
NSF Org: |
OCE Division Of Ocean Sciences |
Recipient: |
|
Initial Amendment Date: | February 7, 2014 |
Latest Amendment Date: | March 6, 2018 |
Award Number: | 1352422 |
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: | March 1, 2014 |
End Date: | February 28, 2021 (Estimated) |
Total Intended Award Amount: | $400,456.00 |
Total Awarded Amount to Date: | $400,456.00 |
Funds Obligated to Date: |
FY 2015 = $81,868.00 FY 2016 = $99,476.00 FY 2017 = $86,756.00 FY 2018 = $73,696.00 |
History of Investigator: |
|
Recipient Sponsored Research Office: |
550 S COLLEGE AVE NEWARK DE US 19713-1324 (302)831-2136 |
Sponsor Congressional District: |
|
Primary Place of Performance: |
DE US 19716-2553 |
Primary Place of
Performance Congressional District: |
|
Unique Entity Identifier (UEI): |
|
Parent UEI: |
|
NSF Program(s): |
PHYSICAL OCEANOGRAPHY, EDUCATION/HUMAN RESOURCES,OCE |
Primary Program Source: |
01001516DB NSF RESEARCH & RELATED ACTIVIT 01001617DB NSF RESEARCH & RELATED ACTIVIT 01001718DB NSF RESEARCH & RELATED ACTIVIT 01001819DB NSF RESEARCH & RELATED ACTIVIT |
Program Reference Code(s): |
|
Program Element Code(s): |
|
Award Agency Code: | 4900 |
Fund Agency Code: | 4900 |
Assistance Listing Number(s): | 47.050 |
ABSTRACT
Turbulent processes in the upper ocean play a key role in weather and climate systems by coupling the ocean and atmosphere. Upper ocean turbulence also distributes nutrients, pollutants, plankton, and bubbles in the ocean mixed layer. The fate of chemical and biological substances in the mixed layer depends on the history of advective turbulent fluid paths. Besides being dispersive, ocean turbulence also aggregates substances to increase encounter rates between them. Upper ocean turbulence is driven by surface waves: Wave-current interactions lead to wind-aligned vortices, called Langmuir circulation (LC), and breaking waves are a source of near surface turbulent kinetic energy. Together, LC and the stochastically breaking wave field lead to complicated nonlocal and intermittent transport. To better understand the dynamics of the complex oceanic boundary layer and to educate students about upper ocean processes, the PI will carry out an interwoven research and education program. This project is a systematic Lagrangian investigation following trajectories of fluid parcels with the Research Objectives to: 1) Develop a Lagrangian analysis framework of the upper ocean with realistic surface wave effects to investigate fundamental mechanisms of fluid exchange in the presence of surface waves, 2) Examine the role of LC and breaking waves in upper ocean transport to assess systematically the accuracy of common upper ocean boundary layer parameterizations, 3) Apply the Lagrangian analysis to quantify plastic marine debris that has emerged as a major ocean pollutant and to revisit related classic ideas of particle trapping in the upper ocean. Tracks of particles will be computed from state-of-the art upper ocean large eddy simulation models with LC and breaking wave effects. As part of the Lagrangian analysis, this project will apply a new and integrative dynamic systems approach to the wave-driven upper ocean boundary layer. To directly utilize knowledge gained from this study, the PI will examine observed distributions of plastic marine debris. The project involves two related education activities that are linked to the research activities on upper ocean dynamics with the Education Objectives to: 1) Educate students about ocean physics and its role in climate change and global pollution, 2) Inspire students to pursue STEM education and careers by engaging students in problem-based learning and implementing Next Generation Science Standards, 3) Involve underrepresented students. The first educational activity will involve the PI's participation in the active education programs on marine debris at the Sea Education Association, reaching out to undergraduate students and the general public. The second education activity is centered on developing a hands-on laboratory educational unit, which will be incorporated into regular curricula of high schools with a large number of underrepresented students and also into the University of Delaware's Forum to Advance Minorities in Engineering Program, which is aimed at increasing the effective participation of minority students in engineering and other science professions. Both activities incorporate the PI's expertise in geophysical fluids dynamics, upper ocean physics, and ongoing research collaborations.
Intellectual Merit: By revealing regions of attraction, repulsion, and intense mixing, the Lagrangian framework provides a natural approach to investigating turbulence that has yet to be systematically explored in the context of wave-driven upper ocean dynamics. Thus, the study bears high potential to uncover a novel, highly physical description of upper ocean turbulence that will ultimately enhance the parameterizations of turbulent transport in larger scale ocean models.
Broader Impacts: The PI will advance coupled ocean-atmosphere models of weather and climate by improving the ability to parameterize air-sea fluxes and ocean turbulence. The research will facilitate communication between the ocean physics and marine debris research communities, a necessary step in effectively quantifying and ultimately managing ocean pollution. Because the topic of marine pollution is accessible to a broad audience, the project activities present a unique opportunity to educate the general public, high school minority students, undergraduate students, and graduate students about ocean turbulence and fluid dynamics in a collaborative environment with experts in upper ocean dynamics, numerical modeling, dynamic systems theory, and sea-going oceanography.
PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH
Note:
When clicking on a Digital Object Identifier (DOI) number, you will be taken to an external
site maintained by the publisher. Some full text articles may not yet be available without a
charge during the embargo (administrative interval).
Some links on this page may take you to non-federal websites. Their policies may differ from
this site.
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.
Turbulent processes in the upper ocean play a key role in weather and climate systems by coupling the ocean and atmosphere. Upper ocean turbulence also distributes nutrients, pollutants, plankton, and bubbles in the ocean mixed layer. The fate of chemical and biological substances in the mixed layer depends on the history of advective turbulent fluid paths. Besides of being dispersive, ocean turbulence also aggregates substances to increase encounter rates between them. Upper ocean turbulence is driven by surface waves: Wave-current interactions lead to wind-aligned vortices, called Langmuir circulation (LC), and breaking waves are a source of near surface turbulent kinetic energy. Together, LC and the stochastically breaking wave field lead to complicated nonlocal and intermittent transport. This project has contributed to a better understanding of the dynamics of the complex oceanic boundary layer and to the education of students about upper ocean processes through an interwoven research and education program. This project has developed a Lagrangian analysis framework of the upper ocean following trajectories of fluid parcels, based on a turbulence resolving computational model with realistic surface wave effects to investigate fundamental mechanisms of fluid exchange in the presence of surface waves. In particular, we have implemented a novel numerical scheme, which is constrained by wind energy input to surface waves, to capture breaking waves in a turbulence resolving computational approach. Unresolved turbulent motions are simulated with a Lagrangian stochastic model to be energetically consistent with the turbulent resolving simulation model. Our Lagrangian analysis reveals three distinct turbulent time scales: an integral, a dispersive mixing, and a coherent structure time. We find that LC and breaking waves fundamentally affect the upper ocean transport by submerging particle to greater depth and aggregating material in regions of convergent flows. Furthermore, particles in the upper ocean experience synergistic vertical mixing in which breaking waves inject particles into Langmuir downwelling velocities sufficient to drive deep mixing. We have developed new upper ocean boundary layer mixing schemes for regional and global models, which we applied to quantify plastic marine debris that has emerged as a major ocean pollutant. We find that microplastic surface measurements substantially underestimate the total microplastic content in the water column due to wind- and wave-driven mixing. We have collaborated with researchers at the Sea Education Association and reached out to undergraduate students and the general public. Through related education activities that are linked to the proposed research activities on upper ocean dynamics, we have educated students about ocean physics and its role in climate change and global pollution and engaged diverse students in problem-based learning. We have developed a hands-on laboratory educational unit "Ocean Density and Mixing: From Climate to Microplastics" with lesson plan in collaboration with Science Educators, which is publicly available for incorporation into regular curricula of middle and high schools. Based on this lesson plan, we organized a Virtual Science Academy for live hands-on activities and a joint remote educator workshop to present the lesson plan to educators across the country. This project also contributed to developing new teaching laboratories at the University of Delaware and the training of multiple graduate students. Therefore, this project has not only contributed to uncovering a novel, highly physical description of upper ocean turbulence that enhances the parameterizations of turbulent transport in larger scale ocean models, but also provided a unique opportunity to educate the general public, diverse K-12 students, undergraduate students, and graduate students about ocean turbulence and fluid dynamics in a collaborative environment with experts in upper ocean dynamics, numerical modeling, and sea-going oceanography.
Last Modified: 06/28/2021
Modified by: Tobias Kukulka
Please report errors in award information by writing to: awardsearch@nsf.gov.