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Deepak Cherian

physical oceanographer
Research Associate (Post-doc), Oregon State University

Research

I study dynamical connections between disparate scales of motion in the climate system with a diverse set of tools. Themes include small-scale turbulence & mixing, large scale air-sea interaction (intraseasonal oscillations and such), mesoscale oceanic eddies, baroclinic instabilities, continental shelf flow and equatorial dynamics. My toolkit includes observational records from moored and satellite platforms as well as high resolution idealized process-study models.

Mixing measurements in the Bay of Bengal

With Emily Shroyer (OSU), Jim Moum (OSU) & the OSU Ocean Mixing Group.

bob-chipods.png

Multiple year-long moored turbulent mixing measurements collected using fast temperature sensors (χ-pods) as part of the ASIRI/DYNAMO/EBoB/RAMA programmes paint a picture of mixing across the Bay of Bengal that spans multiple time scales: interannual to diurnal and shorter.

Interesting signals include interannual & intraseasonal variability, a daily cycle in turbulence, depressed turbulence in barrier layers, elevated mixing associated with the tropical cyclones and a quiet ocean below 50m.

(map shows past and proposed deployments - courtesy Emily Shroyer)

Cross-shelfbreak exchange by mesoscale eddies

Advisor: Ken Brink (WHOI) | Read the paper! | More

eddyshelf-3d.png

My dissertation looked at the interaction of deep-ocean mesoscale eddies with continental shelf-slope topography.

When visualized using passive tracer fields (red tracks eddy water and blue, shelf-slope water), the interaction clearly results in the formation of smaller-scale secondary vortices. We term these 'stacked' vortices to reflect their (unexpected) vertical structure wherein shelf-slope water is stacked over eddy water.

Observational evidence for these features remains elusive.

Shelf flows forced by mesoscale eddies

Advisor: Ken Brink (WHOI) | More

One chapter of my thesis focused on the shelf flows forced by mesoscale eddies translating at the shelfbreak. The flow field is summarized below. What I found most interesting was the difference in vertical structure of the cross-shelfbreak flow. The shelf-water outflow is approximately vertically uniform whereas the eddy- and slope-water inflow is strongly sheared. Our paper explains why this happens.

shelf-flow-summary.png

Inertial-gravity waves in the equatorial Pacific

With Tom Farrar (WHOI) & Ted Durland (OSU) | Code

farrar-durland-spectrum-deepak.png

Satellite observations give humanity an unprecedented detailed look at the surface ocean. The vertical structure of variability associated with surface signals is relatively less known, and the relevance of theoretical structures derived using strict assumptions is debated; viz., the so-called baroclinic vertical modes.

Motivated by the [zonal wavenumber]-frequency spectra of dynamic height calculated by Farrar & Durland (2012) — see image on right — my goal is to infer the vertical structure of 7-day period inertial-gravity waves in the equatorial Pacific (filter band marked by horizontal lines). I am using long term subsurface temperature measurements and inferred dynamic height from the TAO/TRITON project.

Publications

nearly done

(drafts available on request)

  • Cherian D.A., Brink K.H. Shelf flows forced by deep-ocean anticyclonic eddies at the shelfbreak. submitted to Journal of Physical Oceanography.
  • Cherian D.A., Farrar J.T., Durland T.S. in prep. The upper-ocean vertical structure of 7-day period inertial-gravity waves in the equatorial Pacific.

2016

  • Cherian D.A., Brink K.H. (2016) Offshore Transport of Shelf Water by Deep-Ocean Eddies. Journal of Physical Oceanography. 46 3599–3621. DOI PDF

2013

  • Haine T.W.N., Cherian D.A. (2013) Analogies of Ocean/Atmosphere Rotating Fluid Dynamics with Gyroscopes: Teaching Opportunities. Bull. Amer. Meteor. Soc.. 94:684. DOI PDF Supplement
  • Brink K.H., Cherian D.A. (2013) Instability of an idealized tidal mixing front: Symmetric instabilities and frictional effects. Journal of Marine Research. 71(6):26. DOI PDF

Thesis

  • Cherian D.A. (2016) When an eddy encounters shelf-slope topography. PDF

Teaching

While at MIT, I took the semester-long Teaching Certificate Program. I learned that it is generally more effective to have students work through a derivation primarily on their own in class with hints. Following that advice, I created worksheets that guide students through a derivation, guiding them toward important implications and reasoning for various steps. Here are the ones I have so far.

  1. Rossby adjustment - for OSU's Geophysical Waves class
  2. Non-hydrostatic internal waves - for OSU's Geophysical Waves class
  3. Sverdrup balance - for MIT's 12.808 - Observational Physical Oceanography

These are targeted at beginning graduate students. Any comments you might have on these are welcome. Please send me an email.

Latex source is also available on request.

Posts

Contact

Email:

Office Address: Burt 434, OSU, Corvallis SSR, OR

Acknowledgments

My work has been funded by the US National Science Foundation and the Office of Naval Research.

Styling gratefully borrowed from Ethan Schoonover, Nicolas P. Rougier and Matthew Butterick.

Icons from FontAwesome and Academicons.

Website built using Emacs Org-mode (source code)