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Major ocean current could warm greatly
A new study led by researchers at Binghamton University, State University of New York found that the Kuroshio Current Extension is sensitive to global climate change and has the potential to warm greatly with increased carbon dioxide levels.
Tracing a history written in water is the work of paleoceanographers such as Adriane Lam, Presidential Diversity Postdoctoral Fellow in Binghamton University’s Department of Geological Sciences and Environmental Studies. Lam is the lead author of “Pliocene to earliest Pleistocene (5-2.5 Ma) Reconstruction of the Kuroshio Current Extension Reveals a Dynamic Current,” recently published in the journal Paleoceanography and Paleoclimatology. Co-authors include Assistant Professor of Geological Sciences and Environmental Studies Molly Patterson, as well as Kenneth MacLeod of the University of Missouri, Solveig Schilling of the University of Texas at Austin, R. Mark Leckie of the University of Massachusetts Amherst, Andrew Fraass of England’s University of Bristol, and Nicholas Venti of the University of Delaware.
The major western boundary current in the northern Pacific Ocean, the Kuroshio Current and Extension, is analogous to the Gulf Stream, which flows along North America’s east coast. Driven by the wind, boundary currents are the workhorses of the ocean, moving heat, salt and gases from the equatorial seas to the middle latitudes, Lam explained.
“In other words, these currents help distribute heat from the tropics to higher latitudes. In fact, corals occur at their highest latitude of anywhere in the world within the Kuroshio Current because the waters are so warm,” she said.
That warmth stems from the surface waters that collect in the western Pacific Ocean along the equator, called the Western Pacific Warm Pool. The Kuroshio Current takes these waters north, past the Japanese coast, and then eastward at the 36°N latitude, where it joins the open Pacific Ocean. At this point, it becomes the Kuroshio Current Extension.
The current and extension vent vast amounts of heat and moisture evaporating from the warm water into the lower atmosphere in the Northern Hemisphere. Because of this, they help shape precipitation patterns over Japan and North America’s West Coast, as well as the paths of typhoons, which feed off warm waters. In addition to affecting the weather, the Kuroshio also likely affects the climate, although its impact on thousand- and million-year time scales is still unclear.
The Kuroshio also plays a major role in ecosystems and the fishing industry. In the northwest Pacific, it meets the Oyashio Current, which brings the cool waters of the polar region southward. Where the two currents meet, a strong temperature gradient forms due to the mixing of warm and cool waters. It also creates a region of upwelling, where nutrient-rich waters from the deep ocean are brought to the surface as the currents flow eastward.
It’s not just the waters that mingle: the warm- and cool-water organisms that live in the respective currents also flow together in a transition area between ecosystems, known as an ecotone. Its inhabitants include several species of fish and plankton, which ultimately power Japan’s prolific fishing industry and form a major part of that nation’s economy.
Because of their impact on biodiversity, weather and the climate, understanding how boundary currents such as the Kuroshio will respond to climate change and increasing CO2 levels in the atmosphere is critical. Today, these currents are warming two to three times faster than other areas of the ocean, Lam said.
Ocean model studies and observational data also show that the Kuroshio Current Extension is shifting northward and increasing its transport capacity, but researchers don’t yet know how these changes will affect the organisms that live there, or local and regional weather and climate patterns.
The recently published research is the first of its kind to reconstruct the Kuroshio as it was 2.5 to 5 million years ago, a time that spanned both periods of global warming and cooling, as well as the closure of a major seaway in what is now Central America. Looking at the current’s distant past may answer some of the questions about its future.
Past and future oceans
During the Pliocene, which spans 2.5 to 5.3 million years ago, atmospheric CO2 levels were near those we face today: about 350 to 450 parts per million. Today’s atmosphere has about 415 parts per million of CO2.
“The fun part of this time period is that the continents were arranged similar to today, which makes the Pliocene a great time period to use as an analogue as to how the Earth system will respond to increased CO2 concentrations and warming,” Lam said.
There were some differences in regard to landmasses, she noted: Until about 2.5 million years ago, a waterway existed between North and South America that allowed surface waters from the Pacific and Atlantic oceans to mingle. When the Central American Seaway closed, it may have brought the Kuroshio Current Extension into its current configuration.
The Pliocene included a period from 3 to 3.3 million years ago known as the mid-Piacenzian Warm Period (mPWP), which saw increased carbon dioxide levels and global warming. Once that period ended, cooling resumed, accompanied by the growth of glaciers and sea ice in the Northern Hemisphere’s high latitudes.
In the recently published study, the researchers reconstructed the Kuroshio throughout the mPWP, using chemical signatures from the fossilized shells of marine plankton that once lived in the Kuroshio region’s surface waters.
“Our data indicate that during the first phase of mPWP warming in the Pliocene, the current warmed up and potentially shifted its latitudinal position northward. It then cooled back down and perhaps shifted its position back south during a brief period of global cooling,” she said.
Reconstructing the current
Scientists use different techniques to reconstruct the history of an ocean current, depending on the time scale in question. For shorter timescales, they rely on observational data to see how a current’s path changes seasonally, from year to year or decade to decade. But when it comes to climate change, that dataset can fall short.
“This is why it is useful and necessary to reconstruct the behavior of western boundary currents through deep time, using the sedimentary record from millions of years ago,” Lam explained. “Through the lens of the sedimentary record, the shorter-term variations in the current are ‘smoothed’ or averaged out, so we are essentially only able to recover signals that indicate the longer-term, larger changes of the currents.”
In the study, the researchers used the chemical signals obtained from fossil plankton that lived in the surface ocean, as well as three deep-sea sediment cores from Shatsky Rise, a location on the northwest Pacific seafloor. Planktic foraminifera have lived in the open oceans for the last 170 million years; their durable shells, called “tests,” are made of calcium carbonate and accumulate on the ocean floor when they die.
In a previous study, Lam calculated the diversity of fossil plankton at each site used in the later chemical study. She found that diversity was highest at the northernmost site of Shatsky Rise, from 12 million years ago until today. This finding indicates the ecotone created by the current has been around for a very long time — and likely the Kuroshio has, too.
Researchers don’t know how warm the current became during the mPWP, or how much the chemical signal is affected by salinity as well as temperature changes. To get a better picture, Lam and colleagues from other SUNY schools are currently working on a grant that would use different chemical methods to answer these questions.
“The ocean is hugely affected by climate change, and we must think about ways in which we can protect it and marine organisms. This is especially true for the Kuroshio Current Extension, as this region is home to some of the highest biodiversity in our world ocean,” Lam said.
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Early dark energy could resolve cosmology’s two biggest puzzles
A new study by MIT physicists proposes that a mysterious force known as early dark energy could solve two of the biggest puzzles in cosmology and fill in some major gaps in our understanding of how the early universe evolved.
Now, the MIT team has found that both puzzles could be resolved if the early universe had one extra, fleeting ingredient: early dark energy. Dark energy is an unknown form of energy that physicists suspect is driving the expansion of the universe today. Early dark energy is a similar, hypothetical phenomenon that may have made only a brief appearance, influencing the expansion of the universe in its first moments before disappearing entirely.
Some physicists have suspected that early dark energy could be the key to solving the Hubble tension, as the mysterious force could accelerate the early expansion of the universe by an amount that would resolve the measurement mismatch.
The MIT researchers have now found that early dark energy could also explain the baffling number of bright galaxies that astronomers have observed in the early universe. In their new study, reported in the Monthly Notices of the Royal Astronomical Society, the team modeled the formation of galaxies in the universe’s first few hundred million years. When they incorporated a dark energy component only in that earliest sliver of time, they found the number of galaxies that arose from the primordial environment bloomed to fit astronomers’ observations.
“You have these two looming open-ended puzzles,” says study co-author Rohan Naidu, a postdoc in MIT’s Kavli Institute for Astrophysics and Space Research. “We find that in fact, early dark energy is a very elegant and sparse solution to two of the most pressing problems in cosmology.”
The study’s co-authors include lead author and Kavli postdoc Xuejian (Jacob) Shen, and MIT professor of physics Mark Vogelsberger, along with Michael Boylan-Kolchin at the University of Texas at Austin, and Sandro Tacchella at the University of Cambridge.
Big city lights
Based on standard cosmological and galaxy formation models, the universe should have taken its time spinning up the first galaxies. It would have taken billions of years for primordial gas to coalesce into galaxies as large and bright as the Milky Way.
But in 2023, NASA’s James Webb Space Telescope (JWST) made a startling observation. With an ability to peer farther back in time than any observatory to date, the telescope uncovered a surprising number of bright galaxies as large as the modern Milky Way within the first 500 million years, when the universe was just 3 percent of its current age.
“The bright galaxies that JWST saw would be like seeing a clustering of lights around big cities, whereas theory predicts something like the light around more rural settings like Yellowstone National Park,” Shen says. “And we don’t expect that clustering of light so early on.”
For physicists, the observations imply that there is either something fundamentally wrong with the physics underlying the models or a missing ingredient in the early universe that scientists have not accounted for. The MIT team explored the possibility of the latter, and whether the missing ingredient might be early dark energy.
Physicists have proposed that early dark energy is a sort of antigravitational force that is turned on only at very early times. This force would counteract gravity’s inward pull and accelerate the early expansion of the universe, in a way that would resolve the mismatch in measurements. Early dark energy, therefore, is considered the most likely solution to the Hubble tension.
Galaxy skeleton
The MIT team explored whether early dark energy could also be the key to explaining the unexpected population of large, bright galaxies detected by JWST. In their new study, the physicists considered how early dark energy might affect the early structure of the universe that gave rise to the first galaxies. They focused on the formation of dark matter halos — regions of space where gravity happens to be stronger, and where matter begins to accumulate.
“We believe that dark matter halos are the invisible skeleton of the universe,” Shen explains. “Dark matter structures form first, and then galaxies form within these structures. So, we expect the number of bright galaxies should be proportional to the number of big dark matter halos.”
The team developed an empirical framework for early galaxy formation, which predicts the number, luminosity, and size of galaxies that should form in the early universe, given some measures of “cosmological parameters.” Cosmological parameters are the basic ingredients, or mathematical terms, that describe the evolution of the universe.
Physicists have determined that there are at least six main cosmological parameters, one of which is the Hubble constant — a term that describes the universe’s rate of expansion. Other parameters describe density fluctuations in the primordial soup, immediately after the Big Bang, from which dark matter halos eventually form.
The MIT team reasoned that if early dark energy affects the universe’s early expansion rate, in a way that resolves the Hubble tension, then it could affect the balance of the other cosmological parameters, in a way that might increase the number of bright galaxies that appear at early times. To test their theory, they incorporated a model of early dark energy (the same one that happens to resolve the Hubble tension) into an empirical galaxy formation framework to see how the earliest dark matter structures evolve and give rise to the first galaxies.
“What we show is, the skeletal structure of the early universe is altered in a subtle way where the amplitude of fluctuations goes up, and you get bigger halos, and brighter galaxies that are in place at earlier times, more so than in our more vanilla models,” Naidu says. “It means things were more abundant, and more clustered in the early universe.”
“A priori, I would not have expected the abundance of JWST’s early bright galaxies to have anything to do with early dark energy, but their observation that EDE pushes cosmological parameters in a direction that boosts the early-galaxy abundance is interesting,” says Marc Kamionkowski, professor of theoretical physics at Johns Hopkins University, who was not involved with the study. “I think more work will need to be done to establish a link between early galaxies and EDE, but regardless of how things turn out, it’s a clever — and hopefully ultimately fruitful — thing to try.”
“We demonstrated the potential of early dark energy as a unified solution to the two major issues faced by cosmology. This might be an evidence for its existence if the observational findings of JWST get further consolidated,” Vogelsberger concludes. “In the future, we can incorporate this into large cosmological simulations to see what detailed predictions we get.”
This research was supported, in part, by NASA and the National Science Foundation.
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Plant-derived secondary organic aerosols can act as mediators of plant-plant interactions
A new study published in Science reveals that plant-derived secondary organic aerosols (SOAs) can act as mediators of plant-plant interactions. This research was conducted through the cooperation of chemical ecologists, plant ecophysiologists and atmospheric physicists at the University of Eastern Finland.
The study showed that Scots pine seedlings, when damaged by large pine weevils, release VOCs that activate defences in nearby plants of the same species. Interestingly, the biological activity persisted after VOCs were oxidized to form SOAs. The results indicated that the elemental composition and quantity of SOAs likely determines their biological functions.
“A key novelty of the study is the finding that plants adopt subtly different defence strategies when receiving signals as VOCs or as SOAs, yet they exhibit similar degrees of resistance to herbivore feeding,” said Professor James Blande, head of the Environmental Ecology Research Group. This observation opens up the possibility that plants have sophisticated sensing systems that enable them to tailor their defences to information derived from different types of chemical cue.
“Considering the formation rate of SOAs from their precursor VOCs, their longer lifetime compared to VOCs, and the atmospheric air mass transport, we expect that the ecologically effective distance for interactions mediated by SOAs is longer than that for plant interactions mediated by VOCs,” said Professor Annele Virtanen, head of the Aerosol Physics Research Group. This could be interpreted as plants being able to detect cues representing close versus distant threats from herbivores.
The study is expected to open up a whole new complex research area to environmental ecologists and their collaborators, which could lead to new insights on the chemical cues structuring interactions between plants.
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Folded or cut, this lithium-sulfur battery keeps going
Most rechargeable batteries that power portable devices, such as toys, handheld vacuums and e-bikes, use lithium-ion technology. But these batteries can have short lifetimes and may catch fire when damaged. To address stability and safety issues, researchers reporting in ACS Energy Letters have designed a lithium-sulfur (Li-S) battery that features an improved iron sulfide cathode. One prototype remains highly stable over 300 charge-discharge cycles, and another provides power even after being folded or cut.
The team coated iron sulfide cathodes in different polymers and found in initial electrochemical performance tests that polyacrylic acid (PAA) performed best, retaining the electrode’s discharge capacity after 300 charge-discharge cycles. Next, the researchers incorporated a PAA-coated iron sulfide cathode into a prototype battery design, which also included a carbonate-based electrolyte, a lithium metal foil as an ion source, and a graphite-based anode. They produced and then tested both pouch cell and coin cell battery prototypes.
After more than 100 charge-discharge cycles, Wang and colleagues observed no substantial capacity decay in the pouch cell. Additional experiments showed that the pouch cell still worked after being folded and cut in half. The coin cell retained 72% of its capacity after 300 charge-discharge cycles. They next applied the polymer coating to cathodes made from other metals, creating lithium-molybdenum and lithium-vanadium batteries. These cells also had stable capacity over 300 charge-discharge cycles. Overall, the results indicate that coated cathodes could produce not only safer Li-S batteries with long lifespans, but also efficient batteries with other metal sulfides, according to Wang’s team.
The authors acknowledge funding from the National Natural Science Foundation of China; the Natural Science Foundation of Sichuan, China; and the Beijing National Laboratory for Condensed Matter Physics.
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