geomon
Global Earth Observation and Monitoring
of the Atmosphere

 

CARIBIC - The flying observing system

CARIBIC Airbus

A Lufthansa passenger aircraft carries the CARIBIC container to various destinations
to perform monthly measurements on long-distance flights.

The project CARIBIC (Civil Aircraft for the Regular Investigation of the Atmosphere Based on an Instrument Container) deploys a measurement container onboard a Lufthansa passenger aircraft (Airbus A340-600), see a picture of the inlet. The container accommodates 15 fully automated instruments for measurements of aerosols and various trace gases. In addition to in-situ measurements, whole air samples are collected in glass flasks during the CARIBIC flights at roughly one hour intervals with sampling times between 30 and 120 seconds. The samples are analysed for greenhouse gases as well as for organic compounds and isotopes by a number of European laboratories.

The container became operational in December 2004, with flights conducted almost monthly out of Frankfurt, Germany, to various destinations in South America, Asia, and North America (see map below). At cruising altitudes between 9 and 13 km the aircraft frequently crosses the tropopause, in the extra-tropics about 40% of the flight time is spent in the transition layer above the tropopause (ex-TTL).

caribic routes

Map of the CARIBIC flight tracks 2004-2008 and comparison of CO2 flask data from flights to Asia with data from ground stations.

The panel below shows CO2 from flask analysis of CARIBIC whole air samples taken on flights to Asia from 2005 to 2008 in comparison with measurements from ground stations situated close to the aircraft flight tracks (see map).

CARIBIC_ground_station_CO2 comparison
CO2 from flask analysis of CARIBIC whole air samples taken on flights to Asia from 2005 to 2008 in comparison with measurements from ground stations situated close to the aircraft flight tracks (see map).The stations are operated by NOAA (WLQ,KZM,KZD) and the CarboEurope network (HLE).

The annual cycle of CO2 with the summer minimum due to by the carbon fixation by the vegetation is clearly visible in all curves. The CARIBIC data show very good agreement with the ground-based observations. The comparison shows the expected damping of the seasonal cycle's amplitude with increasing altitude of the location. In winter, when the CO2 mixing ratio reaches its maximum, the CARIBIC tropospheric data matches the CO2 level of the highest of the selected stations, Hanle in northern India (HLE). In summer, the minimum mixing ratios are lower at the mountain station than the CARIBIC data. This reflects the influence of the local vegetation.

More information on GEOmon activities related to CARIBIC:

  • Results from WP1.2 (Greenhouse gas data from CARIBIC)
  • Results from WP 2.2 (Reactive gases from CARIBIC)

See the News Archive for previous news from the GEOmon project.

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