A 30-year satellite dataset published in February 2026 confirms: the rate of sea level rise is not just increasing — it is accelerating. From 3.1mm/year in the 1990s, to 4.62mm/year for 2013–2022.
Initial rate when satellites began continuous measurement in 1993 — primarily driven by thermal expansion of warming oceans.
49% faster than the 1990s rate. Now primarily driven by melting land ice — the most important shift in our understanding.
The February 2026 analysis overturns old assumptions: melting land ice (Greenland, mountain glaciers, and Antarctic ice) now accounts for the majority of sea level rise — surpassing thermal expansion.
This is especially alarming because melting land ice has far more permanent consequences — once melted, that water stays in the ocean.
Greenland is losing 200 billion tonnes of ice per year. The WMO confirms 2024 was the warmest year on record, coinciding with record ocean temperatures.
Note: Land ice (Greenland + glaciers + Antarctica) now accounts for 57% of sea level rise, surpassing thermal expansion at 43%.
The Thwaites Glacier is the size of Florida, containing enough ice to raise global sea levels by 65cm if it collapses entirely. Worse, it acts as a buttress holding back other glaciers — if Thwaites goes, it could trigger an additional 3 metres of rise.
February 2026 research: Thwaites is melting faster than previously modelled — even under low-warming scenarios.
UK and South Korean science teams are drilling 1km deep into the ice to directly measure melt rates at the base, where warm seawater contacts the glacier's underside — the primary melting mechanism.
Researchers have also proposed a 150-metre underwater wall to block warm water from reaching the glacier's base — a bold geoengineering idea now under serious consideration.
The February 2026 study published in ScienceDaily draws on data from NASA's ICESat-2 and ESA's GRACE satellites — 'space lasers' that measure ocean surfaces to millimetre accuracy from 500km altitude.
ICESat-2 fires 10,000 laser pulses per second at Earth's surface and measures the return time to nanosecond precision — enabling detection of 1mm changes across entire ocean basins.
GRACE tracks gravity changes — when Greenland ice melts, the gravitational field weakens, which the satellite detects. This is the most precise way to measure ice mass loss.
While the rest of the world faces rising seas, waters around Greenland will actually fall 1–4 metres by 2100 as the ice melts away.
Greenland's massive ice sheet pulls seawater toward it gravitationally. As it melts, this pull weakens — seawater near Greenland actually retreats outward.
As heavy ice melts, the land beneath springs back up — a process called 'isostatic rebound'. Greenland is rising, causing local coastlines to relatively lower.
The meltwater from Greenland flows southward — amplifying sea level rise in Miami, New York, Western Europe, and Southeast Asia beyond the global average.
"Although Greenland is losing 200 billion tonnes of ice annually, sea levels around Greenland itself will actually fall 1–4 metres by 2100, while Southeast Asian and Atlantic coastlines may rise well above the global mean."
From Jakarta to Ho Chi Minh City to Miami — major coastal cities worldwide face existential risks from sea level rise. Learn more about ocean governance in our article on the High Seas Treaty.
Parts of North Jakarta already below sea level; city moving capital to Nusantara
Built on porous limestone — sea water seeps up from below. $4B flood infrastructure investment underway
Mekong Delta at grave risk; land subsidence compounds sea level rise. 10M residents at risk
Low-lying coastal megacity of 20M. Dharavi and other areas face permanent inundation
60% of country below sea level, but world-class delta works protect 17M people — a global model
The difference between limiting warming to 1.5°C versus 2°C by 2100 is not a small number — it determines the fate of hundreds of millions of coastal people.
Further reading on climate's physical impacts on Earth: How Climate Change Is Slowing Earth's Rotation
Rotterdam's Maeslantkering, Thames Barrier — proven technology protecting millions. Cost: $1–10B per city.
Mangroves absorb wave energy 70% better than concrete seawalls. Vietnam replanting 50,000 ha of Mekong delta mangroves.
Relocating communities away from highest-risk zones before disaster strikes. New Zealand leading with coastal policy framework.
Amsterdam testing floating neighborhoods. Maldives building 5,000-unit floating city by 2027 as climate adaptation.
Scientists propose 150-metre underwater wall to block warm water from melting Thwaites glacier from below.
Staying below 1.5°C limits sea level rise to ~0.3m by 2100. Every 0.5°C avoided saves coastal cities billions.
Nations committed under the 2015 Paris Agreement to limit warming to 1.5–2°C. But current pledges put the world on a 2.5–3°C trajectory — meaning 0.6–1.2 metres of sea level rise by 2100.
Protects 30% of oceans by 2030 — helps marine ecosystems adapt to sea level rise
Solar and wind growing exponentially — but must triple pace to meet 1.5°C targets
WMO deploying universal early warning systems for all people by 2027, including coastal flooding
UK–Korea–US cooperating on Thwaites research; EU funding GRACE-FO satellite monitoring to 2030
▸ Sea levels rising at 4.62mm/year means low-lying areas could lose thousands of hectares of farmland within the next 30 years.
▸ If you live in a coastal city, a 0.5m sea level rise by 2050 could directly impact property values within 20km of the shoreline.
Related: Arctic sea ice collapse and Arctic ice maximum record low 2026.
Sea Level Rise 2026 — NASA · ESA · WMO · Columbia Climate School
Related Topics
Stay on top of trends
Bookmark this page and check back often for the latest updates and insights.