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

ERS-2 achievements

ESA's Earth Explorer missions

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.

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

Global carbon budget

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

Twenty years of ERS missions

European Space Agency

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