PIPages
Labs

Jean Lynch-Stieglitz

Georgia Institute of Technology, GA·Earth & Environmental Science

Winds over the tropical oceans decide where warm and cold surface water collects, and that pattern shapes weather and climate around the globe. Inside the ocean, waves and turbulent mixing move heat and water, but the global ocean models used for forecasting struggle to capture them.

Fields

Earth & Environmental Science

Physics

Topics

paleoceanography

paleoclimate

Last Glacial Maximum

Grants
2 known grants, through Jul 2027

What they work on

  1. Test how changes in tropical winds alter thermocline depth across the Indo-Pacific by running sensitivity experiments in a high-resolution ocean model.
  2. Extend a database of oxygen isotope measurements from subsurface planktonic foraminifera shells to the tropical Indian Ocean, covering both modern and Last Glacial Maximum sediments.
  3. Infer Last Glacial Maximum tropical wind fields by inverting foraminiferal proxy data with the model-derived link between winds and thermocline structure.
  4. Measure flow distortion near rough topography, internal wave breaking, and momentum and buoyancy fluxes using a moored array of instruments in the Brazil Basin, South Atlantic.
  5. Compare a statistical description of the regional internal wavefield, built from tracer release and Global Drifter Program data, against five models from HYCOM to large eddy simulations.

More about the research

Both projects ask how ocean circulation works at scales that matter for climate. One reads the record of the last ice age. The other studies present-day mixing in the deep South Atlantic.

Why it matters

Better estimates of how tropical winds and the warm-water layer responded to ice-age conditions could improve understanding of how tropical climate, which steers global weather, may respond to rising greenhouse gases. Testing ocean models against field measurements of internal waves and mixing could help modelers make global circulation and forecast models more reliable. The ice-age reconstructions will also produce shared data that other climate researchers can use.

Known grants

From NIH and NSF research grants. Labs often have other funding we can't see.

Collaborative Research: The Internal Wave Spectrum and Boundary Mixing in the Sub-Tropical South Atlantic

NSF · Aug 2022 – Jul 2027

Collaborative Research: Large-Scale Dynamics of the Last Glacial Maximum Tropical Indo-Pacific

NSF · Jul 2024 – Jun 2027

Closest labs

Patrick Rafter

University of South Florida, FL·Earth & Environmental Science

Test whether Indian Ocean bottom water was unusually old during the last ice age by comparing the radiocarbon ages of fossil shells with sediment ages in four new cores from across the basin.

James Moum

Oregon State University, OR·Earth & Environmental Science

Test whether tropical instability waves in the equatorial Pacific radiate internal waves downward and reshape the internal wave field, using moorings, a fastCTD, the Epsilometer turbulence profiler and WireWalker drifting profilers.

Jessica Conroy

University of Illinois Urbana-Champaign, IL·Earth & Environmental Science

Map an oxygen isotope "isoscape" of the modern tropical Pacific from long-running seawater and precipitation collection sites, showing how seawater and rainfall isotope values shift between El Niño and La Niña phases.

The school

Georgia Institute of Technology: 50 labs on PI Pages, $1.5B a year on research, 572 research doctorates a year.

More about Georgia Institute of Technology

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