Professor
jonathan.nash@oregonstate.edu

Office: 541-737-4573

Burt Hall

Burt Hall 402

2651 SW Orchard Avenue

2651 SW Orchard Avenue
Corvallis, OR 97331

Profile Field Tabs

At OSU
Brief Research Interests: 

The physics of turbulence, mixing and other small-scale processes in the ocean and near ice.
We also develop new technologies (like autonomous vehicles and sensor systems) to measure glacier ice melt, internal waves, submesoscale instabilities, and use these observations to better understand ocean dynamics.

Location: 
Building: 

Research Interests

Ocean Mixing - Exploring the physics of turbulence and mixing is key to our understanding of ocean dynamics. Innovative instrumentation, detailed analysis, and simple dynamical models enable us to:

  • understand the generation and evolution of turbulence
  • quantify irreversible fluxes of heat, salt, biology, chemicals and momentum
  • identify the processes (the pathways to turbulence) which produce these fluxes
  • determine the effects of turbulence on the system in which is embedded, such as:
    • the buoyant ice-melt plumes that bring heat towards glaciers,
    • heat- and carbon-fluxes that control air-sea exchange
    • turbulent diffusion of nutrients and plankton
    • transport of sediment that influences benthic dynamics

Interested in joining our group?

We seek motivated students at all levels to work with our team to explore the turbulent world around us. 
Send me an email if you want to join us to investigate ocean-ice physics, solve climate-related challenges, develop skills to analyze data and devise creative ways to understand geophysical dynamics.    

Current Research

Elucidating ocean Mixing

We develop and deploy instruments to explore dynamics that includes the smallest scales of motion.  These are crucial to understanding ocean turbulence and its effects. Some of our projects of the Ocean Mixing Group include:

  • self-contained instrument packages called chi-pods that can measure mixing on moorings and provide multi-year records of turbulence.  
  • similar packages that can be deployed during routine CTD-profiling and provide a global distribution of deep ocean mixing.

PHYSICS of glacier Ice melt

As relatively warm ocean waters interact with marine-terminating glaciers, they produce buoyant plumes of meltwaters that rise along the face of the glacier, creating beautiful colors and patterns that reveal details of the fluid dynamics that formed them.  We are developing new instruments to probe the boundary-layer dynamics responsible for ice melt.

Take a look at Erin Pettit's site that describes some of our recent work in Alaska 

Autonomous systems for Exploring upper-ocean and near-glacier dynamics

Our team of faculty, graduate and engineering & physics undergraduate students work together we envision, build, and deploy new systems to explore fundamental physics of the natural world. 

Many thanks go to Nick McCombe, June Marion, and an amazing team of OSU engineers for visioning and creating our first Robotic Oceanographic Surface Sampler (ROSS), pictured below in the Bay of Bengal, near India.   

coastal dynamics, internal waves and the submesoscale 

Where river waters meet the coastal ocean, buoyant plumes of fresh water collide with seawater, creating strong fronts, intense mixing, and the exchange of nutrients that fuel biological productivity.   

An example of the three-dimensional structure of the upper ocean in the Gulf of Mexico as collected from our autonomous vessel, AR/V Polly, who performed this repeated triangle 30 times (at approximately 4.5-h repeat rate) during a 6-day period. The left panel shows temperature from Polly's towed T-chain, the right panel is the meridional component of velocity.

 

Education

B.Sc., Queen's University at Kingston, Ont. (Engineering Physics), 1991
M.Sc., Cornell University (Environmental Engineering), 1995
Ph.D., Oregon State University (Physical Oceanography), May 2000

Students, Post-docs and Techs

PhD Candidates -- Anna Simpson, Kaelan Weiss, Nadia Cohen, Fucent Hsu

Post-docs --  Ken Zhao, Aurelie Moulin 

Techs -- Jasmine Nahorniak, Noah Osman

Undergrads -- Erica Tindal, Kyle Jenson, Diego Camacho, Sam Felsted and more

Science Connections 

Collaboration is what makes science fun. At OSU, Meagan Wengrove, Erin Pettit, Eric Skyllingstad, Jesse Cusack, Astrid Leitner, Kipp Shearman, Jessica Garwood, Jim Moum, Bill Smyth work closely and in complementary ways with our group

Lots of great science happens elsewhere.  We work collaboratively with Jen MacKinnon, Matthew Alford, Amy Waterhouse, Sarah Purkey, Effie Fine (at Scripps/UCSD), Trevor Harrison at UW, John Taylor at Cambridge, Leif Thomas at Stanford, Dave Sutherland at the UofO, Becca Jackson at Rutgers, Jody Klymak at University of Victoria. 

Other Stuff

Alaska Glaciers on Petersburg's KFSK
Popping bubbles make glaciers melt faster (EOS)

Publications

Link to Jonathan's Google Scholar page

Below is an assortment of recent work: 

Melting of glacier ice enhanced by bursting air bubbles (2023) Nature Geoscience 16 (10), 871-876 (ME Wengrove, EC Pettit, JD Nash, RH Jackson, ED Skyllingstad)

Internal gravity waves generated by subglacial discharge: Implications for tidewater glacier melt (2022) Geophysical Research Letters, 50 (12) (JM Cusack, RH Jackson, JD Nash, E Skyllingstad, EC Pettit)

Meltwater intrusions reveal mechanisms for rapid submarine melt at a tidewater glacier (2020) Geophysical Research Letters 47 (2), (RH Jackson, JD Nash, C Kienholz, DA Sutherland, JM Amundson, ...)

Climate process team on internal wave–driven ocean mixing (2017) Bulletin of the American Meteorological Society, 2017 (JA MacKinnon, Z Zhao, CB Whalen, AF Waterhouse, JD Nash,...)

Hotspots of deep ocean mixing on the Oregon continental slope, Geophys. Res. Lett., 34, L01605, doi:10.1029/2006GL028170, 2007 (Nash, J. D., M. H. Alford, E. Kunze, K. Martini, and S. Kelly)

Structure of the baroclinic tide generated at Kaena Ridge, Hawaii, J. Phys. Oceanogr., 36(6), 1123-1135, 2006 (Nash, J.D., E. Kunze, C.M. Lee and T.B. Sanford)

River plumes as a source of large-amplitude internal waves in the coastal ocean, Nature, 437, 400-403, 2005 doi:10.1038/nature03936 (J.D. Nash and J.N. Moum)

Estimating Internal Wave Energy Fluxes in the Ocean, J. Atmos. and Oceanic Tech., 22(10), 1551-1570, 2005 (J.D. Nash, M.H. Alford and E. Kunze).

Internal tide reflection and turbulent mixing on the continental slope, J. Phys. Oceanogr. 34(5), 1117-1134, 2004 (J.D. Nash, E. Kunze, J. M. Toole and R. W. Schmitt)

Microstructure observations of turbulent salinity flux and the dissipation spectrum of salinity, J. Phys. Oceanogr., 2002, 32, 2312-2333 (J.D. Nash and J.N. Moum).

Internal hydraulic flows on the continental shelf: high drag states over a small bank, J. Geophys. Res., 106, 4593-4611, 2001 (J.D. Nash and J.N. Moum)

Estimating salinity variance dissipation rate from microstructure conductivity measurements, J. Oceanic Atmos. Technol., 16, 263-274 , 1999 (J.D. Nash and J.N. Moum)