Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Lisbeth Håvik"'
Publikováno v:
Nature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
Warm Atlantic water circulates cyclonically around the Nordic Seas while gradually cooling. Here, the authors show that the retreat of the ice edge toward Greenland has led to further transformation of this water mass, which is no longer situated und
Externí odkaz:
https://doaj.org/article/7e30a63ee13046c5ad2fba4ad6f33dce
Publikováno v:
Journal of Physical Oceanography
Hydrographic measurements from ships, autonomous profiling floats, and instrumented seals over the period 1986–2016 are used to examine the temporal variability in open-ocean convection in the Greenland Sea during winter. This process replenishes t
Autor:
Lisbeth Håvik, Kjetil Våge
Publikováno v:
Journal of Geophysical Research: Oceans. 123:6106-6115
Autor:
Lisbeth Håvik, W.-J. von Appen, Robert S. Pickart, Benjamin E. Harden, Kjetil Våge, Steingrímur Jónsson, Svein Østerhus
Publikováno v:
EPIC3Journal of Physical Oceanography, 47(10), pp. 2631-2646, ISSN: 0022-3670
Data from a mooring array deployed north of Denmark Strait from September 2011 to August 2012 are used to investigate the structure and variability of the shelfbreak East Greenland Current (EGC). The shelfbreak EGC is a surface-intensified current si
Autor:
Lisbeth Håvik, Daniel J. Torres, W.-J. von Appen, Waldemar Walczowski, Andreas M. Thurnherr, Agnieszka Beszczynska-Möller, Kjetil Våge, Robert S. Pickart
Publikováno v:
Journal of Geophysical Research: Oceans. 122:1974-1994
We present measurements from two shipboard surveys conducted in summer 2012 that sampled the rim current system around the Nordic Seas from Fram Strait to Denmark Strait. The data reveal that, along a portion of the western boundary of the Nordic Sea
Publikováno v:
Journal of Physical Oceanography
Dense water masses transported southward along the east coast of Greenland in the East Greenland Current (EGC) form the largest contribution to the Denmark Strait Overflow. When exiting Denmark Strait these dense water masses sink to depth and feed t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cee7e47e25c2ee0544e16aab82419f52
Publikováno v:
Nature Communications
Nature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
Nature Communications, Vol 9, Iss 1, Pp 1-8 (2018)
Warm subtropical-origin Atlantic water flows northward across the Greenland-Scotland Ridge into the Nordic Seas, where it relinquishes heat to the atmosphere and gradually transforms into dense Atlantic-origin water. Returning southward along east Gr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::485c6c2b27ae0b4d57a09579e1ddc4a6
https://hdl.handle.net/1956/17977
https://hdl.handle.net/1956/17977
Autor:
Tore Hattermann, Robert S. Pickart, Frank Bahr, Daniel J. Torres, Benjamin E. Harden, Lisbeth Håvik, Clark Richards, Andreas Macrander, Kjetil Våge, Hedinn Valdimarsson, Svein Østerhus, Eli Børve, Laura de Steur, Steingrímur Jónsson
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers
© The Author(s), 2016. This is the authors version of the work and is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Deep Sea Research Part I: Oceanographic Research Papers 112 (2016)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::60cfd98afc0db40937c7212549215b55
http://imis.nioz.nl/imis.php?module=ref&refid=259115
http://imis.nioz.nl/imis.php?module=ref&refid=259115
To investigate initial sea-ice growth in open water, we carried out an ice-tank study with three different setups: grease ice grew in experiments with waves and in experiments with a current and wind, while nilas formed in a quiescent experimental se
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c283846eb8da3e4e6f9893e4f781b27
https://doi.org/10.5194/tcd-6-125-2012
https://doi.org/10.5194/tcd-6-125-2012