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We are boldly exploring our unknown Ocean to excite interest and inform the wise stewardship of our planet.

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Seeking Salt Fingers in the Tropical Atlantic
In the northwestern equatorial Atlantic, the water column is highly stratified, with warm, salty water sitting atop cooler, fresher, nutrient-rich waters carried northward from the Antarctic by the Atlantic Meridional Overturning Circulation (AMOC). These conditions make the region a hotspot for salt finger mixing, a fine-scale process in which heat and salt are exchanged across density gradients, leading to waters sinking and rising in a beautiful, swirling motion. Scientists suspect that these salt fingers transport essential nutrients for plankton growth, such as nitrate, to the surface, thereby fueling ecosystem productivity and potentially influencing carbon export to deeper waters. Drs. Joseph Gradone, Corday Selden of Rutgers University, U.S., and an international team will venture to the Tropical Atlantic to collect essential data on salt fingers and their role in nutrient transport from the deep sea to surface waters. Scientific evidence suggests that salt fingers in this region are intensifying as waters warm and their salinity changes, driven by the ocean absorbing excess heat from the atmosphere. Gradone and Selden hypothesize that this trend is amplifying salt-finger mixing and potentially offsetting predicted ocean productivity loss in the region by carrying more nutrients to the surface and altering ecosystem structure. Using R/V Falkor (too)’s CTD and rosette, two coordinated gliders, and an untethered, autonomous oceanographic vehicle called the Vertical Microstructure Profiler 5500, they will improve our understanding of the physical dynamics of salt fingers and their impact on primary productivity in this region of the global Ocean.
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In the coming years, our expeditions will explore understudied regions around all seven continents in our global Ocean.

Latest Expedition

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Seeking Salt Fingers in the Tropical Atlantic
In the northwestern equatorial Atlantic, the water column is highly stratified, with warm, salty water sitting atop cooler, fresher, nutrient-rich waters carried northward from the Antarctic by the Atlantic Meridional Overturning Circulation (AMOC). These conditions make the region a hotspot for salt finger mixing, a fine-scale process in which heat and salt are exchanged across density gradients, leading to waters sinking and rising in a beautiful, swirling motion. Scientists suspect that these salt fingers transport essential nutrients for plankton growth, such as nitrate, to the surface, thereby fueling ecosystem productivity and potentially influencing carbon export to deeper waters. Drs. Joseph Gradone, Corday Selden of Rutgers University, U.S., and an international team will venture to the Tropical Atlantic to collect essential data on salt fingers and their role in nutrient transport from the deep sea to surface waters. Scientific evidence suggests that salt fingers in this region are intensifying as waters warm and their salinity changes, driven by the ocean absorbing excess heat from the atmosphere. Gradone and Selden hypothesize that this trend is amplifying salt-finger mixing and potentially offsetting predicted ocean productivity loss in the region by carrying more nutrients to the surface and altering ecosystem structure. Using R/V Falkor (too)’s CTD and rosette, two coordinated gliders, and an untethered, autonomous oceanographic vehicle called the Vertical Microstructure Profiler 5500, they will improve our understanding of the physical dynamics of salt fingers and their impact on primary productivity in this region of the global Ocean.
Read More

From grants for caregivers to an artist-at-sea residency, our programs strive to deepen knowledge and inspire a connection with our planet’s life support system.

Latest Expedition

See all

Seeking Salt Fingers in the Tropical Atlantic
In the northwestern equatorial Atlantic, the water column is highly stratified, with warm, salty water sitting atop cooler, fresher, nutrient-rich waters carried northward from the Antarctic by the Atlantic Meridional Overturning Circulation (AMOC). These conditions make the region a hotspot for salt finger mixing, a fine-scale process in which heat and salt are exchanged across density gradients, leading to waters sinking and rising in a beautiful, swirling motion. Scientists suspect that these salt fingers transport essential nutrients for plankton growth, such as nitrate, to the surface, thereby fueling ecosystem productivity and potentially influencing carbon export to deeper waters. Drs. Joseph Gradone, Corday Selden of Rutgers University, U.S., and an international team will venture to the Tropical Atlantic to collect essential data on salt fingers and their role in nutrient transport from the deep sea to surface waters. Scientific evidence suggests that salt fingers in this region are intensifying as waters warm and their salinity changes, driven by the ocean absorbing excess heat from the atmosphere. Gradone and Selden hypothesize that this trend is amplifying salt-finger mixing and potentially offsetting predicted ocean productivity loss in the region by carrying more nutrients to the surface and altering ecosystem structure. Using R/V Falkor (too)’s CTD and rosette, two coordinated gliders, and an untethered, autonomous oceanographic vehicle called the Vertical Microstructure Profiler 5500, they will improve our understanding of the physical dynamics of salt fingers and their impact on primary productivity in this region of the global Ocean.
Read More

Experience the wonder of our global Ocean via immersive galleries of art, scientific discoveries, and film.

Latest Expedition

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Seeking Salt Fingers in the Tropical Atlantic
In the northwestern equatorial Atlantic, the water column is highly stratified, with warm, salty water sitting atop cooler, fresher, nutrient-rich waters carried northward from the Antarctic by the Atlantic Meridional Overturning Circulation (AMOC). These conditions make the region a hotspot for salt finger mixing, a fine-scale process in which heat and salt are exchanged across density gradients, leading to waters sinking and rising in a beautiful, swirling motion. Scientists suspect that these salt fingers transport essential nutrients for plankton growth, such as nitrate, to the surface, thereby fueling ecosystem productivity and potentially influencing carbon export to deeper waters. Drs. Joseph Gradone, Corday Selden of Rutgers University, U.S., and an international team will venture to the Tropical Atlantic to collect essential data on salt fingers and their role in nutrient transport from the deep sea to surface waters. Scientific evidence suggests that salt fingers in this region are intensifying as waters warm and their salinity changes, driven by the ocean absorbing excess heat from the atmosphere. Gradone and Selden hypothesize that this trend is amplifying salt-finger mixing and potentially offsetting predicted ocean productivity loss in the region by carrying more nutrients to the surface and altering ecosystem structure. Using R/V Falkor (too)’s CTD and rosette, two coordinated gliders, and an untethered, autonomous oceanographic vehicle called the Vertical Microstructure Profiler 5500, they will improve our understanding of the physical dynamics of salt fingers and their impact on primary productivity in this region of the global Ocean.
Read More

Science Team Resources

To help you plan for your expedition, this hub includes information about outreach, technical specifications for our robotic platforms, a list of lab equipment, information about accessing data repositories, and more.

Latest Expedition

See all

Seeking Salt Fingers in the Tropical Atlantic
In the northwestern equatorial Atlantic, the water column is highly stratified, with warm, salty water sitting atop cooler, fresher, nutrient-rich waters carried northward from the Antarctic by the Atlantic Meridional Overturning Circulation (AMOC). These conditions make the region a hotspot for salt finger mixing, a fine-scale process in which heat and salt are exchanged across density gradients, leading to waters sinking and rising in a beautiful, swirling motion. Scientists suspect that these salt fingers transport essential nutrients for plankton growth, such as nitrate, to the surface, thereby fueling ecosystem productivity and potentially influencing carbon export to deeper waters. Drs. Joseph Gradone, Corday Selden of Rutgers University, U.S., and an international team will venture to the Tropical Atlantic to collect essential data on salt fingers and their role in nutrient transport from the deep sea to surface waters. Scientific evidence suggests that salt fingers in this region are intensifying as waters warm and their salinity changes, driven by the ocean absorbing excess heat from the atmosphere. Gradone and Selden hypothesize that this trend is amplifying salt-finger mixing and potentially offsetting predicted ocean productivity loss in the region by carrying more nutrients to the surface and altering ecosystem structure. Using R/V Falkor (too)’s CTD and rosette, two coordinated gliders, and an untethered, autonomous oceanographic vehicle called the Vertical Microstructure Profiler 5500, they will improve our understanding of the physical dynamics of salt fingers and their impact on primary productivity in this region of the global Ocean.
Read More

Delayed Gratification

Back to Expedition

In March I was busy preparing to join R/V Falkor in Exmouth for Leg 2 of the Illuminating Biodiversity of the Ningaloo Canyons

Having a plan that enabled our participation in this voyage has allowed us to take advantage of an opportunity that the lead researchers of this voyage have been waiting years to achieve. My role here is to analyse the quantitative transects that we are undertaking on each ROV dive. I am particularly interested in understanding how the habitats and the composition of the seafloor biota might differ between the canyon systems that we have been exploring with SuBastian. Canyons have a fascinating mix of habitats, including steep hard canyon walls, thickly sedimented slopes, and complex current dynamics which will favour different types of critters in different parts of the canyon. The ability of SuBastian to climb up the steep slopes and image the biota provides us with a completely new picture of these canyon habitats, expanding our knowledge and understanding of a previously unexplored part of the Great Barrier Reef margin.

The dives on this survey have shown that shrimp love living in the soft sediments that blanket the canyon floor and the more gentle parts of canyon walls.

So was it worth making a plan to enable science to continue in a Covid-world? Absolutely, for without this voyage, knowledge of some of our most critical marine ecosystems would not advance. We can no’t effectively manage what we do not understand.

Organisms such as gorgonian fans and other soft corals and anemones take over on hard canyon walls, such as this ancient limestone. As we move upslope into sunlit waters (shallower than ~200 m) we see red coralline algae plastered across rocky surfaces.