Abstract

Abstract. Understanding the role of climate-sensitive trace gas variabilities in the upper troposphere and lower stratosphere region (UTLS) and their impact on its radiative budget requires accurate measurements. The composition of the UTLS is governed by transport and chemistry of stratospheric and tropospheric constituents, such as chlorine, nitrogen oxide and sulfur compounds. The Atmospheric chemical Ionization Mass Spectrometer AIMS has been developed to accurately measure a set of these constituents on aircraft by means of chemical ionization. Here we present a setup using SF5− reagent ions for the simultaneous measurement of trace gas concentrations of HCl, HNO3 and SO2 in the pptv to ppmv (10−12 to 10−6 mol mol−1) range with in-flight and online calibration called AIMS-TG (Atmospheric chemical Ionization Mass Spectrometer for measurements of trace gases). Part 1 of this paper (Kaufmann et al., 2016) reports on the UTLS water vapor measurements with the AIMS-H2O configuration. The instrument can be flexibly switched between two configurations depending on the scientific objective of the mission. For AIMS-TG, a custom-made gas discharge ion source has been developed for generation of reagent ions that selectively react with HCl, HNO3, SO2 and HONO. HNO3 and HCl are routinely calibrated in-flight using permeation devices; SO2 is continuously calibrated during flight adding an isotopically labeled 34SO2 standard. In addition, we report on trace gas measurements of HONO, which is sensitive to the reaction with SF5−. The detection limit for the various trace gases is in the low 10 pptv range at a 1 s time resolution with an overall uncertainty of the measurement of the order of 20 %. AIMS has been integrated and successfully operated on the DLR research aircraft Falcon and HALO (High Altitude LOng range research aircraft). As an example, measurements conducted during the TACTS/ESMVal (Transport and Composition of the LMS/UT and Earth System Model Validation) mission with HALO in 2012 are presented, focusing on a classification of tropospheric and stratospheric influences in the UTLS region. The combination of AIMS measurements with other measurement techniques yields a comprehensive picture of the sulfur, chlorine and reactive nitrogen oxide budget in the UTLS. The different trace gases measured with AIMS exhibit the potential to gain a better understanding of the trace gas origin and variability at and near the tropopause.

Highlights

  • Trace gas measurements at low concentrations with high spatial resolution are challenging

  • The multitude of trace gases simultaneously detected by AIMS enables the identification of the origin of the air mass, differentiating whether it has a more tropospheric character with e.g., enhanced SO2 or more stratospheric character tagged by the stratospheric tracer HCl

  • The instrument has proven its reliability during several airborne campaigns on the research aircraft Falcon and HALO (Voigt et al, 2014; Jurkat et al, 2014)

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Summary

Introduction

Trace gas measurements at low concentrations with high spatial resolution are challenging. In the extratropical upper troposphere and lower stratosphere, a sensitive region concerning the Earth’s radiation budget due to its low temperatures and strong trace gas gradients, accurate measurements are needed (Hegglin et al, 2010). Photochemical processing, convection and downward transport change ozone and nitric acid concentrations in the upper troposphere, thereby affecting the radiative budget of the free troposphere and upper troposphere and lower stratosphere region (UTLS) (Lacis et al, 1990). During the CONCERT2008 campaign (CONtrail and Cirrus ExpeRimenT) (Voigt et al, 2010), the detection mechanism using SF−5 reagent ions was extended to fast and precise measurements of HONO and SO2 in young aircraft exhaust plumes, in order to derive the conversion efficiency from fuel sulfur to sulfuric acid (Jurkat et al, 2011). We present the chemical ionization and calibration methods, inlet specifications and sensitivity studies for the trace gas configuration, focusing on HCl, HNO3, HONO and SO2

The setup of the mass spectrometer
Inlet line
Pressure regulation
Custom-made discharge ion source
Ion molecule reactions
Mass spectrum
Calibration of AIMS-TG
In-flight calibration of HNO3 and HCl
Isotopically labeled SO2
Isotopic labeling of HCl and HNO3
Laboratory calibration of HONO
Retrieval of trace gas concentrations for AIMS-TG
Data quality and sources of uncertainty
Sensitivity and detection limits
Further instrumental uncertainties
Cross-sensitivity
Findings
Conclusion and outlook
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