Award Abstract # 0752972
Collaborative Research: Global Ocean Repeat Hydrography, Carbon, and Tracer Measurements, 2009-2014

NSF Org: OCE
Division Of Ocean Sciences
Recipient: UNIVERSITY OF MIAMI
Initial Amendment Date: January 26, 2009
Latest Amendment Date: February 19, 2014
Award Number: 0752972
Award Instrument: Continuing Grant
Program Manager: Eric C. Itsweire
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: February 1, 2009
End Date: January 31, 2016 (Estimated)
Total Intended Award Amount: $3,805,435.00
Total Awarded Amount to Date: $5,805,375.00
Funds Obligated to Date: FY 2009 = $1,864,939.00
FY 2011 = $1,939,088.00

FY 2013 = $1,005,307.00

FY 2014 = $996,041.00
History of Investigator:
  • Frank Millero (Principal Investigator)
    fmillero@rsmas.miami.edu
  • Dennis Hansell (Co-Principal Investigator)
Recipient Sponsored Research Office: University of Miami
1251 MEMORIAL DR
CORAL GABLES
FL  US  33146-2509
(305)421-4089
Sponsor Congressional District: 27
Primary Place of Performance: University of Miami
1251 MEMORIAL DR
CORAL GABLES
FL  US  33146-2509
Primary Place of Performance
Congressional District:
27
Unique Entity Identifier (UEI): KXN7HGCF6K91
Parent UEI: VNZZYCJ55TC4
NSF Program(s): PHYSICAL OCEANOGRAPHY,
Chemical Oceanography
Primary Program Source: 01000910DB NSF RESEARCH & RELATED ACTIVIT
01001112DB NSF RESEARCH & RELATED ACTIVIT

01001314DB NSF RESEARCH & RELATED ACTIVIT

01001415DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 0000, 1324, 1389, 4444, EGCH, OTHR
Program Element Code(s): 161000, 167000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Intellectual Merit: The systematic and global re-occupation of select hydrographic sections begun during 2003-2008 will be continued in the 2009-2014 period with the continued objective of quantifying changes in storage and transport of heat, fresh water, carbon dioxide (CO2) and related chemical parameters. The program is in support of CLIVAR (CLImate Variability and predictability) and the Carbon Science Programs, and is a component of a global observing system for the physical climate and carbon system. By integrating the scientific needs of the carbon, tracer and hydrographic communities, major scientific synergies and cost savings will continue to be achieved. In addition to efficiency, the coordinated approach produces scientific advances that exceed those of having individual programs. These advances continue to contribute to the following overlapping scientific objectives: Data for Model Calibration, Validation and Model Based Synthesis; Carbon System Studies; Heat and Freshwater Storage and Flux Studies; Deep and Shallow Water Mass and Ventilation Studies; and Calibration of Autonomous Sensors. A joint study of the ocean carbon cycle and circulation is helping to identify critical areas where potential changes in ocean circulation could have serious consequences for future anthropogenic uptake. Global warming-induced changes in the ocean?s transport of heat and freshwater, which could affect the circulation, are being followed through these long-term measurements. An average of two sections will be conducted every year, sometime collaboratively with international partner. The measurements made on each section include hydrography (full-depth vertical profiles of salinity, temperature, oxygen, nutrients, currents), Underway surface temperature, salinity, partial pressure of carbon dioxide (pCO2), air-sea fluxes, bathymetry, navigation), carbon system (dissolved inorganic carbon, pCO2. Total Alkalinity, pH, dissolved organic carbon and nitrogen), and transient tracers (CFCs, SF6, tritium/3He). This project will collect the data and perform the quality control measures routinely carried out by providers of reference-quality data. Post-cruise data updates, distribution, and archive will continue to be managed by groups with separate funding. This ongoing project is integrated with a larger international effort to monitor the ocean's response to climate change.

Broader Impacts: The results will be disseminated broadly to enhance scientific and technological understanding. The project is based on the fundamental concept that data collected belong to the community, and are available to the community at large rather than being proprietary for the investigators involved in the project. The data policy is stringent and geared towards rapid and open dissemination, with a clear structure for all data to undergo thorough quality control and transmission to a recognized data center. This ambitious degree of openness has resulted in rapid and widespread availability and use of the data. The project benefits to society include the collection of a high quality data set, and use of the data to assess climate change. The global program provides full water column data of climatically significant parameters with decadal coverage. These data are and will be used to assess climate change by quantifying the uptake and storage of anthropogenic CO2 by the ocean, and contributing to an understanding and models of the processes that control the uptake and transport of CO2 into the ocean's interior. Since these are likely to be the only systematic observations below 2000 m, they are and will be used to document long term trends in ocean warming, and heat and freshwater fluxes. The data will remain a resource for model calibration of the climate system. The project will continue to promote training and learning. It will continue to serve as a community resource for training and entraining graduate students, postdoctoral scientists, and new scientists in sea-going work. Outreach activities will continue as opportunities arise.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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(Showing: 1 - 10 of 109)
A.G. Dickson "Standards for ocean measurements" Oceanography , v.23(3) , 2010 , p.34
B. Boeher, P. Herzsprung, M. Schultze, and F.J. Millero "Calculating density of water in geochemical lake stratification models," Limnol. & Oceanogr.: Methods , v.8 , 2010 , p.567 10:4319/lom.2010.8.567
B. Casentini, M. Pettine and F.J. Millero "Release of arsenic from volcanic rocks through interactions with inorganic anions and organic ligands" Aquat. Geochem. , v.16 , 2010 , p.373 DOI 10.1007/s10498-010-9090-3
Burd, AB; Hansell, DA; Steinberg, DK: Anderson, TR; Ari�­stegui, J; Baltar, F; Beaupre, SR;Buesseler, KO; DeHairs, F; Jackson, GA; Kadko, DC; Koppelmann, R; Lampitt, RS; Nagata, T; Reinthaler, T; Robinson, C; Robison, BH; Tamburini, C; Tanaka, T "Assessing the Apparent Imbalance Between Geochemical and Biochemical Indicators of Meso- and Bathypelagic Biological Activity: What the @$#! is wrong with present calculations of carbon budgets?" Deep Sea Research II , v.57 , 2010 , p.1557
Bustos-Serrano, H; Morse, JW; Millero, FJ "The formation of whitings on the Little Bahama Bank" MARINE CHEMISTRY , v.113 , 2009 , p.1 View record at Web of Science 10.1016/j.marchem.2008.10.00
C.A. Carlson, D.A. Hansell, C. Tamburini C. "DOC persistence and its fate after export within the ocean interior. In: Jiao N, Azam F, Sanders S (eds). Microbial Carbon Pump in the Ocean" Science/AAAS Business Office , v.10.1126 , 2011 , p.57
C.A. Carlson, D.A. Hansell, C. Tamburini C., "DOC persistence and its fate after export within the ocean interior." Microbial Carbon Pump in the Ocean. Science / AAAS Business Office: Washington DC , 2011 , p.57-59 10.1126/science.opms.sb0001, 2011
Carlson, CA; Hansell, DA; Nelson, NB; Siegel, DA; Smethie Jr., WM; Khatiwala, S; Meyers, MM; Wallner, E "Dissolved organic carbon export and subsequent remineralization in the mesopelagic bathypelagic realms of the North Atlantic basin" Deep-Sea Research Part II , v.57 , 2010 , p.1433
Carter, B.R., J.A. Radich, H.L. Doyle, A.G. Dickson "An automated system for spectrophotometric seawater pH measurements." Limnol Oceanogr-Meth , v.11 , 2013 , p.16
Carter, B.R., Radich, J.A., Doyle, H.L. and Dickson, A.G "An automated system for spectrophotometric seawater pH measurements" Limn. and Oceanog.: Methods , v.11 , 2013 , p.16
C. Foti, G. Lando, F.J. Millero, and S. Sammartano "Experimental study and modeling of inorganic Cd2+ speciation in natural waters" Environ. Chem. , v.8 , 2011 , p.320 10.1071/EN10138
(Showing: 1 - 10 of 109)

PROJECT OUTCOMES REPORT

Disclaimer

This Project Outcomes Report for the General Public is displayed verbatim as submitted by the Principal Investigator (PI) for this award. Any opinions, findings, and conclusions or recommendations expressed in this Report are those of the PI and do not necessarily reflect the views of the National Science Foundation; NSF has not approved or endorsed its content.

Pubic Report for Carbon Measurement for the Global Ocean Ship-Based Hydrographic Investigations Program

Collaborative Research: Global Ocean Repeat Hydrography, Carbon, and Tracer Measurements, 2009-2014


Frank J. Millero, Principal Investigator
Rosenstiel School of Marine & Atmospheric Science
University of Miami
Miami, FL 33149
Email: fmillero@rsmas.miami.edu

This study is supported by the National Science Foundation and is part of the Global Ocean Ship-Based Hydrographic Investigations Program (GO-SHIP; http://www.go-ship.org), an international study of changes in the inorganic and organic content of ocean waters, with those changes observed on a 10 year cycle.  The ocean is a central component of Earth’s climate system and is taking up most of Earth’s excess anthropogenic heat and much of its anthropogenic carbon dioxide.  The ocean takes up about 27% of this anthropogenic carbon, resulting in acidification of the upper ocean.  The pH of surface ocean water is decreasing by 0.002 units per year from the normal value of 8.1. This lower pH makes it harder for organisms with calcite shells to grow, and it also affects the chemistry of the surface oceans.  The global ocean has continued to take up a substantial fraction of the anthropogenic carbon emissions from fossil fuel combustion and from deforestation and it is therefore a major mediator of global climate change; this uptake is observed and assessed in our field work.  Some of the carbon entering the ocean is converted to organic matter by the plants growing there.  A byproduct of this growth is the release of organic molecules to the water, where they accumulate for thousands of years.  With an inventory of almost 700 billion tons of carbon in the ocean, this material is one of Earth’s major carbon reservoirs.  Understanding the distributions, production and consumption of this material is a central goal of our research.

 


Last Modified: 02/03/2016
Modified by: Frank J Millero

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