B23A:
How Do the Carbon Pumps Pump? Mechanisms of the Solubility and Biological Pumps II

Submit an Abstract to this Session

Session ID#: 11457

Session Description:
Cumulatively since pre-industrial times the ocean has absorbed 40% of anthropogenic carbon emissions, and thus has significantly modulated climate change. The ocean’s carbon uptake is mediated by subduction of carbon rich water (solubility pump) and by the export to depth of organic particles and dissolved organic carbon (biological carbon pump). There is much yet unknown about the underlying biological, chemical and physical mechanisms of these pumps, and thus, substantial uncertainty about the how ocean carbon cycling will evolve over the coming century. Developments in sensor technology, particle export techniques, global data compilations, time series observations, and modeling all are enabling new understanding of the carbon pumps and their potential for variability and change. Observational, experimental, empirical and modeling studies addressing the ocean carbon pumps are welcomed to this session.
Primary Chair:  Frederic A.C. Le Moigne, Aix Marseille Univ., Université Toulon, CNRS, IRD, MIO UM 110, Mediterranean Institute of Oceanography, Marseille, France, Marseille, France
Chairs:  Galen A McKinley, Columbia University and Lamont-Doherty Earth Observatory, New York, United States, Stephanie Henson, National Oceanography Centre, Southampton, United Kingdom and Nicole S Lovenduski, University of Colorado, Department of Atmospheric and Oceanic Sciences, Boulder, CO, United States
Moderators:  Galen A McKinley, University of Wisconsin - Madison, Madison, WI, United States and Nicole S Lovenduski, University of Colorado, Department of Atmospheric and Oceanic Sciences, Boulder, CO, United States
Student Paper Review Liaison:  Frederic A.C. Le Moigne, Aix Marseille Univ., Université Toulon, CNRS, IRD, MIO UM 110, Mediterranean Institute of Oceanography, Marseille, France, Marseille, France
Index Terms:

4805 Biogeochemical cycles, processes, and modeling [OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL]
4806 Carbon cycling [OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL]
4815 Ecosystems, structure, dynamics, and modeling [OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL]
4845 Nutrients and nutrient cycling [OCEANOGRAPHY: BIOLOGICAL AND CHEMICAL]
Co-Sponsor(s):
  • CT - Chemical Tracers, DOM and Trace Metals
  • ME - Marine Ecosystems
  • PC - Past, Present and Future Climate
  • PP - Phytoplankton and Primary Production

Abstracts Submitted to this Session:

Using Preformed and Remineralized Nutrients to Map Spatial Variation in Remineralization (91335)
Raffaele Bernardello1, Adrian Martin2, Samar Khatiwala3, Iris Kriest4, Stephanie Henson5, Jeff Blundell6, John P Dunne7, Mark M Moore8 and Andrew Yool2, (1)National Oceanography Centre, Ocean Biogeochemistry and Ecosystems, Southampton, United Kingdom, (2)National Oceanography Centre, Southampton, United Kingdom, (3)University of Oxford, Department of Earth Sciences, Oxford, United Kingdom, (4)GEOMAR, Kiel, Germany, (5)National Oceanography Centre, OBE, Southampton, United Kingdom, (6)National Oceanography Centre, University of Southampton, Ocean and Earth Science, Southampton, United Kingdom, (7)NOAA Geophysical Fluid Dynamics Laboratory, Princeton, United States, (8)University of Southampton, Ocean and Earth Science, Southampton, United Kingdom
The Role of Temperature and Oxygen for the Remineralization of Sinking Organic Matter (91756)
Charlotte Laufkotter1, Charles A Stock2 and John P Dunne2, (1)Princeton University, NOAA/Geophysical Fluid Dynamics Laboratory, Princeton, NJ, United States, (2)NOAA Geophysical Fluid Dynamics Laboratory, Princeton, United States
Tracer constraints on organic particle transfer efficiency to the deep ocean (93514)
Thomas S Weber, University of Washington Seattle Campus, School of Oceanography, Seattle, WA, United States, Jacob Adrian Cram, University of Maryland Center for Environmental Science, Cambridge, United States and Curtis A Deutsch, University of Washington, School of Oceanography, Seattle, WA, United States
The Seasonal Mixed-Layer Pump is a Major Source of Energy for the Mesopelagic Ocean (87557)
Giorgio Dall'Olmo1,2, James Dingle3, Luca Polimene4 and Robert J W Brewin3,5, (1)Plymouth Marine Laboratory, Plymouth, United Kingdom, (2)Plymouth marine Laboratory, National Centre for Earth Observation, Plymouth, United Kingdom, (3)Plymouth Marine Laboratory, EOSA, Plymouth, United Kingdom, (4)Plymouth Marine Laboratory, MEMP, Plymouth, United Kingdom, (5)College of Life and Environmental Sciences, University of Exeter, Penryn, United Kingdom
Influence of the biological pump on carbon uptake over the annual cycle across the North Pacific Ocean (88216)
Hilary I Palevsky, Boston College, Earth and Environmental Sciences, Chestnut Hill, United States and Paul Quay, University of Washington, School of Oceanography, Seattle, WA, United States
The impact of resolving mesoscale eddies on the biological pump and the associated planktonic community structure in an earth system model. (92841)
Cheryl S Harrison, Louisiana State University, Department of Oceanography & Coastal Sciences, Baton Rouge, LA, United States, Matthew C Long, [C]Worthy, LLC, Boulder, United States and Peter Gaube, Applied Physics Laboratory University of Washington, Seattle, United States
Detectability of Change in the Ocean Carbon Sink (90392)
Galen A McKinley1, Darren Pilcher2, Amanda R Fay1, Keith T Lindsay3, Matthew C Long4 and Nicole S Lovenduski5, (1)University of Wisconsin - Madison, Madison, WI, United States, (2)University of Wisconsin Madison, Madison, United States, (3)National Center for Atmospheric Research, Boulder, CO, United States, (4)[C]Worthy, LLC, Boulder, United States, (5)University of Colorado, Department of Atmospheric and Oceanic Sciences, Boulder, CO, United States
The calcium carbonate counter pump: Fundamentals, evolution through time, and future feedbacks (88844)
Richard E Zeebe, University of Hawai'i at Mānoa, Oceanography, Honolulu, United States