Award Abstract # 1553593
CAREER: Evolution of Ocean Mesoscale Turbulence in a Changing Climate

NSF Org: OCE
Division Of Ocean Sciences
Recipient: THE TRUSTEES OF COLUMBIA UNIVERSITY IN THE CITY OF NEW YORK
Initial Amendment Date: February 8, 2016
Latest Amendment Date: March 17, 2020
Award Number: 1553593
Award Instrument: Continuing Grant
Program Manager: Baris Uz
bmuz@nsf.gov
 (703)292-4557
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: February 15, 2016
End Date: January 31, 2022 (Estimated)
Total Intended Award Amount: $762,946.00
Total Awarded Amount to Date: $762,946.00
Funds Obligated to Date: FY 2016 = $132,734.00
FY 2017 = $150,245.00

FY 2018 = $151,220.00

FY 2019 = $158,539.00

FY 2020 = $170,208.00
History of Investigator:
  • Ryan Abernathey (Principal Investigator)
    ra2697@columbia.edu
Recipient Sponsored Research Office: Columbia University
615 W 131ST ST
NEW YORK
NY  US  10027-7922
(212)854-6851
Sponsor Congressional District: 13
Primary Place of Performance: Lamont-Doherty Earth Observatory of Columbia University
61 Route 9W
Palisades
NY  US  10964-1707
Primary Place of Performance
Congressional District:
17
Unique Entity Identifier (UEI): F4N1QNPB95M4
Parent UEI:
NSF Program(s): PHYSICAL OCEANOGRAPHY,
EDUCATION/HUMAN RESOURCES,OCE
Primary Program Source: 01001617DB NSF RESEARCH & RELATED ACTIVIT
01001718DB NSF RESEARCH & RELATED ACTIVIT

01001819DB NSF RESEARCH & RELATED ACTIVIT

01001920DB NSF RESEARCH & RELATED ACTIVIT

01002021DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 1045, 4444
Program Element Code(s): 161000, 169000
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Once the large-scale ocean circulation was viewed as a sluggish continuous flow. Thanks to new satellite and in situ observations, powerful numerical models, and advances in theory, it is now understood that ocean mesoscale turbulence, the highly energetic, nonlinear jumble of waves, eddies, and jets which characterizes ocean currents on scales of 20-500 km, is an essential component of ocean circulation, transport, and marine ecosystems. Because this turbulence draws its energy from instabilities of the large-scale flow, its properties are themselves sensitive to changes in climate. This project seeks to answer the question: how, and on what timescales, do large-scale changes in global climate affect the properties of ocean mesoscale turbulence? As such, the proposed work has the potential to transform how the climate community views mesoscale turbulence. Because most ocean climate models are too coarse to resolve the mesoscale, the effects of mesoscale turbulence are parameterized. As a result, mesoscale turbulence is reduced to a "parameter" to be tuned, rather than an emergent, dynamic part of the Earth system. The project is aimed at deepening basic physical understanding of the processes that regulate the properties of mesoscale turbulence and the timescales on which these properties respond to changes in climate. Consideration of this two-way interaction will lead to a richer understanding of the role of the ocean in the climate system, opening the door to new mechanisms for climate feedbacks. The project will also lead to methodological advances in Big Data computational tools for oceanography. The curriculum development will address the need for students to develop strong computational skills and, in particular, the capability to handle Big Data, to meet the emerging challenges of 21st century science. It will also promote active learning and the use of data in the oceanography classroom. The open-source nature of the teaching materials will encourage wide adoption. Strong interaction between research and education is guaranteed, because the same tools used in the research will be incorporated into the curriculum, both evolving together throughout the project.

The research component of this CAREER award will examine the link between climate change, baroclinic instability, mesoscale eddy properties (kinetic energy and length scales), and mesoscale mixing, using a hierarchy of models and observations. Idealized process models will build a theoretical foundation of understanding of how changes in surface wind and buoyancy forcing lead to changes in mesoscale turbulence. Decadal variability in mesoscale statistics and baroclinic instability will also be examined in satellite and hydrographic observations. Finally, the theoretical framework and statistical analysis will be applied to global, eddy-resolving climate model simulations of greenhouse warming. To facilitate this work, Python-based computational tools for rapid data processing will be developed. These tools will be integrated into education through development of an open-source curriculum in "Big Data Oceanography," in which the computational skills necessary to study global, high-resolution datasets are taught side-by-side with core ocean science concepts. These modules will be deployed and assessed in an undergraduate course and disseminated widely online and at education conferences.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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(Showing: 1 - 10 of 18)
Anirban Sinha and R. Abernathey "Timescales of Southern Ocean Eddy Equilibration" J. Phys. Oceanogr. , v.46 , 2016 , p.2785--280 10.1175/JPO-D-15-0192.1
Bailey, Shanice Tseng and Jones, Spencer and Abernathey, Ryan Patrick and Gordon, Arnold L. and Yuan, Xiaojun "Water mass transformation variability in the Weddell Sea in Ocean Reanalyses" Ocean science discussions , 2022 https://doi.org/10.5194/egusphere-2022-129 Citation Details
Bolton, T., R. Abernathey, and L. Zanna "Regional and Temporal Variability of Lateral Mixing in the North Atlantic" Journal of Physical Oceanography , v.49 , 2019 , p.260126 10.1175/JPO-D-19-0042.1
C. S. Jones Ryan P. Abernathey "Isopycnal mixing controls deep ocean ventilation" Geophysical Research Letters , v.46 , 2019 , p.13144 10.1029/2019GL085208
J. Busecke and R. P. Abernathey "Ocean mesoscale mixing linked to climate variability" Science Advances , v.5 , 2019 10.1126/sciadv.aav5014
Jeong, Hyein and Asay-Davis, Xylar S. and Turner, Adrian K. and Comeau, Darin S. and Price, Stephen F. and Abernathey, Ryan P. and Veneziani, Milena and Petersen, Mark R. and Hoffman, Matthew J. and Mazloff, Matthew R. and Ringler, Todd D. "Impacts of ice-shelf melting on water mass transformation in the Southern Ocean from E3SM simulations" Journal of Climate , 2020 https://doi.org/10.1175/JCLI-D-19-0683.1 Citation Details
Jeong, Hyein ; Asay-Davis, Xylar S. ; Turner, Adrian K. ; Comeau, Darin S. ; Price, Stephen F. ; Abernathey, Ryan P. ; Veneziani, Milena ; Petersen, Mark R. ; Hoffman, Matthew J. ; Mazloff, Matthew R. ; Ringler, Todd D. "Impacts of ice-shelf melting on water mass transformation in the Southern Ocean from E3SM simulations" Journal of Climate , v.33 , 2020 , p.5787-5807 10.1175/JCLI-D-19-0683.1
Lei Wang and M. F. Jansen and R. P. Abernathey "Eddy phase speeds in a two-layer model of quasigeostrophic baroclinic turbulence with applications to ocean observations" Journal of Physical Oceanography , v.46 , 2016 , p.1963--198 10.1175/JPO-D-15-0192.1
Liu, T., Abernathey, R., Sinha, A., & Chen, D. "Quantifying eulerian eddy leakiness in an idealized model" Journal of Geophysical Research: Oceans , v.124 , 2019 , p.8869-8886 10.1029/2019JC015576
N. Tarshish and R. P. Abernathey and C. Zhang and C. O. Dufour and I. Frenger and S. M. Griffies "Identifying Lagrangian Coherent Structures in a Mesocale Eddy-Permitting Ocean Model" Ocean Modeling , v.130 , 2018 , p.15 10.1016/j.ocemod.2018.07.001
R. P. Abernathey and G. Haller "Transport by Coherent Lagrangian Vortices in the Eastern Pacific" Journal of Physical Oceanography , v.48 , 2018 , p.667 10.1175/JPO-D-17-0102.1
(Showing: 1 - 10 of 18)

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.

In terms of science impacts, our research made signifcant advanceds in the following three areas.
  1. Temporal Dynamics of Mesoscale Energetics - This was the original focus of the proposal. Our first paper (Sinha & Abernathey, 2016) identified the key mechanisms governing the time-dependent response of turbulence to external forcing and influenced future work by other authors.
  2. Lagrangian Coherent Structures - our work has provided new methods for quantifying the impact of coherent mesoscale eddies on transport. Challenging published results, we showed that the "trapping" effect of eddies has a minimal contribution to transport. We published several papers on this, which are now cited regularly.
  3. Novel diagnostics of temporal variability - work in the later part of the award (Tesdal & Abernathey, 2021; Bailey et al, 2022) focused on developing rigorous diagnostics for understanding drivers of temporal variability in the ocean. These methods have broad applicability, beyond the specific areas where they were applied. 

In terms of broader impacts, the innovative, data-driven curriculum for scientific computing in geoscience has had a significant influence on workforce development. Over the past four years, I have trained roughly 100 first-year PhD students in the fundamentals of open-source, data-intensive scientific computing with Python via the Research Computing in Earth Science course. During that time period, these skills have become increasingly desireable in the emerging private sector related to climate and weather risk analysis. Consequently our students are now very well poised to fill data science positions in these new companies, and several have already made this transition.


Last Modified: 08/24/2022
Modified by: Ryan Abernathey

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