The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM) ...
Observations show robust changes in the circulation, temperature, and salinity of the Southern Ocean in recent decades. To what extent these changes are related to the formation of the ozone hole in the late twentieth century is an open question. Using a comprehensive chemistry-climate Earth system...
Main Authors: | , , , |
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Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Columbia University
2015
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Subjects: | |
Online Access: | https://dx.doi.org/10.7916/d8qz29tf https://academiccommons.columbia.edu/doi/10.7916/D8QZ29TF |
_version_ | 1821717665671020544 |
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author | Solomon, Abraham L. Polvani, Lorenzo M. Abernathey, Ryan Patrick Smith, Karen L. |
author_facet | Solomon, Abraham L. Polvani, Lorenzo M. Abernathey, Ryan Patrick Smith, Karen L. |
author_sort | Solomon, Abraham L. |
collection | DataCite |
description | Observations show robust changes in the circulation, temperature, and salinity of the Southern Ocean in recent decades. To what extent these changes are related to the formation of the ozone hole in the late twentieth century is an open question. Using a comprehensive chemistry-climate Earth system model, we contrast model runs with varying and with fixed surface concentrations of ozone depleting substances (ODS) from 1955 to 2005. In our model, ODS cause the majority of the summertime changes in surface wind stress which, in turn, induce a clear poleward shift of the ocean's meridional overturning circulation. In addition, more than 30% of the model changes in the temperature and salinity of the Southern Ocean are caused by ODS. These findings offer unambiguous evidence that increased concentrations of ODS in the late twentieth century are likely to have been been an important driver of changes in the Southern Ocean. ... |
format | Article in Journal/Newspaper |
genre | Southern Ocean |
genre_facet | Southern Ocean |
geographic | Southern Ocean |
geographic_facet | Southern Ocean |
id | ftdatacite:10.7916/d8qz29tf |
institution | Open Polar |
language | unknown |
op_collection_id | ftdatacite |
op_doi | https://doi.org/10.7916/d8qz29tf10.1002/2015gl064744 |
op_relation | https://dx.doi.org/10.1002/2015gl064744 |
publishDate | 2015 |
publisher | Columbia University |
record_format | openpolar |
spelling | ftdatacite:10.7916/d8qz29tf 2025-01-17T00:54:23+00:00 The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM) ... Solomon, Abraham L. Polvani, Lorenzo M. Abernathey, Ryan Patrick Smith, Karen L. 2015 https://dx.doi.org/10.7916/d8qz29tf https://academiccommons.columbia.edu/doi/10.7916/D8QZ29TF unknown Columbia University https://dx.doi.org/10.1002/2015gl064744 Ozone-depleting substances Ocean temperature Salinity--Environmental aspects Ozone layer depletion Atmospheric ozone Ocean circulation Atmosphere Meteorology Climatic changes Chemical oceanography Text article-journal Articles ScholarlyArticle 2015 ftdatacite https://doi.org/10.7916/d8qz29tf10.1002/2015gl064744 2024-10-01T11:38:12Z Observations show robust changes in the circulation, temperature, and salinity of the Southern Ocean in recent decades. To what extent these changes are related to the formation of the ozone hole in the late twentieth century is an open question. Using a comprehensive chemistry-climate Earth system model, we contrast model runs with varying and with fixed surface concentrations of ozone depleting substances (ODS) from 1955 to 2005. In our model, ODS cause the majority of the summertime changes in surface wind stress which, in turn, induce a clear poleward shift of the ocean's meridional overturning circulation. In addition, more than 30% of the model changes in the temperature and salinity of the Southern Ocean are caused by ODS. These findings offer unambiguous evidence that increased concentrations of ODS in the late twentieth century are likely to have been been an important driver of changes in the Southern Ocean. ... Article in Journal/Newspaper Southern Ocean DataCite Southern Ocean |
spellingShingle | Ozone-depleting substances Ocean temperature Salinity--Environmental aspects Ozone layer depletion Atmospheric ozone Ocean circulation Atmosphere Meteorology Climatic changes Chemical oceanography Solomon, Abraham L. Polvani, Lorenzo M. Abernathey, Ryan Patrick Smith, Karen L. The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM) ... |
title | The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM) ... |
title_full | The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM) ... |
title_fullStr | The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM) ... |
title_full_unstemmed | The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM) ... |
title_short | The impact of ozone depleting substances on the circulation, temperature, and salinity of the Southern Ocean: An attribution study with CESM1(WACCM) ... |
title_sort | impact of ozone depleting substances on the circulation, temperature, and salinity of the southern ocean: an attribution study with cesm1(waccm) ... |
topic | Ozone-depleting substances Ocean temperature Salinity--Environmental aspects Ozone layer depletion Atmospheric ozone Ocean circulation Atmosphere Meteorology Climatic changes Chemical oceanography |
topic_facet | Ozone-depleting substances Ocean temperature Salinity--Environmental aspects Ozone layer depletion Atmospheric ozone Ocean circulation Atmosphere Meteorology Climatic changes Chemical oceanography |
url | https://dx.doi.org/10.7916/d8qz29tf https://academiccommons.columbia.edu/doi/10.7916/D8QZ29TF |