Blar i Geophysical Institute på forfatter "Darelius, Elin Maria K."
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Variability and mixing of the Filchner overflow plume on the continental slope,Weddell Sea
Daae, Kjersti; Fer, Ilker; Darelius, Elin Maria K. (Peer reviewed; Journal article, 2019-01)A large fraction of Antarctic Bottom Water is produced in the Weddell Sea, through mixing between the cold and dense shelf water masses and the warm and saline off-shelf water. We present observations of the dense Filchner ... -
Volume transport and mixing of the cold water overflow downstream of the Faroe Bank Channel from one year of moored measurements
Ullgren, Jenny; Darelius, Elin Maria K.; Fer, Ilker (Peer reviewed; Journal article, 2016-03-15)One-year long time series of current velocity and temperature from eight moorings deployed in the Faroe Bank Channel (FBC) are analysed to describe the structure and variability of the dense overflow plume on daily to ... -
Warm Circumpolar Deep Water at the Western Getz Ice Shelf Front, Antarctica
Assmann, Karen; Darelius, Elin Maria K.; Wåhlin, Anna K.; Kim, Tae Wan; Lee, Sang Hoon (Peer reviewed; Journal article, 2019-01-04)The Getz Ice Shelf is one of the largest sources of fresh water from ice shelf basal melt in Antarctica. We present new observations from three moorings west of Siple Island 2016–2018. All moorings show a persistent flow ... -
Wind stress mediated variability of the Filchner Trough overflow, Weddell Sea
Daae, Kjersti; Darelius, Elin Maria K.; Fer, Ilker; Østerhus, Svein; Ryan, S. (Peer reviewed; Journal article, 2018-05-06)The Filchner Trough (FT) is a key site for exchange of water masses between the Weddell Sea continental shelf and the deep ocean. Cold and dense Ice Shelf Water (ISW), a precursor for Antarctic Bottom Water, flows north ...