• LACROS at nighttime

    The LACROS site at nighttime

  • Sc nearby Invercargill

    A stratocumulus cloud field nearby Invercargill

  • The coastline 8 km west of the LACROS site

    The coastline 8 km west of the LACROS site

  • Double rainbow

    A double rainbow appears above Invercargill post the passage of an evening shower.

  • LACROS station

    The LACROS site

  • Southern Alps

    The Southern Alps of New Zealand appear to be very close to Invercargill

  • St. Marys Basilica

    St. Mary's Basilica of Invercargill in late winter

  • LACROS during nighttime

    The LACROS station at nighttime

  • Fuzzy cirrus clouds in the sky above Invercargill

    Fuzzy cirrus clouds in the sky above Invercargill

  • The lidar beam of LACROS leaving the emission window

    The laser beam of LACROS' PollyXT Lidar leaving the emission window

goSouth-2 in brief

The southern tip of New Zealand at the northern edge of the Southern Ocean is a unique place to study the relationships between aerosols and clouds. The atmosphere in this region can be very clean when air masses approach from Antarctica. But the atmosphere there can also be burden with continental-sourced aerosols when air masses approach via Australia. We want to make use of these strong contrasts to learn more about how the properties of clouds respond to perturbations in the aerosol load. The related activities are running in the framework of the project goSouth-2, which is guided by the following main objectives:

  • Observations: Deploy an extensive set of remote-sensing and in-situ instrumentation for a period covering at least a full annual cycle to capture aerosols, clouds, precipitation as well as the involved atmospheric dynamics and the resulting effects on the budget of solar and terrestrial radiation of the atmosphere. 
  • Method developments: 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.
  • Statistics: Evaluate regional and temporal contrasts of aerosol, cloud, dynamics and precipitation properties on a statistical basis. This requires the availability of long-term, quality controlled data sets.
  • Collaboration: Liaise with further atmospheric research projects currently ongoing in and around New Zealand.