GSO faculty and scientists are internationally recognized through their leadership in scientific programs, the impact of their research, their positions of leadership for scientific journals and societies, and their scientific awards and fellowships. Links to laboratories and research programs with web pages are listed below.
Estimated percent of subseafloor sedimentary respiration supported by in situ water radiolysis at South Pacific gyre sites (in red box) (D’Hondt et al., 2009) and eastern equatorial Pacific sites (Blair et al., 2007).
Diagram of the Inverted Echo Sounder (IES): an ocean bottom-moored instrument that measures vertical acoustic travel time ( VATT ) round trip from the sea floor to the sea surface. GSO/URI currently produces Model 6.2 IES.
Numerical model simulation of Hurricane Gustav. Langmuir circulation direction predicted with Lagrangian Shear direction (black line). Red = Wind direction, black = Lagrangian Shear direction, blue = Surface Stokes drift direction.
Numerical model output of the wave-dependent drag Coefficients of Hurricane Bonnie.
Chart depicting the decay of a near-inertial wave.
Tuning up the new FTIR system: a Thermo Nicolet iS50 FTIR bench spectrometer coupled with a Continuum IR microscope, for analysis of C-O-H compounds in natural and synthetic materials. The microscope is equipped with 250 µm and 50 µm MCT-A detectors, and has automated mapping capability.
In order to get a concentration that can be analyzed easily by gas chromatography and mass spectrometry (GC/MS), samples are further concentrated to about 0.2 mL using a mini-evaporator.
From a biodiversity study in planktonic microorganisms. A result of a population model simulating the effects 30 competing species. Coexistence for at least 1000 generations was observed in at least 90% of the simulations when there were initially at least 1000 individuals per species. No extinctions were observed.
Rynearson lab graduate student Kerry Whittaker sampling diatoms from the Gulf of Alaska, aboard the R/V Thomas G Thompson
The traveltime sensitivity kernels for the head wave on the horizontal planes at depths below and above the interface that separates the low and high velocity layers. The green line marks the head wave ray path. The source is located on the left side of this figure. The negative (red colors) and positive (blue colors) values are so defined that a low-velocity anomaly located in the region of the negative kernels results in a travel time delay and the same velocity perturbation in the region of positive kernels leads to an earlier head wave arrival. Zhang et al., GJI, 2007.