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The freshwater composition of the Fram Strait outflow derived from a decade of tracer measurements

The freshwater composition of the Fram Strait outflow derived from a decade of tracer measurements
The freshwater composition of the Fram Strait outflow derived from a decade of tracer measurements
The composition of the Fram Strait freshwater outflow is investigated by comparing 10 sections of concurrent salinity, ?18O, nitrate and phosphate measurements collected between 1997 and 2011. The largest inventories of net sea ice meltwater are found in 2009, 2010 and 2011. The 2009–2011 sections are also the first to show positive fractions of sea ice meltwater at the surface near the core of the EGC. Sections from September 2009–2011 show an increased input of sea ice meltwater at the surface relative to older September sections. This suggests that more sea ice now melts back into the surface in late summer than previously. Comparison of April, July and September sections reveals seasonal variations in the inventory of positive sea ice meltwater, with maximum inventories in September sections. The time series of sections reveals a strong anti-correlation between meteoric water and net sea ice meltwater inventories, suggesting that meteoric water and brine may be delivered to Fram Strait together from a common source. We find that the freshwater outflow at Fram Strait exhibits a similar meteoric water to net sea ice meltwater ratio as the central Arctic Ocean and Siberian shelves, suggesting that much of the sea ice meltwater and meteoric water at Fram Strait may originate from these regions. However, we also find that the ratio of meteoric water to sea ice meltwater inventories at Fram Strait is decreasing with time, due to an increased surface input of sea ice meltwater in recent sections.
0148-0227
C11005
Dodd, Paul A.
b186d680-b9c8-457d-8e9a-fef7d90481cd
Rabe, Benjamin
b6b25c05-4e93-4f1e-9679-42999b98c453
Hansen, Edmond
5227618e-7dff-456b-ba33-b16454fd1cfe
Falck, Eva
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Mackensen, Andreas
6d2cc458-fa3e-402d-a69a-13a519dbd5a1
Rohling, Eelco
a2a27ef2-fcce-4c71-907b-e692b5ecc685
Stedmon, Colin
01b7a587-7a38-4957-83c5-ec964d657b6c
Kristiansen, Svein
678bc3ad-83df-462a-a580-8f06f0ae194f
Dodd, Paul A.
b186d680-b9c8-457d-8e9a-fef7d90481cd
Rabe, Benjamin
b6b25c05-4e93-4f1e-9679-42999b98c453
Hansen, Edmond
5227618e-7dff-456b-ba33-b16454fd1cfe
Falck, Eva
2a331a7b-0287-4291-a0b6-1d2497c09e2d
Mackensen, Andreas
6d2cc458-fa3e-402d-a69a-13a519dbd5a1
Rohling, Eelco
a2a27ef2-fcce-4c71-907b-e692b5ecc685
Stedmon, Colin
01b7a587-7a38-4957-83c5-ec964d657b6c
Kristiansen, Svein
678bc3ad-83df-462a-a580-8f06f0ae194f

Dodd, Paul A., Rabe, Benjamin, Hansen, Edmond, Falck, Eva, Mackensen, Andreas, Rohling, Eelco, Stedmon, Colin and Kristiansen, Svein (2012) The freshwater composition of the Fram Strait outflow derived from a decade of tracer measurements. Journal of Geophysical Research, 117 (C11), C11005. (doi:10.1029/2012JC008011).

Record type: Article

Abstract

The composition of the Fram Strait freshwater outflow is investigated by comparing 10 sections of concurrent salinity, ?18O, nitrate and phosphate measurements collected between 1997 and 2011. The largest inventories of net sea ice meltwater are found in 2009, 2010 and 2011. The 2009–2011 sections are also the first to show positive fractions of sea ice meltwater at the surface near the core of the EGC. Sections from September 2009–2011 show an increased input of sea ice meltwater at the surface relative to older September sections. This suggests that more sea ice now melts back into the surface in late summer than previously. Comparison of April, July and September sections reveals seasonal variations in the inventory of positive sea ice meltwater, with maximum inventories in September sections. The time series of sections reveals a strong anti-correlation between meteoric water and net sea ice meltwater inventories, suggesting that meteoric water and brine may be delivered to Fram Strait together from a common source. We find that the freshwater outflow at Fram Strait exhibits a similar meteoric water to net sea ice meltwater ratio as the central Arctic Ocean and Siberian shelves, suggesting that much of the sea ice meltwater and meteoric water at Fram Strait may originate from these regions. However, we also find that the ratio of meteoric water to sea ice meltwater inventories at Fram Strait is decreasing with time, due to an increased surface input of sea ice meltwater in recent sections.

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More information

Published date: 2012
Organisations: Paleooceanography & Palaeoclimate

Identifiers

Local EPrints ID: 346812
URI: http://eprints.soton.ac.uk/id/eprint/346812
ISSN: 0148-0227
PURE UUID: 8a0c5edd-962d-4121-996d-463bccf4ed0b
ORCID for Eelco Rohling: ORCID iD orcid.org/0000-0001-5349-2158

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Date deposited: 09 Jan 2013 12:07
Last modified: 15 Mar 2024 02:47

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Contributors

Author: Paul A. Dodd
Author: Benjamin Rabe
Author: Edmond Hansen
Author: Eva Falck
Author: Andreas Mackensen
Author: Eelco Rohling ORCID iD
Author: Colin Stedmon
Author: Svein Kristiansen

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