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3. The high altitude platform and the APE-GAIA payload
The complete set of instrument which operated in the frame of the APE-GAIA campaign is listed in Table 1, along with some general information about the techniques and the products of the measurements. The location of the instruments onboard the M55 Geophysica aircraft is shown in Figure 1. The payload includes remote sensing and in-situ equipment for gaseous trace compounds, instruments aimed at characterising aerosols and cloud particles and devices for radiation measurements. From the point of view of the scientific objectives and of the measurement technique, the payload can be divided into remote sensing instruments for the measurement of the chemical composition of the atmosphere (remote sensing chemistry payload), in-situ instruments for the measurement of the chemical composition of the atmosphere (in-situ chemistry payload), and instruments for the study of the aerosols (microphysics payload)
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Figure 1 : Location of the APE-GAIA scientific instruments on board the Geophysica aircraft
The remote sensing chemistry instruments are the core of this payload as they provide simultaneous measurements of a large suite of chemical species. The two Fourier Transform Spectrometers MIPAS-STR and SAFIRE-A make limb and upward soundings to obtain column amounts above the aircraft and profiles below. Together they cover the main components of the Cly family (ClO, HCl and ClONO2), MIPAS-STR almost covers the entire the NOy family, whereas SAFIRE-A obtains information on Bry. GASCOD-A uses the DOAS technique and measures total amounts of the trace constituents at zenith and nadir in the case of high sun, and vertical profiles in the case of sunrise and sunset. Important active species observed by this instrument are OClO and BrO. The three instruments also observe several long-lived source gases. Their redundant measurements allow validation of the individual measurements and thus an improvement of the quality and reliability of the APE-GAIA data. In situ instruments provide measurements of ozone, water vapour and long-lived tracers at flight altitude with high spatial resolution. From these measurements vertical distributions can be observed during dives of the aircraft. The horizontal variability of the atmospheric composition and the dynamics of the mixing can be derived during flights at constant altitude ensuring an important synergy with the more extended vertical maps that the remote observations obtain on the basis of the assumption of horizontal homogeneity. Aerosols and PSC particles are detected and characterised by lidars and scatterometers pointing at different directions and operating with different ranges and different longitudinal resolutions. Correlation of PSC detection with the measurements of atmospheric composition simultaneously made by the "chemistry payload" provides an opportunity for the direct analysis of the effects of PSC formation (denitrification, dehydration, heterogeneous chemistry). Finally, two instruments provide measurements of radiation fluxes for a more precise quantification of photochemical parameters.
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Remote-sensing Chemistry and Radiation |
GASCOD-A Gas Absorption Spectrometer Correlating Optical Differences ? Airborne |
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Vertical profiles and column of O3, NO2, OClO, BrO. Actinic flux measurements |
ISAO-CNR Bologna, Italy |
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MIPAS-STR Michelson Interferometer for Passive Atmospheric Sounding ? STRatospheric |
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IMK-FZK Karlsruhe, Germany |
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SAFIRE-A Spectoscopy of the Atmosphere using Far-InfaRed Emission-Airborne |
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IROE-CNR Firenze, Italy |
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SORAD SOlar RADiation |
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CAO Moscow, Russia |
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ECOC ElectroChemical Ozone Cell |
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CAO Moscow, Russia |
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FOZAN Fast OZone Analyzer |
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CAO Moscow, Russia |
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FISH Fast In-situ Stratospheric Hygrometer |
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ICG-FZJ Juelich, Germany |
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FLASH FLuorescence Airborne Stratospheric Hygrometer |
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CAO Moscow, Russia |
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HAGAR High Altitude Gas AnalyzeR |
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N2O, SF6, CO2, CFC-12, CFC-11, Halon-1211 |
IMG, Univ. of Frankfurt Frankfurt, Germany |
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ABLE AirBorne Lidar Experiment |
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Particle density and optical properties from 2 to 15 km from the aircraft |
Univ. of Rome Rome, Italy |
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MAL-1 Microjoule Airborne Lidar |
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Particle density up to 10 km above the aircraft |
Observatory of Neuchatel Neuchatel, Switzerland |
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MAL-2 Microjoule Airborne Lidar |
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Particle density up to 10 km below the aircraft |
Observatory of Neuchatel Neuchatel, Switzerland |
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MAS Multiwavelength Aerosol Scatterometer |
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Particle density up to 2 km from the aircraft |
IFA-CNR Roma, Italy |
Table 1: The APE-GAIA scientific instruments
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