Award Abstract # 1048926
Collaborative Research Type 2 - MOBY: Modeling Ocean Variability and Biogeochemical Cycles

NSF Org: OCE
Division Of Ocean Sciences
Recipient: MASSACHUSETTS INSTITUTE OF TECHNOLOGY
Initial Amendment Date: February 24, 2011
Latest Amendment Date: February 24, 2011
Award Number: 1048926
Award Instrument: Standard Grant
Program Manager: Baris Uz
bmuz@nsf.gov
 (703)292-4557
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: March 1, 2011
End Date: February 28, 2018 (Estimated)
Total Intended Award Amount: $2,633,961.00
Total Awarded Amount to Date: $2,633,961.00
Funds Obligated to Date: FY 2011 = $2,633,961.00
History of Investigator:
  • John Marshall (Principal Investigator)
    jmarsh@mit.edu
  • Glenn Flierl (Co-Principal Investigator)
  • Michael Follows (Co-Principal Investigator)
  • Raffaele Ferrari (Co-Principal Investigator)
  • Stephanie Dutkiewicz (Co-Principal Investigator)
Recipient Sponsored Research Office: Massachusetts Institute of Technology
77 MASSACHUSETTS AVE
CAMBRIDGE
MA  US  02139-4301
(617)253-1000
Sponsor Congressional District: 07
Primary Place of Performance: Massachusetts Institute of Technology
77 MASSACHUSETTS AVE
CAMBRIDGE
MA  US  02139-4301
Primary Place of Performance
Congressional District:
07
Unique Entity Identifier (UEI): E2NYLCDML6V1
Parent UEI: E2NYLCDML6V1
NSF Program(s): ANT Ocean & Atmos Sciences,
CR, Earth System Models
Primary Program Source: 01001112DB NSF RESEARCH & RELATED ACTIVIT
0100XXXXDB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 8012
Program Element Code(s): 511300, 801200
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Intellectual Merit: This project (MOBY) focuses on decadal predictability of the ocean component of the climate system, both in its physical and biogeochemical aspects. It will advance understanding of the coupled physical, chemical and biological processes in the ocean that respond to, and feedback on, the global climate. Physical and biogeochemical activity on the mesoscale, the scale at which most of the kinetic energy in the ocean resides, is thought to play a major role in controlling the ability of the ocean to sequester heat and carbon in to its interior on interannual to decadal timescales. The mesoscale and its interaction with biogeochemical cycles must therefore be either resolved, or understood and parameterized, before we can have confidence in decadal climate predictions. The current generation of ocean climate models, however, do not resolve the mesoscale, and, if they represent biogeochemistry at all, only a few 'compartments' are included.

To address this challenge, scientists at the Massachusetts Institute of Technology, Woods Hole Oceanographic Institution, and the National Center for Atmospheric Research, propose a multi-scale modeling approach in which regional, high-resolution models are embedded in global, coarser-scale ocean models. The resulting numerical 'zoom lenses' will be deployed in key regions of climate variability in an attempt to resolve the mesoscale and submesoscale environment experienced by ocean ecosystems, but embedded in a global model. Then, models of biogeochemical cycles will be overlain to study the interaction of ecosystems with fully-resolved mesoscale turbulence. 'Self-assembling' ecosystem models will be employed that have the capacity to represent the response of the ecosystem to the changing environment and modes of variability. Finally, the integrated effects on heat/carbon uptake, and ecosystem community structure will be studied. The global context of these calculations will allow plausible inferences to be made about the rectified effects of mesoscale physical, chemical and biological interactions and inform strategies to parameterize them in the coarser-resolution coupled climate models used in projections of decadal variability and climate change.

These overlapping activities will be focused on three regions of strong natural variability where there is vigorous small-scale variability: the equatorial Pacific, the Southern Ocean and the subtropical northwest Atlantic. The associated modes of variability are ENSO, the Southern Annular Mode (SAM), and North Atlantic Oscillation (NAO), respectively.

Broader Impacts: The proposed research is key to our understanding and modeling the ocean and life within it, the evolution of life within the ocean over earth history, the global cycle of carbon and nutrients, the conservation and exploitation of the ocean's natural resources, management of fisheries, geoengineering (to inform decisions about the pros and cons of attempting to ameliorate anthropogenic impacts) and ocean acidification, among many other grand challenges. These collaborative efforts will provide training and learning opportunities to the graduate and undergraduate students participating in the research. A current Ph.D. student in the MIT/WHOI Joint Program will be supported by this project, along with two further students. The investigators will also attempt to entrain undergraduates into the project through the WHOI Summer Student Fellowship/NSF Research Experience for Undergraduates program. Finally, in addition to yearly group meetings of the project participants (students, post-docs and scientists from the three collaborating institutions), two-day 'community workshops' in years 2 and 4 of the project will be held to inform, and be informed by a wider group of scientists working on the broad science themes embraced by the MOBY project.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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(Showing: 1 - 10 of 15)
Barton, A.D., B.A. Ward, R.G. Williams, and M.J. Follows "The impact of fine-scale turbulence on phytoplankton community structure" Limnology and Oceanography: Fluids and Environments , v.4 , 2014 DOI 10.1215/21573689-2651533
Bates, M., Tulloch, R., Marshall, J., and Ferrari, R. "Rationalizing the Spatial Distribution of Mesoscale Eddy Diffusivity in Terms of Mixing Length Theory" Journal of Physical Oceanography , v.44 , 2014 doi: http://dx.doi.org/10.1175/JPO-D-13-0130.1
Clayton, S., S. Dutkiewicz , O. Jahn, and M.J. Follows "Dispersal, eddies, and the diversity of marine phytoplankton" Limnology and Oceanography: Fluids and Environment , v.3 , 2013 doi:10.1215/21573689-2373515
Clayton, S., T. Nagai and M.J. Follows "Fine scale phytoplankton community structure across the Kuroshio Front" Journal of Plankton Research , 2014 10.1093/plankt/fbu020
Dutkiewicz, S. B.A. Ward, J.R. Scott, and M.J. Follows "Understanding Predicted Shifts in Diazotroph Biogeography using Resource Competition Theory" Biogeosciences , v.11 , 2014 10.5194/bg-11-5445-2014
Illari, L., Marshall, J., and McKenna, W.D. "Virtually Enhanced Fluid Laboratories for Teaching Meteorology" Bulletin of the American Meteorological Society , 2017 doi = 10.1175/BAMS-D-16-0075.1
Ito, T., and M.J. Follows "Air-sea disequilibrium of carbon dioxide enhances the biological carbon sequestration in the Southern Ocean" Global Biogeochem. Cycles , v.27 , 2013 doi:10.1002/2013GB004682
LaCasce, J.H., Ferrari, R., Marshall, J., Tulloch, R., Balwada, D. and Speer, K "Float-derived isopycnal diffusivities in the DIMES experiment" J. Phys. Oceanogr. , v.44 , 2014 doi: http://dx.doi.org/10.1175/JPO-D-13-0175.1
Levy, M., O. Jahn, S. Dutkiewicz, and M.J. Follows "Phytoplankton diversity and community structure affected by oceanic disperal and mesoscale turbulence." Limnology and Oceanography: Fluids and Environment , v.4 , 2014 0.1215/21573869-2768549
Lovenduski, N. S., M. C. Long, P. R. Gent, and K. Lindsay. "Multi-decadal trends in the advection and mixing of natural carbon in the Southern Ocean" Geophy. Res. Lett., , v.40 , 2013 , p.1-4 10.1029/2012GL054483
Luo, Y.-W., Doney, S.C., Anderson, L.A., Benavides, M., Berman-Frank, I., Bode, A., Bonnet, S., Boström, K.H., Böttjer, D., Capone, D.G., Carpenter, E.J., Chen, Y.L., Church, M.J., Dore, J.E., Falcón, L.I., Fernández, A., Foster, R.A., Furuya, K., Gómez, "Database of diazotrophs in global ocean: abundance, biomass and nitrogen fixation rates." Earth System Science Data , v.4 , 2012 , p.47-73 10.5194/essd-4-47-2012
(Showing: 1 - 10 of 15)

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.

The MOBY (Modeling Ocean Variability and Biogeochemical Cycles) project was a collaboration between scientists at MIT, Woods Hole and NCAR, which focused on decadal predictability of the ocean component of the climate system, both in its physical and biogeochemical aspects. It advanced our understanding of the coupled physical, chemical and biological processes in the ocean and how it responds to, and feedback on, the global climate.

The ocean is full of small-scale eddying motions akin to the Atmosphere’s weather systems, but instead of being 1000’s in horizontal scale, they are 100km or so. This, so-called, ‘mesoscale’ -  the scale at which most of the kinetic energy in the ocean resides - is thought to play a major role in controlling the ability of the ocean to sequester heat and carbon in to its interior on interannual to decadal timescales. The mesoscale and its interaction with biogeochemical cycles must therefore be either resolved, or understood and parameterized, before we can have confidence in decadal climate predictions. The current generation of ocean climate models, however, do not resolve the mesoscale, and, if they represent biogeochemistry at all, only a few ‘compartments’ are included.

To address this challenge the MOBY project deployed a multi-scale modeling approach in which:

1. regional, high-resolution models were embedded in to global, coarser-scale ocean models in an attempt to resolve the mesoscale and submesoscale environment experienced by ocean ecosystems, but embedded in a global model.

2. models of biogeochemical cycles were overlain to study the interaction of ecosystems with fully-resolved mesoscale turbulence. ‘Self-assembling’ ecosystem models were employed that have the capacity to represent the response of the ecosystem to the changing environment and modes of variability,

3. the integrated effects on heat/carbon uptake, and ecosystem community structure were studied to inform strategies to parameterize them in the coarser-resolution coupled climate models used in projections of decadal variability and climate change.

Two regions of the ocean were the main focus of the activity, the Southern Ocean and, latterly, the tropical Pacific.

Outreach activities to the public involved the development of laboratory experiments and a ‘virtual lab’ that illustrate aspects of tropical dynamics.


Last Modified: 05/04/2018
Modified by: John C Marshall

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