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New research sinks an old theory for the doldrums, a low-wind equatorial region that stranded sailors for centuries

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New research sinks an old theory for the doldrums, a low-wind equatorial region that stranded sailors for centuries


During the Age of Sail, sailors riding the trade winds past the equator dreaded becoming stranded in the doldrums, a meteorologically distinct region in the deep tropics. For at least a century, scientists have thought that the doldrums’ lack of wind was caused by converging and rising air masses. Now, new research suggests that the opposite may be true.

“The idea of what causes the doldrums came from a time where we didn’t know a lot about how air actually moves in the tropics,” said Julia Windmiller, an atmospheric scientist at the Max Planck Institute for Meteorology and the study’s author. “We have forgotten about the doldrums to such a degree that nobody has taken the trouble of thinking through this original argument again.”

Instead, Windmiller proposes that low wind speeds throughout the doldrums are created by large areas of sinking air that diverge at the surface, creating clear and windless days. Her explanation challenges the conventional explanation for the tropical, oceanic phenomenon that has stranded sailors, inspired poets and largely slipped out of scientific literature.

Traditionally, areas of low to no wind around the equator have been explained by converging and rising air masses. And while those air masses do create low-pressure, slow-wind areas at the surface, that idea can only explain the doldrums’ extended regions of low winds when many areas of convergence are averaged together over days or weeks. On the shorter timescales, converging air masses do not cover enough area to create large windless regions that can last for days — the doldrums.

The research was published in Geophysical Research Letters, an open-access AGU journal that publishes high-impact, short-format reports with immediate implications spanning all Earth and space sciences.

Deciphering the doldrums

The doldrums, also known as the Intertropical Convergence Zone, was named by early 19th century sailors marooned at sea by bouts of little or no wind. The term, originally defined as a period of despondency or depression, has come to describe the sometimes-stormy, sometimes-calm equatorial region. The oceanic area was even referenced in Samuel Taylor Coleridge’s 1834 poem, “The Rime of the Ancient Mariner”:

Day after day, day after day, We stuck, nor breath nor motion; As idle as a painted ship Upon a painted ocean.

The Intertropical Convergence Zone is usually characterized as a region of converging trade winds and rising air masses near the equator. The air masses, warmed by equatorial heat, float up like balloons, form clouds and whip up storms over the equator. They then sink back down at approximately 30 degrees North and South of the equator, completing what is known as Hadley Cell circulation. This pattern of converging and rising air near the equator has traditionally been accepted as the cause for the doldrums, as pockets of low to no winds are generally created under rising air masses.

However, little modern research has focused on proving the root cause of the doldrums. The accepted explanation for the doldrums could not be completely correct, Windmiller said, unless the regions of uplifting air were averaged over time.

“There’s this fascinating break in reasoning because this upward circulation of air doesn’t work for short time scales and large areas of still wind,” said Windmiller. “To some degree, because we’ve historically forgotten about the doldrums, this flaw in the logic never really came up.”

Windmiller analyzed Intertropical Convergence Zone meteorological data for the Atlantic Ocean between 2001 and 2021 and buoy data ranging from 1998 to 2018 to define the edges of the Intertropical Convergence Zone and investigate low wind speed events in the region. Low wind speed events are characterized by winds blowing slower than three meters per second, or five knots, for at least six hours. Windmiller examined the data on multi-day, hourly and minute-by-minute timescales, and considered how the low wind speed events evolved over time.

She found that low wind speed events coincided with clear weather conditions, lowered air temperatures and a lack of precipitation: conditions that point to sinking air masses diverging at the surface rather than rising air masses. Windmiller also found that low wind speed events mainly happen in the inner regions of the Intertropical Convergence Zone, and that they only occur on average in about 5% of the region at any given time (but can occur as often as 21% of the time in the eastern Atlantic during the Northern Hemisphere’s summer). Low wind speed locations also varied based on the season and region of the Atlantic Ocean.

“Most of the air inside the Intertropical Convergence Zone is actually going down rather than up,” said Windmiller. “It’s not just on average that we have low wind speeds in this region, but that we have these moments in time when the wind has just gone away over very large areas.”

Her idea is supported not just by scientific evidence, but by the next verse in Coleridge’s poem, which famously describes a ship’s stranding in a windless, rainless region within the doldrums:

Water, water, every where, And all the boards did shrink; Water, water, every where, Nor any drop to drink.

Upending an old explanation

For years, Windmiller has queried other atmospheric scientists about the doldrums: What really causes the wind to occasionally disappear around the equator?

“They would start to explain this upward circulation of air, but as they were explaining it, they often realized it didn’t actually make sense,” said Windmiller. “I was always surprised. It’s such a basic phenomenon, so why wouldn’t we have a theory for it?”

Some questions do remain. Windmiller is not certain what causes the Intertropical Convergence Zone’s large regions of sinking air. While most of the air in the tropics is slowly sinking, that effect alone may not be strong enough to cause the doldrums. Other possible causes include large convective systems that leave downdrafts in their wakes, or humidity gradients that cause local air to cool and sink, she said.

And while modern mariners are unlikely to be stranded in the doldrums thanks to diesel engines, understanding the doldrums’ true cause could still have present-day impacts. New, high-resolution climate models struggle to simulate regions of low wind speeds, so better understanding the doldrums could improve model predictions of precipitation and wind patterns.

“We can no longer explain these low wind speed events in the way we’ve done before,” said Windmiller. “I hope that this is something that people will see and read, and realize that the explanation is really upside down from what we’ve had.”



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Early dark energy could resolve cosmology’s two biggest puzzles

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New research sinks an old theory for the doldrums, a low-wind equatorial region that stranded sailors for centuries


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.

One puzzle in question is the “Hubble tension,” which refers to a mismatch in measurements of how fast the universe is expanding. The other involves observations of numerous early, bright galaxies that existed at a time when the early universe should have been much less populated.

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

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New research sinks an old theory for the doldrums, a low-wind equatorial region that stranded sailors for centuries


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.

It is well known that plants release volatile organic compounds (VOCs) into the atmosphere when damaged by herbivores. These VOCs play a crucial role in plant-plant interactions, whereby undamaged plants may detect warning signals from their damaged neighbours and prepare their defences. “Reactive plant VOCs undergo oxidative chemical reactions, resulting in the formation of secondary organic aerosols (SOAs). We wondered whether the ecological functions mediated by VOCs persist after they are oxidated to form SOAs,” said Dr. Hao Yu, formerly a PhD student at UEF, but now at the University of Bern.

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

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New research sinks an old theory for the doldrums, a low-wind equatorial region that stranded sailors for centuries


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.

Sulfur has been suggested as a material for lithium-ion batteries because of its low cost and potential to hold more energy than lithium-metal oxides and other materials used in traditional ion-based versions. To make Li-S batteries stable at high temperatures, researchers have previously proposed using a carbonate-based electrolyte to separate the two electrodes (an iron sulfide cathode and a lithium metal-containing anode). However, as the sulfide in the cathode dissolves into the electrolyte, it forms an impenetrable precipitate, causing the cell to quickly lose capacity. Liping Wang and colleagues wondered if they could add a layer between the cathode and electrolyte to reduce this corrosion without reducing functionality and rechargeability.

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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