Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope
A series of cross-slope transects were occupied in 2013 and 2015 that extended eastward from St. Anna Trough to the Lomonosov Ridge. High-resolution physical and chemical observations collected along these transects revealed fronts in the potential temperature and the stable oxygen isotopic rati...
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doaj-ca60093dc06b4d02b2acbf1d62ae7c112020-11-25T01:50:52ZengCopernicus PublicationsOcean Science1812-07841812-07922017-11-011398399510.5194/os-13-983-2017Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slopeM. B. Alkire0I. Polyakov1R. Rember2A. Pnyushkov3V. Ivanov4V. Ivanov5I. Ashik6Applied Physics Laboratory, University of Washington, Seattle, WA, USAInternational Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, USAInternational Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, USAInternational Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, USAInternational Arctic Research Center, University of Alaska Fairbanks, Fairbanks, AK, USAArctic and Antarctic Research Institute, St. Petersburg, RussiaArctic and Antarctic Research Institute, St. Petersburg, RussiaA series of cross-slope transects were occupied in 2013 and 2015 that extended eastward from St. Anna Trough to the Lomonosov Ridge. High-resolution physical and chemical observations collected along these transects revealed fronts in the potential temperature and the stable oxygen isotopic ratio (<i>δ</i><sup>18</sup>O) that were observed north of Severnaya Zemlya (SZ). Using linear regressions, we describe mixing regimes on either side of the front that characterize a transition from a seasonal halocline to a permanent halocline. This transition describes the formation of lower halocline water (LHW) and the cold halocline layer via a mechanism that has been previously postulated by Rudels et al. (1996). Initial freshening of Atlantic Water (AW) by sea-ice meltwater occurs west of SZ, whereas higher influences of meteoric water and brine result in a transition to a separate mixing regime that alters LHW through mixing with overlying waters and shifts the characteristic temperature–salinity bend from higher (34.4 ≤ <i>S</i> ≤ 34.5) toward lower (34.2 ≤ <i>S</i> ≤ 34.3) salinities. These mixing regimes appear to have been robust since at least 2000.https://www.ocean-sci.net/13/983/2017/os-13-983-2017.pdf |
collection |
DOAJ |
language |
English |
format |
Article |
sources |
DOAJ |
author |
M. B. Alkire I. Polyakov R. Rember A. Pnyushkov V. Ivanov V. Ivanov I. Ashik |
spellingShingle |
M. B. Alkire I. Polyakov R. Rember A. Pnyushkov V. Ivanov V. Ivanov I. Ashik Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope Ocean Science |
author_facet |
M. B. Alkire I. Polyakov R. Rember A. Pnyushkov V. Ivanov V. Ivanov I. Ashik |
author_sort |
M. B. Alkire |
title |
Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope |
title_short |
Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope |
title_full |
Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope |
title_fullStr |
Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope |
title_full_unstemmed |
Combining physical and geochemical methods to investigate lower halocline water formation and modification along the Siberian continental slope |
title_sort |
combining physical and geochemical methods to investigate lower halocline water formation and modification along the siberian continental slope |
publisher |
Copernicus Publications |
series |
Ocean Science |
issn |
1812-0784 1812-0792 |
publishDate |
2017-11-01 |
description |
A series of cross-slope transects were occupied in 2013 and 2015
that extended eastward from St. Anna Trough to the Lomonosov Ridge.
High-resolution physical and chemical observations collected along these
transects revealed fronts in the potential temperature and the stable oxygen
isotopic ratio (<i>δ</i><sup>18</sup>O) that were observed north of Severnaya
Zemlya (SZ). Using linear regressions, we describe mixing regimes on either
side of the front that characterize a transition from a seasonal halocline to
a permanent halocline. This transition describes the formation of lower
halocline water (LHW) and the cold halocline layer via a mechanism that has
been previously postulated by Rudels et al. (1996). Initial freshening of
Atlantic Water (AW) by sea-ice meltwater occurs west of SZ, whereas higher
influences of meteoric water and brine result in a transition to a separate
mixing regime that alters LHW through mixing with overlying waters and shifts
the characteristic temperature–salinity bend from higher
(34.4 ≤ <i>S</i> ≤ 34.5) toward lower
(34.2 ≤ <i>S</i> ≤ 34.3) salinities. These mixing regimes appear to
have been robust since at least 2000. |
url |
https://www.ocean-sci.net/13/983/2017/os-13-983-2017.pdf |
work_keys_str_mv |
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