• A rainbow-forming shower cloud during descent for Punta Arenas airport

    A rainbow-forming shower cloud during descent for Punta Arenas airport

  • Radiation measurements on the roof top of UMAG

    Radiation measurements on the roof top of UMAG

  • LACROS site at UMAG in Punta Arenas

    LACROS site at UMAG in Punta Arenas

  • 23 November 2018: Delivery of the LACROS containers to UMAG

    23 November 2018: Delivery of the LACROS containers to UMAG

  • An altocumulus cloud field approaching Punta Arenas

    An altocumulus cloud field approaching Punta Arenas

  • An altocumulus cloud field over Punta Arenas

    An altocumulus cloud field over Punta Arenas

  • Moon hiding behind cirrus clouds over Punta Arenas

    Moon hiding behind cirrus clouds over Punta Arenas

  • Cumulus humilis of Patagonia

    Cumulus humilis of Patagonia

  • Illuminated cirrus clouds during sunset over Punta Arenas

    Illuminated cirrus clouds during sunset over Punta Arenas

  • Altostratus during sunset over Punta Arenas

    Altostratus during sunset over Punta Arenas

  • Rainbow over Punta Arenas after passage of a cumulus congestus

    Rainbow over Punta Arenas after passage of a cumulus congestus

  • Steady westerly winds bend trees in southern Patagonia

    Steady westerly winds bend trees in southern Patagonia

  • Wave clouds forming over the strait of Magellan

    Wave clouds forming over the strait of Magellan

  • LACROS field site during nighttime at Limassol

    LACROS field site during nighttime at Limassol

  • LACROS site of Limassol in front of the Limassol water tower

    LACROS site of Limassol in front of the Limassol water tower

DACAPO in brief

Clouds and aerosols are inseparably coupled, linked via complex pathways of interaction whose outcome manifests in the macroscopic properties of precipitation and radiation fields. The project DACAPO (Dynamics, Aerosol, Cloud And Precipitation Observations) aims on disentangling the different processes involved in the formation of clouds, precipitation and their radiative impact. The approach to achieve this goal is threefold:

  • Conducting field experiments in key regions of aerosol pollution, ranging from clean near-pristine, over moderately polluted to highly polluted places.
  • Development of novel observational techniques and methods for data analysis. Key for understanding the role of aerosol particles in cloud and precipitation formation is to characterize number, size and mass of the particles involved in the processes. It is still a long way to go to make this feasible with remote sensing techniques.
  • Evaluate regional contrasts of aerosol, cloud, dynamics and precipitation properties on a statistical basis. This requires the availability of long-term, quality controlled data sets