Balloons on a Climate Mission: Searching for Clues in the Stratosphere

5 June 2025

The launch of the weather balloon on 27 May was the first of many this year – marking the start of a unique measurement campaign which will continue until October, with weekly launches. Its aims include investigating the influence of the Asian summer monsoon on the stratosphere over Europe across an entire season.

During the balloon campaign, several miniature sensor packages will rise to an altitude of over 30 kilometers, directly recording the vertical distribution of various trace gases, aerosols, and cloud particles. These precise measurements will also help verify measurements from satellite instruments and check the results of climate models.

The balloons carry a range of different measuring instruments. Some transmit their data directly to the climate researchers' ground station. Others take air samples in the troposphere, which are then examined later in the laboratories of the Institute of Climate and Energy Systems (ICE-4). "As a result of the decreasing air pressure, the balloon expands more and more at higher altitudes until it finally bursts. The devices are tracked and can then be recovered after they land," explains atmospheric researcher Christian Rolf, who is coordinating the campaign.

Long-term effects on the climate

The balloon campaign follows on from the PHILEAS aircraft campaign in 2023. This campaign also focused on the climate impact of the Asian monsoon. In this large-scale weather system, thunderstorms accumulate and transport heavily polluted air from the lower atmosphere in Southeast Asia up to an altitude of 15 kilometers. From there, the polluted air spreads westward to the eastern Mediterranean and eastward across the Pacific Ocean.

The monsoon has no direct influence on the weather in Europe. It is the long-term effects on the climate that are at stake here. “The Asian monsoon region is characterized by strong vertical transport,” explains Christian Rolf. "Air masses near the ground, containing all the local emissions, are thus quickly transported vertically to the tropopause. From there, the air masses slowly spread across the entire northern lower stratosphere, so that we can also measure the influence and air from the Asian monsoon here."

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Contact

  • Institute of Climate and Energy Systems (ICE)
  • Stratosphere (ICE-4)
Building 05.2 /
Room 1059d
+49 2461/61-6524
E-Mail

Dr. Christian Rolf

wissenschaftlicher Mitarbeiter

  • Institute of Climate and Energy Systems (ICE)
  • Stratosphere (ICE-4)
Building 05.2 /
Room 1056
+49 2461/61-6933
E-Mail

Dr. Regine Panknin

Pressereferentin

    Building 15.3 /
    Room R 3028
    +49 2461/61-9054
    E-Mail

    Last Modified: 11.06.2025