AAOE_TraceGas_AircraftInSitu_ER2_Data is the in-situ trace gas data collected onboard the ER-2 aircraft during the Airborne Antarctic Ozone Experiment (AAOE) suborbital campaign. Data was collected by instruments such as the Whole Air Sampler (WAS), Multiple Axis Resonance Fluorescence Chemical Conversion Detector for ClO and BrO (ClO/BrO), NOAA NOy Instrument (NOAA NOy), Multi-Filter Sampler (MFS), Airborne Tunable Laser Absorption Spectrometer (ATLAS), Dual-Beam UV-Absorption Ozone Photometer (NOAA O3 Classic), and the Ultraviolet Ozone Photometer (UOP). Data collection for this product is complete.
The AAOE suborbital campaign was an international and multi-organizational campaign with NASA, NOAA, NSF, and Chemical Manufacturer’s Association (CMA). It also involved the UK Meteorological Office and the European Center for Medium-range Weather Forecasts (ECMWF). UKMO provided weather forecasters with Falkland Island experience to make predictions for the wind-sensitive ER-2 from Punta Arenas. The main goal of AAOE was to perform a complex study of polar stratospheric clouds and their relation to the late winter and spring ozone loss over the Antarctic (the ozone hole). In order to collect the proper data to complete its objective, AAOE utilized specially instrumented NASA ER-2 and DC-8 aircrafts. The instruments on these aircrafts were used to acquire data on chemical, meteorological, and cloud-physical parameters associated with this ozone loss phenomenon that was observed when this campaign was conducted. Along with the aircrafts, three separate satellite systems, ozone sondes, and ground-based sensors were employed in various locations in Antarctica to collect data.
The AAOE mission was conducted from August to October 1987 with flights based in Punta Arenas, Chile. The DC-8 aircraft was equipped with 9 instruments for this campaign. A few of those instruments were the JPL Mark IV Balloon Interferometer (MkIV), the Differential Absorption Lidar (DIAL), the Whole Air Sampler (WAS (NCAR)), the in-situ ozone sampler from NASA Langley, and the NOAA Lyman-Alpha Total Water Hygrometer (NOAA TW). The MkIV was responsible for taking various data points, including temperature and pressure. Along with these, the MkIV took measurements on the vertical column of a multitude of compounds including CO, H2O, NO, NO2, CH4, CO2, O3, and N2O in units of molecules/cm2. The DIAL collected measurements of ozone mixing ratio in parts per billion by volume (ppbv), IR aerosol backscatter, IR atmospheric scattering ratio, visible (VIS) aerosol backscatter, and VIS atmospheric scattering ratio. The WAS (NCAR) was used to take measurements on whole air mixing ratio, which includes CH4, CO, and N2O in different concentrations. Finally, The NOAA TW onboard the DC-8 aircraft collected data sets on H2O mixing ratios in the atmosphere. The ER-2 aircraft was equipped with 16 instruments, including the Multiple Axis Resonance Fluorescence Chemical Conversion Detector for ClO and BrO (ClO/BrO), the NOAA NOy Instrument (NOAA NOy), and the Airborne Tunable Laser Absorption Spectrometer (ATLAS). As its name suggests, the ClO/BrO was used to collect data on ClO and BrO mixing ratios. The NOAA NOy collected measurements of NOy mixing ratio, while the ATLAS took measurements on N2O mixing ratio. Finally, balloon sondes were deployed with the responsibility of gathering data on atmospheric temperature, pressure, wind speed, wind direction, as well as ozone column data in various concentrations. The Journal of Geophysical Research: Atmospheres, Volume 94, Issue D14 and Issue D9 have more information on the AAOE campaign.