GRID Β· FIELD GUIDE

The Water Cost of Compute β€” Why Data Centres and Water Stress Collide

A data centre full of AI accelerators throws off enormous heat, and a great deal of the world still carries that heat away with water β€” sometimes millions of litres a day at a single large site. So when a new campus is announced, there's a second question hiding behind the headline megawatts: is there water where it's going? This guide is about how to read the world's watersheds for that answer.

LEV Grid DeskUpdated June 25, 20266 min read
See it on the Water Stress mapOpen β†’

There's a number that rarely makes the press release. When a new AI data centre is announced, the headline figure is power β€” hundreds of megawatts, sometimes more than a small city draws. But all of that electricity ends up as heat, and a great deal of the world still carries that heat away with water. A single large site running evaporative cooling can turn millions of litres a day into vapour. So behind every megawatts-and-jobs announcement sits a quieter question: is there water where this is going?

This guide is about reading the water-stress map for that answer β€” and about why the new wave of data centres so often lands in exactly the places where water is already tight.

Compute is a thermal problem

It's easy to think of a data centre as a building full of computers. It's more useful to think of it as a building full of heaters. Every watt of electricity a server draws comes back out as heat, and the dense racks used for AI training throw off far more heat per square metre than the web servers of a decade ago. Keeping the chips inside their safe temperature range is half the engineering of a modern facility.

There are a few ways to do it, and they trade water against energy. Evaporative (or "swamp") cooling sprays or trickles water so that, as it evaporates, it pulls heat out of the air β€” cheap and effective, but it consumes the water. Air cooling uses fans and chillers instead, sparing water but spending more electricity. Newer closed-loop liquid systems circulate the same coolant over and over, and some sites run on recycled or non-potable water. Across the fleet that already exists, though, a large share of cooling still leans on fresh water β€” and that's before counting the water used at the power plants supplying the electricity, many of which need cooling water of their own. (That second link is why the power-plants layer belongs in the same conversation.)

The upshot is simple: more compute, in most of today's world, means more water demand β€” and where you put the compute decides whose water it draws on.

What "water stress" actually measures

The map colours the world by baseline water stress, the headline indicator from the World Resources Institute's Aqueduct project. The idea is a ratio: how much water people withdraw from a basin, divided by how much renewable water that basin has. Aqueduct sorts every watershed into bands β€” low is under a tenth of the available water withdrawn; extremely high is over four-fifths, meaning almost all the renewable supply is already spoken for and there's almost no slack for a drought or a thirsty new user.

A class apart is arid & low water use β€” the deserts. These basins have very little water, but they also have very little demand, so they're neither comfortably supplied nor overdrawn; the map gives them their own neutral shade rather than forcing them onto the stress ramp. And where the underlying data runs out, a basin is simply left unfilled rather than shown as a guess, so empty land means low stress or not assessed, never "we made something up." That's the honesty rail this whole project runs on.

Across the roughly 15,800 assessed watersheds, a little over 17% already sit at medium-high stress or worse β€” a minority of the map, but a consequential one, because that's where almost all the friction lives.

Why the map is drawn by watershed, not by country

The single most important design choice here is the unit. It would be easy to colour countries β€” the data exists at that level β€” but a national average is exactly the wrong lens for this question, because water doesn't follow borders.

Take the United States. As a whole it's moderate. But that average quietly blends the water-rich East with the chronically overdrawn basins of the Southwest, and a country-coloured map would paint Phoenix the same shade as Pittsburgh. The entire point of the overlay β€” that a specific cluster of data centres sits in abundant or in scarce water β€” would vanish into the average.

So this map keeps Aqueduct's native unit, the sub-basin: a watershed defined by the land that drains to a common point, not by a line on a political map. It's both the honest choice and the practical one. It's the resolution at which you can put a data-centre dot down and read its real water situation β€” which is the whole reason to fuse the two layers.

That sub-basin view does throw up a couple of results that look surprising until you understand them. Las Vegas reads low, despite its reputation, because it's a small demand sitting in an enormous, near-empty desert basin β€” its genuine constraint is its slice of Colorado River water, a matter of reservoirs and interstate law rather than local supply. Singapore reads low because it imports much of its water and recycles relentlessly β€” a real exposure that a basin-supply number can't see. Neither is a bug; both are reminders that this is a map of physical basin stress, one lens on water risk, not the whole of it.

The collision: where compute meets scarcity

Now lay the two layers over each other, and the reason for all of this becomes obvious.

The data centres cluster where land, power and fibre are cheap and where the customers are β€” and those places are not chosen for their water. The result is a set of striking contrasts. Northern Virginia's Ashburn β€” "Data Centre Alley," the densest concentration of server halls on Earth β€” sits on comfortably low stress. The fast-growing campuses around Phoenix, drawn by cheap land and solar power, sit in extremely high stress. Same country, opposite ends of the water budget.

Zoom out and the pattern hardens. Rank the world by the sheer area of land under high or extremely high stress and the leaders are China, the United States and India β€” which are also, not coincidentally, the three countries building the most compute. The new data centres and the scarce water are converging on the same map. That's not a forecast of disaster; plenty of those projects will use air cooling, recycled water or sites with genuine supply. But it's precisely the tension this overlay exists to make visible β€” and it's why "how many megawatts" is only ever half the question.

How to use the layer

Open the Grid map, switch on Water Stress, and then switch on Data Centres as well. Read the watersheds first β€” the dark globe stays calm where water is abundant, and glows amber to red where withdrawals are pressing against supply. Then read the data-centre bubbles against that backdrop: a dot on dark is a campus with water to spare; a dot on deep red is one competing for a basin that's already nearly fully drawn.

It pairs naturally with the rest of the Grid. The power-plants layer adds the generators that also drink water; the carbon-intensity layer adds how clean the electricity behind it all is. Together they're a way of asking the fuller question about the build-out β€” not just where the compute is going, but what it costs the place it lands in.

Frequently asked questions

Why do data centres need water at all?

Servers turn electricity into heat, and that heat has to go somewhere. Many large data centres β€” especially the dense, hot racks used for AI β€” are cooled by evaporating water, which is very effective but consumes it: a single large site can evaporate on the order of millions of litres a day at full tilt. There's a second, indirect draw too: the power stations supplying the electricity often use cooling water of their own, so a data centre's true water footprint includes the water used to generate its power. Newer designs cut this with air cooling, closed-loop liquid cooling or recycled water, but across the existing fleet, compute and water are tightly linked β€” which is why it's worth knowing whether a basin has water to spare.

What exactly does 'baseline water stress' mean?

It's the ratio of how much water people withdraw from a basin to how much renewable water that basin has available β€” roughly, demand divided by supply. WRI's Aqueduct framework sorts every watershed into bands: low is under 10% of available water withdrawn, and extremely high is over 80%, meaning almost all the renewable water is already being used and there's very little slack for a dry year or a new large user. It's a measure of how tight the local water budget is, not of drinking-water quality or flood risk β€” those are separate indicators.

Why colour watersheds instead of countries?

Because water doesn't follow borders, and national averages hide the thing that matters. The United States as a whole is moderate, but that average blends water-rich Appalachia with the overdrawn basins of the Southwest β€” so a country-coloured map would paint Phoenix the same as Pittsburgh and lose the entire story. Aqueduct works at the level of the sub-basin (a HydroBASINS Level-6 watershed), and this map keeps that native unit. It's both the honest choice and the useful one: it's the resolution at which a specific data-centre cluster sits in clearly abundant or clearly scarce water.

Why do Las Vegas and Singapore show up as low stress?

Both are famous for water scarcity, so they look like errors β€” but they're showing exactly what the indicator measures, which is local basin supply against local withdrawals. Las Vegas is a relatively small demand sitting in a vast, nearly empty desert basin, so the local ratio is low; its real constraint is its allocation of Colorado River water, which is a matter of reservoirs and interstate politics, not local supply. Singapore reads low because it imports much of its water and recycles aggressively β€” an exposure that a basin-supply indicator simply doesn't capture. The lesson is to read this as a map of physical basin stress, and to remember it's one lens on water risk, not all of them.

Is this a live, real-time layer?

No, and we badge it as exactly that. Baseline water stress is a modelled risk index from WRI Aqueduct 4.0 (the 2023 release), built from long-run hydrological data β€” it describes the standing condition of each basin, not today's reservoir level, so it doesn't tick over minute to minute the way the live grid layers do. Watersheds without enough input data are dropped rather than shown as a guess, which is why some land is left unfilled. It's the right tool for the question 'is this a water-scarce place to build,' and the wrong tool for 'how much water is in the lake this afternoon.'

SEE IT LIVE

Everything in this guide is on the live map β€” explore the world’s data centres for yourself.

Open the water stress map β†’