Exploring the upper ocean

Tandon Laboratory at UMass Dartmouth

Month: August 2021

JGR-Oceans paper published on “Revisiting the Atlantic South Equatorial Current”

A paper published on June 17, 2021 by Caique Luko, an oceanographer at the University of São Paulo, Brazil and colleagues including Iury Simoes-Sousa, PhD Candidate at UMass Dartmouth and Prof Tandon (Caique’s co-advisor in his Master’s thesis) in JGR-Oceans reveal that the southern branch of the South Equatorial Current is a multi-banded flow with surface signatures arising from different subsurface cores (Figure 1).

Figure 1: (a) Horizontal distribution of the geostrophic velocities mean field derived from altimetry data. Gray shaded area masks regions shallower than 100 m, and background gray shading highlights regions shallower than 4,000 m. (b) Meridional section of the zonal velocities at 30°W (blue line in panel a). (c) Horizontal distribution of the geostrophic velocities mean field zoomed in to the region of the Brazil Current origin site (blue dashed box in panel a)

“The SSEC is an ocean current that flows from Africa to South America. It consists on the northern limit of the South Atlantic Subtropical Gyre. This current is the main pathway that connects waters from the Pacific and Indian Oceans to the tropical Atlantic western boundary currents supply (Brazil Current and North Brazil Undercurrent). By feeding both currents, the SSEC can affect the global climate since the SSEC-North Brazil Undercurrent-North Brazil Current system is an element of the upper portion of the Meridional Overturning Circulation. In fact, the SSEC constitutes an important source of warm water to the North Atlantic, which explicits its importance to global climate.”

Figure 2: 3-D depiction of the complexity of incoming SSECjets that form the WBCs off
the coast of Brazil. Extracted from Soutelino et. al (2013). SEC: South Equatorial Current; BC: Brazil Current; NBUC: North Brazil Undercurrent; NBC: North Brazil Current; IWBC: Intermediate Western Boundary Current; DWBC: Deep Western Boundary Current; TW: Tropical Water; SACW: South Atlantic Central Water; AAIW: Antarctic Intermediate Water; NADW: North Atlantic Deep Water.

Originally, the southern branch of the South Equatorial Current (SSEC) was thought to be a broad sluggish jet that narrowed and shifted its bifurcation point poleward with increasing depth (Figure 2). However, by analyzing satellite data and reanalyses outputs, Caique and the co-authors showed that, actually, the SSEC is a multi-banded flow that extends its vertical extension and deepens its core depth with increasing latitudes (Figures 1 and 3).

Figure 3: Mean zonal velocity vertical section at 32°W derived from: (a) GLORYS12V1; (b) FOAM-GloSea5; (c) ORAS5; and (d) C-GLORS05. Red dashed boxes delimit the specified SSEC sectors. Solid (dashed) contours represent positive (negative) velocities, and contour intervals are of 0.005 m s ⁻¹ .

“This work gives more detail to the SSEC mean state and annual cycle, as well as its impacts on the western boundary circulation off Eastern Brazil. However, there is still a lot of work to be done. We still do not know what causes this distinct multi-banded pattern to occur. Furthermore, as the SSEC is a key component to global climate, we must ask: Does this flow change its structure in a changing climate, and what would be the consequences of these possible alterations? Finally, we observed that the SSEC seasonality modulates the annual cycle of semi-permanent mesoscale eddies off Brazil. A question that must be posed is: Does this observed variability impact the regional planktonic dynamics?”

To read more about this research access: click here

High-resolution turbulence measurements reveal a large-scale mixing hotspot in the Kuroshio flowing seamounts south of Kyushu Japan

A recent paper published August 23, 2021, in the journal, Nature: Communication, Earth & Environment by Takeyoshi Nagai, an oceanographer at Tokyo University of Marine Science and Technology, Japan and colleagues including Prof. Amit Tandon at UMassD, who was Takeyoshi’s mentor 17 years ago, reveal an unprecedented long-lasting vigorous turbulent streak over 100 km along the Kuroshio Current in the North Pacific, flowing over the seamounts in the Tokara Strait south of Kyushu Japan. This long-lasting turbulent streak cannot be explained by previous turbulence theories for ocean interior that consider only velocity vertical gradient of internal waves as the major source of turbulence. By conducting a series of intensive turbulence observations and numerical simulations, the authors find submesoscale (a few hundred meters – a few kilometers) instability caused by the Kuroshio flowing over steep seamounts can extract energy of the Kuroshio through its velocity gradients along horizontal as well as vertical directions and inject it to microscale (a few millimeters – a few 10th of meters) turbulence.

Sunset over islands in south of Kyushu (Kagoshima). There are many volcanic islands and seamounts where the Kuroshio Current flows.

“Our finding may have big implications for understanding how the wind-driven ocean general circulation is maintained and how the interior of the ocean is mixed. Both remain uncertain for decades, and the latter is very important for nutrient supply for phytoplankton” says Tandon.

Ocean general circulation, that consists of numerous mesoscale eddies and large scale major ocean currents, is driven by about 1 TW power input by wind. To achieve its equilibrium, energy has to be dissipated at the same rate. The energy dissipation can occur by fluid friction only at the smallest scale, microscale (a few millimeters – a few 10th of meters), while large scale flows tend to transfer energy to larger scale. Therefore, it has been a puzzle on how the energy of the general circulation reach to the scale to the dissipation. One of the candidates is the lee waves. Lee waves can be generated by ocean currents flowing over the bottom topography. Several studies pointed out that lee waves can extract energy from general circulation at a rate about 0.2 TW. However, a previous study suggested that a large fraction of the lee wave energy is not dissipating near the generation sites and radiates away. These radiated waves can be reabsorbed to the large scale ocean current and do not necessarily dissipate their energy.

Takeyoshi continues “The missing pieces could be hidden in the submesoscale”. The submesoscale processes have spatial scale that ranges from a few hundred meters to a few kilometers, which is in between microscale (a few millimeters – a few 10th of meters) and mesoscale (a few 10th of kilometers – a few hundred meters), both are relatively well-explored. “We are now very exciting era, in which observationally and numerically resolvable scales are emerging both from microscale and mesoscale toward the submesoscale.  Tandon sensei said this when I joined him as a Postdoctoral fellow at UMassD, and it got me very interested. I have been working on the submesoscale observationally and numerically since then” said by Takeyoshi. The word “sensei” means teacher in Japanese.

Their paper finds that when the Kuroshio flows over the steep seamounts in the Tokara Strait, clockwise spinning flow, in opposite sense to the Earth’s spinning, is generated from one side of the slopes, producing a streak of water spinning clockwise that triggers submesoscale instability, called inertial and symmetric instabilities and associated strong microscale turbulence. Although these instabilities have been reported along the continental slopes in the abyssal Southern Ocean, there has been no observational evidence that this mechanism provides a large scale mixing hotspot in the major ocean currents flowing over seamounts in relatively shallow layers until this study.

Picture 1: Tow-yo turbulence profiler, Underway-VMP, which consists of VMP250 (Rockland Scientific International) and UCTD Winch (Teledyne Ocean Science)

Turbulence is intermittent. That’s why scientists need to measure it at high spatial resolution to know where mixing occurs. But measuring turbulence is not easy, because turbulence probes are very sensitive and easily detect unwanted signals caused by instrument motions by rope’s tension. “In fact, it can detect noises of your steps when it placed at the lab” says Takeyoshi. His team developed the method to measure turbulence at 1-2 km horizontal resolution using a tow-yo microstructure profiler (Picture 1) without stopping a ship. They use 1.5 mm diameter Dyneema rope to let it sink quasi-freely without severe unwanted contamination from the rope’s tension and recover it to the surface repeatedly while a ship is steaming at a slow speed, 1-2 m/s. While yo-yo profiling is to keep deploying and recovering the instrument vertically at one location like a yo-yo, this method is called tow-yo profiling. Using this new technique and Training vessel Kagoshima-Maru (Kagoshima University, Picture 2), the authors and participants of cruises (Picture 3) find the enhanced turbulence by 100-1000-fold compared to typical interior ones, that spreads over 100 km scale along the Kuroshio behind the seamounts.


Picture 2: Training vessel Kagoshima-Maru (Kagoshima University)

Picture 3: Group photos of the Kagoshima-Maru cruises











Takeyoshi continues “Our finding may have very important implications in nutrient supply to the Kuroshio, and this could be a key to solve the Kuroshio Paradox”. The Kuroshio surface water is known to be nutrient poor and yet many fish species spawn in the regions southwest of Kyushu where their eggs and larvae are advected from by the nutrient poor Kuroshio Current and utilize the Kuroshio to migrate north. Nutrient depletion usually means less food availability for higher trophic levels. Why many fish species spawn there, risking their larva’s lives under food depleting environment? Why are there so many fish in the Kuroshio regions, one of the major fishing sites of the North Pacific, even with less food? This has been called the “Kuroshio Paradox”. The observed strong turbulence can inject nutrients, which are abundant in the deeper layers of the Kuroshio, toward the sunlit surface, where phytoplankton can photosynthesize. Then, zooplankton eat phytoplankton and are eaten by fish in the downstream. But the question remains why the Kuroshio surface water remains nutrient poor even with the observed large nutrient injection. “This is probably because these biological responses are happening in the subsurface layers. Also, another recent study pointed out that these trophic transfers may occur very rapidly in nutrient depleted environment. In other words, as everybody is so hungry, they eat as fast as possible so that nobody can see it. We need to have more observations to figure this out” Takeyoshi said.

This is not the end of the story, because the Kuroshio and the Kuroshio Extension regions are found to be one of the major net CO2 sinks for the Earth’s atmosphere. The diffused nutrients toward the shallower layers and associated phytoplankton growth are very important for the CO2 uptake in these regions. “However, climate model predicts the upper layers of these regions will be warmed leading to more strongly stratified layers, which will become more difficult to mix by turbulence within several decades. If this is the case, then phytoplankton will decrease and CO2 uptake in these regions will also decline. Furthermore, dependent higher trophic levels including commercially valuable fish are expected to decrease too” said by Takeyoshi.

ONR (N0014-18-1-2799) supported Prof. Amit Tandon for this work. Also, check out the videos which explain this particular phenomenon visually. The paper can be found here


Skip to toolbar