Year-round observations of carbon biomass and flux variability in the Southern Ocean
Three Carbon Explorer (CE) floats profiling to kilometer depths in the Southern Ocean tracked dawn-dusk variations of mixing/stratification, particulate organic carbon (POC), and light scattering and sedimentation at 100, 250, and 800 m continuously from January 2002 to April 2003. Data were analyze...
Published in: | Global Biogeochemical Cycles |
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Lawrence Berkeley National Laboratory
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Online Access: | https://doi.org/10.1029/2008GB003206 https://digital.library.unt.edu/ark:/67531/metadc930086/ |
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ftunivnotexas:info:ark/67531/metadc930086 2023-05-15T18:24:41+02:00 Year-round observations of carbon biomass and flux variability in the Southern Ocean Bishop, James K.B. Wood, Todd Lawrence Berkeley National Laboratory. Earth Sciences Division. 2009-02-01 Text https://doi.org/10.1029/2008GB003206 https://digital.library.unt.edu/ark:/67531/metadc930086/ English eng Lawrence Berkeley National Laboratory rep-no: LBNL-1674E grantno: DE-AC02-05CH11231 doi:10.1029/2008GB003206 osti: 952854 https://digital.library.unt.edu/ark:/67531/metadc930086/ ark: ark:/67531/metadc930086 Journal Name: Global Biogeochemical Cycles Biomass Light Scattering 58 54 Exports Phytoplankton Sedimentation Particulates Transients Satellites Carbon Chlorophyll Zooplankton Stratification Article 2009 ftunivnotexas https://doi.org/10.1029/2008GB003206 2017-09-30T22:08:02Z Three Carbon Explorer (CE) floats profiling to kilometer depths in the Southern Ocean tracked dawn-dusk variations of mixing/stratification, particulate organic carbon (POC), and light scattering and sedimentation at 100, 250, and 800 m continuously from January 2002 to April 2003. Data were analyzed in conjunction with contemporaneous satellite winds and chlorophyll and derived subsurface light fields. The CE deployed at 66{sup o}S 172{sup o}W operated in the ice edge zone in absence of light. Two CEs deployed at 55{sup o}S 172{sup o}W recorded wintertime mixing to {approx}400 m, yet observed very different bloom dynamics and sedimentation the following spring. Four hypotheses are explored. The strongest is that shallow transient stratification of the deep winter mixed layer to shallower than photosynthetic critical depth occurred more frequently in the non-bloom/higher sedimentation case. The lower particle export to 800 m under the bloom was hypothesized to be due to higher interception of sinking carbon by a relatively starved over wintering zooplankton population. In the Southern Ocean surface phytoplankton biomass may counter indicate particle flux at kilometer depths. Article in Journal/Newspaper Southern Ocean University of North Texas: UNT Digital Library Southern Ocean Global Biogeochemical Cycles 23 2 n/a n/a |
institution |
Open Polar |
collection |
University of North Texas: UNT Digital Library |
op_collection_id |
ftunivnotexas |
language |
English |
topic |
Biomass Light Scattering 58 54 Exports Phytoplankton Sedimentation Particulates Transients Satellites Carbon Chlorophyll Zooplankton Stratification |
spellingShingle |
Biomass Light Scattering 58 54 Exports Phytoplankton Sedimentation Particulates Transients Satellites Carbon Chlorophyll Zooplankton Stratification Bishop, James K.B. Wood, Todd Year-round observations of carbon biomass and flux variability in the Southern Ocean |
topic_facet |
Biomass Light Scattering 58 54 Exports Phytoplankton Sedimentation Particulates Transients Satellites Carbon Chlorophyll Zooplankton Stratification |
description |
Three Carbon Explorer (CE) floats profiling to kilometer depths in the Southern Ocean tracked dawn-dusk variations of mixing/stratification, particulate organic carbon (POC), and light scattering and sedimentation at 100, 250, and 800 m continuously from January 2002 to April 2003. Data were analyzed in conjunction with contemporaneous satellite winds and chlorophyll and derived subsurface light fields. The CE deployed at 66{sup o}S 172{sup o}W operated in the ice edge zone in absence of light. Two CEs deployed at 55{sup o}S 172{sup o}W recorded wintertime mixing to {approx}400 m, yet observed very different bloom dynamics and sedimentation the following spring. Four hypotheses are explored. The strongest is that shallow transient stratification of the deep winter mixed layer to shallower than photosynthetic critical depth occurred more frequently in the non-bloom/higher sedimentation case. The lower particle export to 800 m under the bloom was hypothesized to be due to higher interception of sinking carbon by a relatively starved over wintering zooplankton population. In the Southern Ocean surface phytoplankton biomass may counter indicate particle flux at kilometer depths. |
author2 |
Lawrence Berkeley National Laboratory. Earth Sciences Division. |
format |
Article in Journal/Newspaper |
author |
Bishop, James K.B. Wood, Todd |
author_facet |
Bishop, James K.B. Wood, Todd |
author_sort |
Bishop, James K.B. |
title |
Year-round observations of carbon biomass and flux variability in the Southern Ocean |
title_short |
Year-round observations of carbon biomass and flux variability in the Southern Ocean |
title_full |
Year-round observations of carbon biomass and flux variability in the Southern Ocean |
title_fullStr |
Year-round observations of carbon biomass and flux variability in the Southern Ocean |
title_full_unstemmed |
Year-round observations of carbon biomass and flux variability in the Southern Ocean |
title_sort |
year-round observations of carbon biomass and flux variability in the southern ocean |
publisher |
Lawrence Berkeley National Laboratory |
publishDate |
2009 |
url |
https://doi.org/10.1029/2008GB003206 https://digital.library.unt.edu/ark:/67531/metadc930086/ |
geographic |
Southern Ocean |
geographic_facet |
Southern Ocean |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
Journal Name: Global Biogeochemical Cycles |
op_relation |
rep-no: LBNL-1674E grantno: DE-AC02-05CH11231 doi:10.1029/2008GB003206 osti: 952854 https://digital.library.unt.edu/ark:/67531/metadc930086/ ark: ark:/67531/metadc930086 |
op_doi |
https://doi.org/10.1029/2008GB003206 |
container_title |
Global Biogeochemical Cycles |
container_volume |
23 |
container_issue |
2 |
container_start_page |
n/a |
op_container_end_page |
n/a |
_version_ |
1766205493047459840 |