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European emerging Copernicus Contributing Missions

Informing landfill sites from space

Taking gravity measurements into the future

Next Generation Gravity Mission measuring concept

Sea-level rise is not the same everywhere

Sea level and us

Causes of sea-level rise

Measuring sea-level change

Impacts of the IRIDE programme

IRIDE data flow

IRIDE ground station network

HydroGNSS reflectometry

Mapping extreme waves

The IRIDE system

ESA's Earth Explorer missions

Sentinel-5: tangible benefits for society

MetOp-SG and MTG: taking weather forecasting into the future

Sentinel-5 data applications

The benefits of the MetOp Second Generation mission

The invisible risks to public health

Beyond carbon storage

Carbon-rich biomass

Earth's green lungs

Global carbon cycle

Sentinel-1B reentry phases

EarthCARE facts and figures

Aerosols and climate

Clouds in the climate system

EarthCARE key facts

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

ERS-2 achievements

Earth radiation budget

Key stages in Aeolus’ reentry

Copernicus at 25: the growing community of Sentinel data users

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.

The Flexible Combined Imager on MTG-I

Aeolus-2 Value of Information

Aeolus Value of Information

More than just weather

Watching the weather

State-of-the-art European technologies

Next generation weather forecasting

Supporting the Paris Agreement from Space

Copernicus Sentinel Expansion Missions

Possible future temperature rise

Weather versus climate at a glance

Get to know Europe's meteorological missions

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