Atmospheric carbon & water recovery

Let the wind do the work of capturing carbon.

Oasys Systems is developing the Oasys Sail: a kilometer-scale sorbent mesh flown on tethered aerostats in high-wind coastal regions. Wind delivers the air. Moisture-swing chemistry releases the CO₂. Recovered atmospheric water closes the loop — and becomes a second product.

See how it works
~10 km²
Sorbent mesh area per sail, flown through moving air instead of waiting for still air to arrive
0.7–1.8 Mt CO₂/yr
Back-of-envelope capture estimate for a single sail — orders of magnitude beyond a still-air flat sheet
→ Gt/yr scale
A fleet of a few hundred sails approaches the annual removal the IPCC associates with direct air capture
Why we build

There is a thin blue film around this planet. Everything you have ever loved lives inside it.

Watch her. A polar bear, three days in open water, swimming through a sea that was ice within her own lifetime.1 Her kind spent hundreds of thousands of years mastering the frozen ocean3 — and in a handful of decades, we have melted the ground from under her. Somewhere ahead, she trusts, there is an ice-floe that will bear her weight. More and more often, there is only water, and she swims until she can swim no more. The longest recorded swim is nine days and 687 kilometres; that bear reached the ice having lost a fifth of her body, and her cub did not reach it at all.2 Nearly half the mothers tracked on such swims lost their young to the open sea.1 The cubs drown. The mothers that make it ashore are often too spent to hunt, and starve.

At the far end of the Earth, an emperor penguin chick stands where ten thousand generations stood before it, on ice that was meant to hold until it had grown its waterproof feathers. The ice no longer keeps its promise. In the spring of 2022 it broke up beneath four of the five colonies of the Bellingshausen Sea, weeks before a single chick had fledged. They dropped through into the water they were born to command — and they drowned, or froze, in their thousands. Not one is believed to have survived.4 Nearly a third of all known emperor colonies have now been struck by early ice loss, and the emperors of that region have declined by more than a fifth in fourteen years — faster than the worst models predicted.5

Do not mistake this for misfortune. This is the web of life being unpicked, thread by thread — and it is our hands pulling the threads. Even the ocean itself, the great patient ally that has swallowed more of the carbon we drill, pump and burn from oil and gas than every forest on Earth combined,6 is turning acid in silence. In the Southern Ocean and along the Pacific coast, the shells of the sea butterflies — the tiny swimming snails at the very base of the food web — are being eaten away while the animals inside them are still alive.7 Off California, the share of them dissolving has already doubled since the industrial age began, and is on course to triple.8 When the base of the web dissolves, everything built upon it goes hungry: the fish, the whales, the seabirds — and, in time, us. We are a strand in that same web. What we unravel, unravels us.

And in the frozen ground of Siberia, something older than any forest is beginning to stir. For thirty years, from a lonely research station on the Kolyma River, the Russian geophysicist Sergey Zimov has warned anyone who would listen that the permafrost is not merely ice. It is the deep-frozen remains of a vanished world — the grasses and beasts of the mammoth steppe, layered twenty-five metres deep across a million square kilometres.10 Frozen, it is harmless. Thawed, the microbes wake and breathe it out as carbon dioxide and methane. The Arctic permafrost holds roughly twice the carbon of the entire atmosphere — more than three times everything humanity has ever released from oil, gas and coal.11 Zimov once stripped the moss from a patch of ground near his station to show what comes next: within a decade it had collapsed into pits three metres deep, exhaling as it went. “This is the future we are facing,” he says, “if we cannot stabilize the permafrost.”10 The thaw has begun, and it does not negotiate. Which is why merely cutting what we emit will never be enough. The carbon already loosed must be drawn back down.

None of this is mystery. We drill oil and gas a hundred million years old out of the ground and hand their carbon to the sky faster than the living world can ever take it back. In 2025, we burned more of it than in any year in human history — and that tide is still rising.9

Oasys Systems is our answer. Not to mourn the breaking, nor merely to slow it — but to reverse it: to draw carbon down out of the sky with the wind itself, and to give back water to the places that thirst. The unravelling was done by human hands. So the mending must be.

Sources & citations
  1. Pagano, A.M., Durner, G.M., Simac, K.S., York, G. & Amstrup, S.C. (2012). Long-distance swimming by polar bears (Ursus maritimus) of the southern Beaufort Sea during years of extensive open water. Canadian Journal of Zoology 90(5): 663–676. Fifty swims by 20 bears, 0.7–9.7 days (mean 3.4 days); five of eleven mothers with cubs lost them. doi:10.1139/Z2012-033
  2. Durner, G.M., Whiteman, J.P., Harlow, H.J., Amstrup, S.C., Regehr, E.V. & Ben-David, M. (2011). Consequences of long-distance swimming and travel over deep-water pack ice for a female polar bear during a year of extreme sea ice retreat. Polar Biology 34: 975–984. The 687 km, nine-day swim; 22% body-mass loss; loss of yearling cub. doi:10.1007/s00300-010-0953-2
  3. Liu, S., Lorenzen, E.D., Fumagalli, M. et al. (2014). Population genomics reveal recent speciation and rapid evolutionary adaptation in polar bears. Cell 157(4): 785–794. Polar–brown bear divergence dated to roughly 343,000–479,000 years ago. doi:10.1016/j.cell.2014.03.054
  4. Fretwell, P.T., Boutet, A. & Ratcliffe, N. (2023). Record low 2022 Antarctic sea ice led to catastrophic breeding failure of emperor penguins. Communications Earth & Environment 4: 273. Total sea-ice loss in the Bellingshausen Sea in November 2022; probable complete breeding failure at four of five colonies; chicks fledge December–January. doi:10.1038/s43247-023-00927-x
  5. Fretwell, P.T. et al. (2025). Regional emperor penguin population declines exceed modelled projections. Communications Earth & Environment. 22% decline across the Bellingshausen and Weddell Seas, 2009–2023; ~30% of known colonies affected by early sea-ice loss (British Antarctic Survey). nature.com/articles/s43247-025-02345-7
  6. Friedlingstein, P. et al. (2025). Emerging climate impact on carbon sinks in a consolidated carbon budget. Nature. Revised budget: the ocean absorbed ~29% of anthropogenic CO₂ over 2015–2024 versus ~21% for the land sink; the ocean sink is ~15% larger than the land sink. doi:10.1038/s41586-025-09802-5
  7. Bednaršek, N., Tarling, G.A., Bakker, D.C.E. et al. (2012). Extensive dissolution of live pteropods in the Southern Ocean. Nature Geoscience 5: 881–885. doi:10.1038/ngeo1635
  8. Bednaršek, N., Feely, R.A., Reum, J.C.P. et al. (2014). Limacina helicina shell dissolution as an indicator of declining habitat suitability owing to ocean acidification in the California Current Ecosystem. Proceedings of the Royal Society B 281: 20140123. Share of pteropods with dissolving shells doubled since pre-industrial times; projected to triple by 2050. doi:10.1098/rspb.2014.0123
  9. Global Carbon Project (2025). Global Carbon Budget 2025 — fossil CO₂ emissions reach a new record in 2025. Friedlingstein, P. et al., Earth System Science Data. essd.copernicus.org/articles/17/965/2025 · Summary: Carbon Brief analysis
  10. Zimov, S.A., Schuur, E.A.G. & Chapin, F.S. III (2006). Permafrost and the global carbon budget. Science 312(5780): 1612–1613. Yedoma deposits >1 million km², ~25 m average depth; ~450–500 Gt carbon; up to 500 Gt releasable within a century under extreme but plausible warming. doi:10.1126/science.1128908 · Zimov quote and the Chersky thaw experiment: Andersen, E. (2015). “Born to rewild.” Science 350(6265): 1148–1151. doi:10.1126/science.350.6265.1148
  11. Schuur, E.A.G. et al. (2015). Climate change and the permafrost carbon feedback. Nature 520: 171–179. Northern permafrost holds 1,330–1,580 Pg C — roughly twice the atmosphere; a further ~400 Pg in deep sediments remains unquantified. doi:10.1038/nature14338 · Updated inventory 1,460–1,600 Pg C: NOAA Arctic Report Card 2019, Permafrost and the Global Carbon Cycle. Cumulative fossil-fuel emissions since 1850 (~480 Pg C): Global Carbon Budget, ref. 9.

On pteropods: recent work (Peck et al., 2018, Nature Communications) shows some species can partially repair dissolving shells — at a metabolic cost. The dissolution is real; the animals are not without defences. We state the science as it stands.

The concept

Air through the sorbent, not past it.

Conventional direct air capture spends most of its energy moving air. The Oasys Sail inverts that: it keeps proven moisture-swing sorbent chemistry but changes the geometry — from fixed tiles on a column to a permeable mesh held aloft where the wind already blows. When wind replaces fans and natural convection, throughput stops being limited by air delivery and starts being limited by engineering.

Wind-driven delivery

Tethered aerostats hold the sorbent mesh in persistent coastal winds. Air passes through the material continuously — no fans, minimal electricity, designed toward self-powered operation.

Moisture-swing capture

The sorbent binds CO₂ when dry and releases it when wet — the passive chemistry pioneered by Klaus Lackner. Captured atmospheric water drives the regeneration cycle and rinses the mesh clean.

Two products, one loop

Concentrated CO₂ for storage or synthetic fuels, and surplus recovered water as a second output — an oasis made from air, in the regions that need both.

Honest engineering

The concept isn't contradicted by physics. It's bottlenecked by engineering.

We publish the open questions because they define the work. These are the feasibility studies that would justify a pilot testbed.

Sorbent cycle life

Can a moisture-swing sorbent survive roughly 10⁵ wet/dry cycles — about 20 cycles a day for a decade — without losing working capacity? Published studies stop well short of that. This is the binding question.

Capture efficiency

The mesh must capture a meaningful fraction of the CO₂ in air moving through it — a target of η ≥ 0.3 at wind speeds around 10 m/s — without so much flow resistance that the wind simply goes around.

Structure & lift

Kilometer-scale aerostat architecture: tether loads, mesh tensioning, lift gas selection, and survival through storms in exactly the high-wind sites the concept depends on.

Collaborate

We're designing the feasibility studies now.

Oasys Systems is seeking collaborators across sorbent materials science, aerostat structures, and atmospheric modeling — and conversations with researchers, funders, and partners who want to pressure-test the numbers. Read the technical summary for the physics baseline, the sorbent shortlist, and the three feasibility gates.

Read the technical summary

ant@theixo.com