Award Abstract # 1130678
Collaborative Research: Langmuir Turbulence Under Tropical Cyclones

NSF Org: OCE
Division Of Ocean Sciences
Recipient: UNIVERSITY OF DELAWARE
Initial Amendment Date: August 30, 2011
Latest Amendment Date: August 30, 2011
Award Number: 1130678
Award Instrument: Standard Grant
Program Manager: Eric C. Itsweire
OCE
 Division Of Ocean Sciences
GEO
 Directorate for Geosciences
Start Date: September 1, 2011
End Date: August 31, 2015 (Estimated)
Total Intended Award Amount: $274,890.00
Total Awarded Amount to Date: $274,890.00
Funds Obligated to Date: FY 2011 = $274,890.00
History of Investigator:
  • Tobias Kukulka (Principal Investigator)
    kukulka@udel.edu
Recipient Sponsored Research Office: University of Delaware
550 S COLLEGE AVE
NEWARK
DE  US  19713-1324
(302)831-2136
Sponsor Congressional District: 00
Primary Place of Performance: University of Delaware
DE  US  19716-2553
Primary Place of Performance
Congressional District:
00
Unique Entity Identifier (UEI): T72NHKM259N3
Parent UEI:
NSF Program(s): PHYSICAL OCEANOGRAPHY,
EMERGING TOPICS
Primary Program Source: 01001112DB NSF RESEARCH & RELATED ACTIVIT
Program Reference Code(s): 9150
Program Element Code(s): 161000, 776400
Award Agency Code: 4900
Fund Agency Code: 4900
Assistance Listing Number(s): 47.050

ABSTRACT

Turbulent mixing in the ocean surface layer under tropical cyclones effectively couples the ocean and atmosphere through air-sea fluxes of heat and momentum. Air-sea heat fluxes sustain Tropical Cyclones and strongly depend on near surface temperature, which is determined by mixing with cooler deeper water. Understanding the turbulent processes involved in near-surface layer mixing remains one of the great challenges in modeling the coupled ocean-Tropical Cyclone system. Upper ocean turbulence is driven by the surface wind stress, resulting in sheared subsurface currents. Furthermore, surface gravity waves influence upper ocean turbulence through wave-current interactions that lead to wind-aligned vortices, called Langmuir circulation or Langmuir turbulence. Wave effects on ocean turbulence are particularly complex under Tropical Cyclones, since wind, wave, and current fields are inhomogeneous and may be misaligned. In addition, the surface wave height spectrum can comprise multiple peaks at different wave frequencies and directions. The proposed work is aimed at understanding Langmuir circulation under realistic Tropical Cyclone conditions and at assessing the role of Langmuir circulation on the coupled ocean-wave-atmosphere Tropical Cyclone dynamics. This project addresses the following hypotheses: Langmuir circulation characteristics under Tropical Cyclones critically depend on detailed wind, wave, and current conditions. Specifically, regions under Tropical Cyclones exist where upper ocean mixing is greatly influenced by Langmuir circulation. The use of an ocean mixing scheme with explicit Langmuir circulation effects will lead to significantly modified mixing and sea surface temperature cooling in Langmuir circulation regions. Including explicitly the Langmuir circulation effect will have a significant effect on the three-dimensional Tropical Cyclone dynamics and prediction.

These hypotheses will be tested by applying synergistically a coupled atmosphere-wave-ocean model (AWO) and a turbulence resolving large eddy simulation model (LES) that captures Langmuir circulation. Initially, the AWO will provide critical output (wind, waves, and currents) to drive the LES model. LES results, in turn, will aid in characterizing Langmuir circulation under tropical cyclones and in critically assessing the ocean mixing parameterization. Finally, a turbulent mixing scheme with explicit Langmuir circulation and turbulence effects will be implemented in the ocean model component of the AWO model and a sensitivity study by simulating idealized and real case tropical cyclones will be performed. The model results will then be validated against available field observations in collaboration with scientists at the University of Washington.

Intellectual Merit: This project investigates ocean and atmosphere dynamics under Tropical Cyclones, which are coupled through turbulent upper ocean mixing. The investigators will examine an insufficiently understood turbulent process, Langmuir circulation, that is not explicitly represented in most ocean models, despite the fact that Langmuir circulation and turbulence may be a principal mixing component. The combination of regional and process-based models is anticipated to significantly advance our understanding of Langmuir circulation under Tropical Cyclones.

Broader Impact: While pursuing some fundamental scientific questions related to air-sea interactions, turbulent mixing, and Tropical Cyclone dynamics, the research will aid in addressing an important societal challenge. Tropical Cyclones critically disrupt infrastructure, cause severe flooding, and displace people in coastal regions. The investigator will advance the scientific basis of Tropical Cyclones models and improve their prediction skill, which will ultimately lead to increased reliability of hurricane forecasts and thus confidence in the official hurricane warnings. The resources from the proposed grant will train two doctoral graduate researchers. The outreach effort will educate the public about basic science with its societal impacts through special events (e.g., at the Open House at the University of Delaware). Science material developed in the course of this project will contribute to the University of Rhode Island comprehensive educational website Hurricanes: Science and Society (www.hurricanescience.org). The website provides information on the science of hurricanes, how hurricanes impact society, and how people and communities can prepare for and mitigate the impacts of hurricanes.

PUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH

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Brunner, K., T. Kukulka, G. Proskurowski, K. L. Law "Passive buoyant tracers in the ocean surface boundary layer: 2. Observations and simulations of microplastic marine debris" J. Geophys. Res. , v.120 , 2015 10.1002/2015JC010840
Kukulka, T., A. J. Plueddemann, and P. P. Sullivan "Nonlocal transport due to Langmuir circulation in a coastal ocean" JOURNAL OF GEOPHYSICAL RESEARCH , 2012 10.1029/2012JC008340
Kukulka, T., A. J. Plueddemann, and P. P. Sullivan, "Inhibited upper ocean restratification in nonequilibrium swell conditions" GEOPHYSICAL RESEARCH LETTERS , 2013 10.1002/grl.50708
Kukulka, T., K. Brunner "Passive buoyant tracers in the ocean surface boundary layer: 1. Influence of equilibrium wind-waves on vertical distributions" J. Geophys. Res. , v.120 , 2015 10.1002/2014JC010487
Rabe, T., Kukulka, T., I. Ginis, T. Hara, B. Reichl, E. D?Asaro, R. Harcourt, P. P. Sullivan "Langmuir turbulence under Hurricane Gustav (2008)" J. Phys. Oceanogr. , v.45 , 2015 , p.657 10.1175/JPO-D-14-0030.1

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 mixing in the ocean surface layer under tropical cyclones (TC) effectively couples the ocean and atmosphere through air-sea fluxes of heat and momentum. Air-sea heat fluxes sustain TCs and strongly depend on near surface temperature, which is determined by mixing with cooler deeper water. Understanding the turbulent processes involved in near-surface layer mixing remains one of the great challenges in modeling the coupled ocean-TC system. Upper ocean turbulence is driven by the surface wind stress, resulting in sheared subsurface currents. Furthermore, surface gravity waves influence upper ocean turbulence through wave-current interactions that lead to wind-aligned vortices, called Langmuir circulation or Langmuir turbulence (LC/T). Wave effects on ocean turbulence are particularly complex under TCs, since wind, wave, and current fields are inhomogeneous and may be misaligned. In addition, the surface wave height spectrum can comprise multiple peaks at different wave frequencies and directions. This project has advanced our understanding of LC/T under realistic TC conditions and contributed to the development of the next generation operational hurricanes prediction models.

 

To investigate coupled ocean-TC dynamics, the Project PIs and their Graduate Students applied synergistically a coupled atmosphere-wave-ocean model (AWO) and a turbulence resolving large eddy simulation model (LES) that captures LC/T. The AWO provided critical output (wind, waves, and currents) to drive the LES. LES results, in turn, were used to characterize LC/T under tropical cyclones. We validated model results against available field observations in collaboration with researchers from the University of Washington.  Our results demonstrate that without LC/T effects, simulated turbulence levels are significantly lower than observed ones. Consistent with observations, the LES with LC/T effects predicts a suppression of turbulence near the hurricane eye due to wind-wave misalignment. To include sea state dependent LC/T effects explicitly in common regional and global ocean models, we modified a turbulent mixing model and tested its performance against concurrent LES experiments under tropical cyclone conditions. The modified model enhances mixing and significantly improves the prediction of upper ocean temperatures and currents compared to the default (unmodified) turbulence model under tropical cyclones. We implemented the new turbulent mixing model with explicit LC/T effects in the ocean model component of the AWO and performed a sensitivity study by simulating idealized and real-case tropical cyclones. Our results suggest that accurate predictions of the LC/T effects on upper ocean response to a tropical cyclone requires an explicit sea-state dependent LC/T parameterization.

 

The Project PIs and their Graduate Students examined an insufficiently understood turbulent process, LC/T, that is not explicitly represented in most ocean models, despite the fact that LC/T is a principal mixing component. By combining regional and process-based models, we have advanced our understanding of LT/C under TCs. While pursuing some fundamental scientific questions related to air-sea interactions, turbulent mixing, and TC dynamics, the outcomes of this project aid in addressing an important societal challenge. TCs critically disrupt infrastructure, cause severe flooding, and displace people in coastal regions. The research contributed to advancing the scientific basis of TC models and to improving their prediction skill, which will ultimately lead to increased reliability of hurricane forecasts and thus confidence in the official hurricane warnings. This project trained one MS and two PhD Graduate Researchers.  We educated the public about basic science with its societal impacts through special events, public presentations, institutional seminars, an...

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