Plain language, no background needed

Sea level rise, explained plainly

Most explanations of sea level rise are either too vague to be useful or too technical to follow. This page is neither. It answers the questions people actually ask, defines every term the first time it appears, and corrects the three misunderstandings that come up most often.

The short version

  • Melting sea ice does not raise sea level. It is already floating. Only ice that sits on land counts, and that is Greenland and Antarctica.
  • Miami cannot be saved by a sea wall. The ground is porous limestone, so water arrives from underneath rather than over the shore.
  • The land is also sinking, adding roughly half a foot by 2100 no matter what anyone does about emissions.
  • Before about 2070, cutting emissions barely changes the number. That is not a reason to do nothing. It means the near-term uncertainty lives in the ice, not in policy.

What actually raises sea level

Two things, in roughly equal measure so far.

Water gets bigger when it warms. Not a lot, but the ocean is enormous, so a small expansion across an enormous volume adds up. This is called thermal expansion.

Ice that sits on land melts and runs into the sea. That is new water arriving. This is the part that can get dramatic, because Greenland and Antarctica hold enough ice to raise the ocean by many metres if they were ever to go entirely.

And one thing that does not raise sea level at all, despite being the image everyone pictures: floating sea ice.

Two glasses of water showing that floating ice does not raise the level but ice resting on a shelf does On the left, an ice cube floats in a glass; when it melts the water level is unchanged, because floating ice already displaces its own weight. On the right, an ice block rests on a ledge above the water; when it melts the water level rises, because that water was not in the glass before. Floating ice (sea ice) Melts, level unchanged ← level stays put Ice on land (ice sheets) Melts, level rises ← rises was here
Put an ice cube in a full glass and let it melt: the level does not change, because floating ice already pushes aside exactly its own weight in water. Now rest an ice cube on a ledge above the glass. When that melts, the level rises, because you added water that was not in the glass before. Sea ice is the first glass. Greenland and Antarctica are the second.

Why Miami is a special case

Most coastal cities can, in principle, build something. A wall, a barrier, a raised shoreline. Miami largely cannot, and the reason is geology rather than money or will.

South Florida sits on porous limestone. It is full of tiny connected holes, more like a hard sponge than like solid rock. Seawater moves through it. That has two consequences that most people find surprising.

First, a wall does not help much. If the barrier is on the shoreline but the water can travel underneath it through the rock, you have not stopped the water. You have only changed where it appears.

Second, the ground water underneath the city rises with the sea. That matters because the storm drains are already sitting in it. In this project's own measurements, more than half of the drainage structures with a known bottom depth already sit below the wet-season water table. The drains are not empty pipes waiting for rain. They are partly full before the first drop lands, which is why a heavy downpour on a normal sunny day can still flood a street.

Cross-section of Miami showing seawater moving through porous limestone under a sea wall A sea wall stands at the shoreline. Below ground, the limestone is porous, and arrows show seawater passing beneath the wall and pushing the ground water table upward under the city. Storm drains sit inside that raised water table, so they are already partly full before any rain falls. Sea Downtown Miami sea wall porous limestone (water moves through it) ground water table seawater passes underneath storm drain, already partly full
Water arrives from below, not just over the edge. This is why Miami floods on clear days at high tide, and why the storm drains cannot be treated as empty capacity when the rain starts.

What El Niño has to do with it

El Niño is a recurring warming of the surface water in the middle of the tropical Pacific Ocean. It shows up every few years, lasts roughly a year, and shifts weather patterns worldwide. Its opposite, a cooling, is called La Niña.

Here is the part that catches people out, including people who build dashboards for a living. During a strong El Niño, the floating ice shelves around West Antarctica get taller and lighter at the same time.

Taller, because the weather pattern brings more snow, which piles on top. Lighter, because warmer water reaches in underneath and melts them from below. Height goes up. Mass goes down.

So if you measured only the height of that ice, from a satellite, during exactly the period it was losing the most mass, your instrument would tell you it was growing. Same ice, same moment, two honest measurements, opposite conclusions.

That is the single best reason to be careful with confident-looking numbers, and it is why the monitor on this site labels what each measurement can and cannot tell you.

An ice shelf gaining height from snowfall while losing mass to warm water melting it from below Snow falls on top of a floating ice shelf, increasing its height, shown by an upward arrow. At the same time warm Circumpolar Deep Water flows in underneath and melts the base, shown by a downward arrow for mass. The two arrows point in opposite directions, so a height measurement and a mass measurement disagree. grounded ice floating ice shelf HEIGHT goes up (snow) warm deep water melts the underside MASS goes down (melt)
Height and mass move in opposite directions during a strong El Niño. Only mass affects sea level. This is why the monitor treats "we could not measure the mass" as important news rather than a minor gap.
Where the Pacific is right now
loading current conditions

Two numbers are shown because they answer different questions. The weekly figure is the ocean roughly a week ago. The official index averages three months and is centred about two months back, so during a strengthening event it always reads lower. Neither is wrong. They measure different things, and a page that showed only one would be quietly picking an answer for you.

Three things people get wrong

Not true"The Arctic ice is melting, so the sea will rise."

Arctic sea ice is floating, so its melting adds essentially nothing to sea level. It matters enormously for other reasons: it reflects sunlight, it shapes weather, and its loss lets ocean waves reach places they could not reach before.

But if you want to know about sea level, watch Greenland and Antarctica, where the ice rests on rock.

Not true"Insurance companies would be fleeing if this were real."

This project searched for that specific evidence in six independent ways, including a US Senate investigation covering 249 million policy records. No insurer has ever given sea level rise as its reason for leaving a market. Not once.

That sounds like reassurance. It is not. Home insurance is sold one year at a time, so a slow-moving hazard never needs to be announced. It gets quietly priced in, renewal by renewal, or the policy simply is not offered again. A hazard that arrives over decades is invisible in a market that re-prices every twelve months. The silence is what the mechanism predicts.

True, but"Cutting emissions will not change much by 2050."

Broadly correct, and routinely misused. Every major emissions scenario gives nearly the same sea level in 2050, because the ocean and ice respond slowly to what we do. The paths separate after about 2070.

What follows from that is the opposite of "so it does not matter." Choices made now determine the second half of the century, when the paths are far apart. And near-term uncertainty is not small, it just lives somewhere else: in how the ice sheets behave, which is exactly what is hardest to predict and what this site watches.

How to read the monitor without being misled

The ice monitor shows live numbers. Live is not the same as important, and the difference is worth ten seconds of your attention.

Check the lag before the value. Every tile says when the instrument actually observed the thing, and how far behind that is now. A number is not fresh because a web page loaded.

Check whether it raises sea level at all. Sea ice tiles are marked as context. They update daily and look urgent, and they contribute nothing directly.

Notice what is missing. The most important measurement, the actual mass of Greenland and Antarctica, is marked unavailable, because the data requires a login this site does not have. That gap is displayed rather than hidden, and the alarm that depends on it is shown as unarmed. A dashboard with no gaps is usually a dashboard that hides them.

What the monitor can see right now
loading

Words you will meet

NAVD88
The official height reference for North America. Every elevation on this site is measured against it, so numbers can be compared to each other.
MHHW (mean higher high water)
The average of the highest tide each day. Roughly "normal high tide". At Virginia Key it is 0.23 feet above the NAVD88 zero point.
King tide
The highest predictable tides of the year, when the sun and moon line up. Not a storm. This is when Miami floods on a clear day.
Storm surge
Water pushed ashore by a storm's wind and low pressure. Separate from sea level rise, but it starts from whatever the sea level already is, which is the point.
Ice shelf
The floating edge of an ice sheet, where it has flowed off the land and out over the sea. It does not raise sea level itself, but it acts like a doorstop holding back the ice behind it.
Buttressing
That doorstop effect. Remove the shelf and the grounded ice behind it flows faster into the ocean, and that ice does raise sea level.
Grounding line
The boundary where an ice sheet stops resting on rock and starts floating. When it retreats inland, more ice becomes vulnerable.
Circumpolar Deep Water
A relatively warm layer of ocean water circling Antarctica at depth. When it reaches in under the ice shelves it melts them from below, out of sight.
Subsidence
Land sinking. Around Miami it runs near 1 millimetre a year, which adds about a third of a foot by 2100 regardless of emissions.
Anomaly
The difference from normal, rather than the raw value. "Two degrees above average for this date" is an anomaly.
Sigma (σ)
How unusual something is, compared with how much it normally varies. Around 2σ is roughly a once-in-twenty-times event. Bigger is rarer.
Screening level
An honest label for work that is good enough to see where the problems are, and not detailed enough to design anything. This whole site is screening level.

Where to go next