Sea Ice Formation, Glacial Melt and the Solubility Pump Boundary Conditions in the Ross Sea

Seasonal formation of Dense Shelf Water (DSW) in the Ross Sea is a direct precursor to Antarctic Bottom Water, which fills the deep ocean with atmospheric gases in what composes the southern limb of the solubility pump. Measurements of seawater noble gas concentrations during katabatic wind events i...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Loose, Brice, Stammerjohn, Sharon, Sedwick, Peter, Ackley, Stephen
Format: Text
Language:unknown
Published: DigitalCommons@URI 2023
Subjects:
Online Access:https://digitalcommons.uri.edu/gsofacpubs/1829
https://doi.org/10.1029/2022JC019322
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spelling ftunivrhodeislan:oai:digitalcommons.uri.edu:gsofacpubs-2799 2024-01-21T10:00:49+01:00 Sea Ice Formation, Glacial Melt and the Solubility Pump Boundary Conditions in the Ross Sea Loose, Brice Stammerjohn, Sharon Sedwick, Peter Ackley, Stephen 2023-08-01T07:00:00Z https://digitalcommons.uri.edu/gsofacpubs/1829 https://doi.org/10.1029/2022JC019322 unknown DigitalCommons@URI https://digitalcommons.uri.edu/gsofacpubs/1829 doi:10.1029/2022JC019322 https://doi.org/10.1029/2022JC019322 Graduate School of Oceanography Faculty Publications air/sea exchange dense shelf water noble gases polynya solubility pump text 2023 ftunivrhodeislan https://doi.org/10.1029/2022JC019322 2023-12-25T19:10:01Z Seasonal formation of Dense Shelf Water (DSW) in the Ross Sea is a direct precursor to Antarctic Bottom Water, which fills the deep ocean with atmospheric gases in what composes the southern limb of the solubility pump. Measurements of seawater noble gas concentrations during katabatic wind events in two Ross Sea polynyas reveal the physical processes that determine the boundary value properties for DSW. This decomposition reveals 5–6 g kg−1 of glacial meltwater in DSW and sea-ice production rates of up to 14 m yr−1 within the Terra Nova Bay polynya. Despite winds upwards of 35 m s−1 during the observations, air bubble injection had a minimal contribution to gas exchange, accounting for less than 0.01 μmols kg−1 of argon in seawater. This suggests the slurry of frazil ice and seawater at the polynya surface inhibits air-sea exchange. Most noteworthy is the revelation that sea-ice formation and glacial melt contribute significantly to the ventilation of DSW, restoring 10% of the gas deficit for krypton, 24% for argon, and 131% for neon, while diffusive gas exchange contributes the remainder. These measurements reveal a cryogenic component to the solubility pump and demonstrate that while sea ice blocks air-sea exchange, sea ice formation and glacial melt partially offset this effect via addition of gases. While polynyas are a small surface area, they represent an important ventilation site within the southern-overturning cell, suggesting that ice processes both enhance and hinder the solubility pump. Text Antarc* Antarctic Ross Sea Sea ice University of Rhode Island: DigitalCommons@URI Antarctic Ross Sea Terra Nova Bay Journal of Geophysical Research: Oceans 128 8
institution Open Polar
collection University of Rhode Island: DigitalCommons@URI
op_collection_id ftunivrhodeislan
language unknown
topic air/sea exchange
dense shelf water
noble gases
polynya
solubility pump
spellingShingle air/sea exchange
dense shelf water
noble gases
polynya
solubility pump
Loose, Brice
Stammerjohn, Sharon
Sedwick, Peter
Ackley, Stephen
Sea Ice Formation, Glacial Melt and the Solubility Pump Boundary Conditions in the Ross Sea
topic_facet air/sea exchange
dense shelf water
noble gases
polynya
solubility pump
description Seasonal formation of Dense Shelf Water (DSW) in the Ross Sea is a direct precursor to Antarctic Bottom Water, which fills the deep ocean with atmospheric gases in what composes the southern limb of the solubility pump. Measurements of seawater noble gas concentrations during katabatic wind events in two Ross Sea polynyas reveal the physical processes that determine the boundary value properties for DSW. This decomposition reveals 5–6 g kg−1 of glacial meltwater in DSW and sea-ice production rates of up to 14 m yr−1 within the Terra Nova Bay polynya. Despite winds upwards of 35 m s−1 during the observations, air bubble injection had a minimal contribution to gas exchange, accounting for less than 0.01 μmols kg−1 of argon in seawater. This suggests the slurry of frazil ice and seawater at the polynya surface inhibits air-sea exchange. Most noteworthy is the revelation that sea-ice formation and glacial melt contribute significantly to the ventilation of DSW, restoring 10% of the gas deficit for krypton, 24% for argon, and 131% for neon, while diffusive gas exchange contributes the remainder. These measurements reveal a cryogenic component to the solubility pump and demonstrate that while sea ice blocks air-sea exchange, sea ice formation and glacial melt partially offset this effect via addition of gases. While polynyas are a small surface area, they represent an important ventilation site within the southern-overturning cell, suggesting that ice processes both enhance and hinder the solubility pump.
format Text
author Loose, Brice
Stammerjohn, Sharon
Sedwick, Peter
Ackley, Stephen
author_facet Loose, Brice
Stammerjohn, Sharon
Sedwick, Peter
Ackley, Stephen
author_sort Loose, Brice
title Sea Ice Formation, Glacial Melt and the Solubility Pump Boundary Conditions in the Ross Sea
title_short Sea Ice Formation, Glacial Melt and the Solubility Pump Boundary Conditions in the Ross Sea
title_full Sea Ice Formation, Glacial Melt and the Solubility Pump Boundary Conditions in the Ross Sea
title_fullStr Sea Ice Formation, Glacial Melt and the Solubility Pump Boundary Conditions in the Ross Sea
title_full_unstemmed Sea Ice Formation, Glacial Melt and the Solubility Pump Boundary Conditions in the Ross Sea
title_sort sea ice formation, glacial melt and the solubility pump boundary conditions in the ross sea
publisher DigitalCommons@URI
publishDate 2023
url https://digitalcommons.uri.edu/gsofacpubs/1829
https://doi.org/10.1029/2022JC019322
geographic Antarctic
Ross Sea
Terra Nova Bay
geographic_facet Antarctic
Ross Sea
Terra Nova Bay
genre Antarc*
Antarctic
Ross Sea
Sea ice
genre_facet Antarc*
Antarctic
Ross Sea
Sea ice
op_source Graduate School of Oceanography Faculty Publications
op_relation https://digitalcommons.uri.edu/gsofacpubs/1829
doi:10.1029/2022JC019322
https://doi.org/10.1029/2022JC019322
op_doi https://doi.org/10.1029/2022JC019322
container_title Journal of Geophysical Research: Oceans
container_volume 128
container_issue 8
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