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Beyond carbon storage

Carbon-rich biomass

Earth's green lungs

Global carbon cycle

ESA's Earth Explorer missions

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

European emerging Copernicus Contributing Missions

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.

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

Sea-level rise is not the same everywhere

Sea-level rise and us

Six key facts about Copernicus Sentinel-6

Causes of sea-level rise

Measuring sea-level change

Global glacier mass loss 1961–2016

Causes of sea-level rise

Sea-level rise and us

Satellite altimeters

Sea-level rise is not uniform

Sentinel-5P infographic

EarthCARE data products

Twenty years of ERS missions

European Space Agency

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