.1111/j.1502-3885.2005.tb01103.x
https://doi.org/10.1111/j.1502-3885.2005.tb01103.x
Autor:
Jan Mangerud, Ida Lønne
Publikováno v:
Boreas. 20:85-104
A 20 m thick shallow marine sequence, capped by a Late Weichselian lodgement till, is exposed for 200111 along the river in Linnedalen on the west coast of Svalbard. Five formations are recognized: Formation A, the oldest, consists of a shallow marin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::13e0de07e34e35970231b0b3b30a45c2
https://doi.org/10.1111/j.1502-3885.1991.tb00298.x
https://doi.org/10.1111/j.1502-3885.1991.tb00298.x
Autor:
Astrid Lyså, Ida Lønne
Publikováno v:
Geomorphology. 72:300-319
The late culmination of the Little Ice Age (LIA) on Svalbard allows a detailed reconstruction of the landscape's response to the subsequent climatic warming. The study area comprises a small glacier (400–1000 m a.s.l.), on the south side of Adventf
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9076a4da983bd9341069a95715af38b4
https://doi.org/10.1016/j.geomorph.2005.06.003
https://doi.org/10.1016/j.geomorph.2005.06.003