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ERS-2 reentry – how and why is it happening?

ESA's Earth Explorer missions

Copernicus Sentinel Expansion Missions

Possible future temperature rise

The Arctic is experiencing disproportionately higher temperature increases compared to the rest of the planet, triggering a series of cascading effects known as Arctic amplification.

Satellite altimeters

Six key facts about Copernicus Sentinel-6

Global carbon cycle

Global glacier mass loss 1961–2016

HydroGNSS reflectometry

Weather versus climate at a glance

Causes of sea-level rise

Sea-level rise is not the same everywhere

Key stages in Aeolus’ reentry

Measuring sea-level change

Supporting the Paris Agreement from Space

Causes of sea-level rise

Aeolus-2 Value of Information

Aerosols and climate

Sentinel-5P infographic

Mapping extreme waves

Carbon-rich biomass

Sentinel-1B reentry phases

Clouds in the climate system

Beyond carbon storage

Earth's green lungs

Get to know Europe's meteorological missions

Measuring sea-level change

Earth radiation budget

Taking gravity measurements into the future

EarthCARE key facts

The Flexible Combined Imager on MTG-I

Aeolus Value of Information

Sea-level rise and us

Sentinel-5: tangible benefits for society

State-of-the-art European technologies

Sea-level rise and us

Sea-level rise is not uniform

European emerging Copernicus Contributing Missions

EarthCARE facts and figures

More than just weather

Next generation weather forecasting

The benefits of the MetOp Second Generation mission

Informing landfill sites from space

Causes of sea-level rise

Sentinel-5 data applications

Watching the weather

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