Air and aerosol sampling facilities

RRS Sir David Attenborough has air and aerosol sampling facilities that draw air from two locations – the foremast platform, above the vessel’s bow, and from above the crow’s nest. These locations ensure clean, ambient air samples that are uncontaminated by ship emissions.

The aerosol sampling system uses 50mm-diameter stainless steel tubing with minimal bends. This feeds into the main atmospheric science lab, below the foredeck. The aerosol lab is located at the very top deck to minimise the distance between the sampling location and the laboratory.

Scientific meteorological equipment will be mounted on both the foremast and above the bridge. Measuring in two locations ensures there is back-up for these critical measurements. The meteorological instruments are connected to the atmospheric science laboratory space.

RRS Sir David Attenborough also has the following meteorological and atmospheric instrumentation:

  • An extensive suite of meteorological sensors to measure surface air pressure, wind speed and direction, air temperature and humidity, visibility, and precipitation (including the presence of freezing rain or icing conditions).
  • Dew point chilled mirrored hygrometer to provide an accurate measure of humidity.
  • Trace gas measurements will be made of carbon monoxide, carbon dioxide, methane and ozone. Measurements of carbon dioxide dissolved in sea water are also made.
  • Solar/Infra-red radiometers provide downwelling radiative fluxes.
  • Sea surface temperature is measured by a Heimann KT15 infra-red temperature sensor, while bulk water temperature is measured at the pumped sea water inlet.

The polar oceanic regions are remote and inhospitable resulting in sparse data coverage, particularly in the Southern Ocean. This lack of data makes it difficult to address some of the key atmospheric science questions. RRS Sir David Attenborough enables scientists to access this remote region and tackle some of these globally relevant challenges.

For example, we don’t yet adequately understand the main sources of small particles in the atmosphere, known as aerosols. The sources of these aerosols are likely to be different in different regions (e.g. the open ocean, sea ice zone, biologically-active coastal waters) and at different times of the year. It’s important to understand where aerosols come from because these small particles influence how clouds form, and the cloud’s characteristics. For example, whether a cloud has a large number of small droplets or a small number of large droplets affects the way the cloud interacts with solar radiation, affecting the surface energy budget and near-surface atmospheric temperatures.

Long-term measurements of greenhouse gases are essential for assessing their influence on global temperatures and understanding how the atmosphere is evolving. For example, the Southern Ocean is a key sink for carbon dioxide – it is estimated that it has absorbed up to 50% of the human-related emissions that have entered the oceans. However, there is evidence that the Southern Ocean’s ability to remove carbon dioxide from the atmosphere is reducing. On-going measurements are therefore needed to capture this change and to understand the implications for future climate-projections which influence international climate policy.

Changes in the atmosphere’s composition are driven also by growth in urban centres, changes in agricultural practice, and burning of biomass. Signals of these activities can be detected as continental air masses flow out over the oceans. In the Arctic, changes in shipping – enabled by retreat of sea ice – is likely to influence the composition of the regional atmosphere. The instruments on board RRS Sir David Attenborough will provide fundamental observations to underpin studies of changing air quality due to anthropogenic changes.