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Establishing Regular Measurements of Halocarbons at Taunus Observatory Tanja Schuck, Fides Lefrancois, Franziska Gallmann, and Andreas Engel Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences Taunus Observatory


  1. Establishing Regular Measurements of Halocarbons at Taunus Observatory Tanja Schuck, Fides Lefrancois, Franziska Gallmann, and Andreas Engel Goethe University Frankfurt, Institute for Atmospheric and Environmental Sciences

  2. Taunus Observatory • Regular halocarbon measurements in Europe are made predominantly at clean air stations (NOAA and AGAGE network) • Data from a semi-polluted site in central Europe will result in stronger constraints for emission estimates NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 2

  3. Taunus Observatory • Taunus Observatory is located at Kleiner Feldberg at 50.22 ° N, 8.44 ° W at 825m altitude. • The site is influenced by emissions from the densely populated Rhein-Main region. • Long-range transport is mainly from westerly directions, including marine background air from the North Sea. • Regular measurements of halocarbons started October 2013. courtesy Dominik Brunner NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 3

  4. Current Status • Samples collected weekly in stainless steel canisters • Analysis by GC-MS (Agilent 7980A) using a quadrupole MS (Agilent 5975C) and a TOF-MS (ALMSCO/BenchTOF) in parallel • Sample drying with Mg(ClO 4 ) 2 Cryo-trapping at -80 ° C (Stirling cooler), desorption at ≈ 200 ° C • • Data quality assessment by taking double samples and having two analyses of each individual canisters TOF-MS preconcentration unit calibration gas ASCEND gas chromatograph sample and stream selection Quadrupole-MS Hoker et al., Atmos. Meas. Tech. 2015 NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 4

  5. Sample Collection at Mace Head - Comparison with NOAA HATS data chloromethane r=0.98 methylchloroform r=0.98 HCFC-141b r=0.66 27 4.0 600 26 IAU [ppt] IAU [ppt] IAU [ppt] 560 3.5 520 25 3.0 480 24 480 520 560 600 3.0 3.5 4.0 24 25 26 27 NOAA [ppt] NOAA [ppt] NOAA [ppt] HCFC-142b r=0.84 HFC-134a r=0.60 (0.99) CFC-11 r=0.48 105 25 240 100 24 238 IAU [ppt] 95 IAU [ppt] IAU [ppt] 236 90 23 85 234 22 80 232 75 21 75 80 85 90 95 100 105 21 22 23 24 25 232 234 236 238 240 NOAA [ppt] NOAA [ppt] NOAA [ppt] • sample collection at Mace Head twice per month (when wind is from clean air sector) • comparison with NOAA data set @ Mace Head (sample collection for us and NOAA is under background conditions within less than half an hour) • our calibration is on AGAGE scales, scale conversion necessary for most substances NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 5

  6. Time Series 550 10 Taunus Observatory Taunus Observatory Mace Head Mace Head 8 CH3CCl3 [pptV] AGAGE Global Mean AGAGE Global Mean CFC-12 [pptV] 6 525 4 2 500 0 2011 2012 2013 2014 2015 2016 2017 2011 2012 2013 2014 2015 2016 2017 30 60 Taunus Observatory Taunus Observatory 50 Mace Head Mace Head 28 HCFC-141b [ppt] HFC_143a [ppt] AGAGE @ Mace Head AGAGE @ Mace Head 40 26 30 24 20 22 10 20 0 2011 2012 2013 2014 2015 2016 2017 2011 2012 2013 2014 2015 2016 2017 200 Taunus Observatory 175 dichloromethane [ppt] • mixing ratios at Mace Head nicely represent background Mace Head 150 • good agreement with AGAGE data at Mace Head 125 100 • higher variability at Taunus Observatory with many 75 polluted samples (includes data from all wind sectors, 50 whereas Mace Head is from clean air sector only) 25 0 NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 2013 2014 2015 2016 2017 6

  7. Seasonal Cycles 200 Taunus Observatory 175 dichloromethane [ppt] Mace Head 150 125 100 75 50 25 0 2013 2014 2015 2016 2017 30 Taunus Observatory Mace Head 28 HCFC-141b [ppt] AGAGE @ Mace Head 26 24 22 20 2011 2012 2013 2014 2015 2016 2017 NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 7

  8. Trajectory Analysis • Back trajectory calculations were performed for every single sample using • HYSPLIT4 • 120 hours backward • 1 ° x 1 ° GDAS1 dataset NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 8

  9. Trajectory Analysis: CFC-11 270 Taunus Observatory Mace Head 260 AGAGE Global Mean • use of CFC-11 is regulated CFC-11 [pptV] 250 • atmospheric mixing ratios decrease • variability at Taunus Observatory is low 240 with few outliers 230 220 2010 2011 2012 2013 2014 2015 2016 2017 • HYSPLIT trajectories (120 hours backward) for samples collected in 2015 • color coded by CFC-11 mixing ratio • elevated mixing ratios correlate with air mass origin from southwest NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 9

  10. Trajectory Analysis HCFC-142b 35 • used as replacement for CFCs Taunus Observatory Mace Head • use is regulated AGAGE@ Mace Head 30 HCFC-142b • mixing ratios have stabilized and are expected to decrease in the future • over our observation period atmospheric 25 mixing ratios have no significant trend • variability at Taunus Observatory is high 20 2011 2012 2013 2014 2015 2016 2017 compared to Mace Head clean air samples • HYSPLIT trajectories for samples collected in 2015 • color coded by HCFC-42b mixing ratio • elevated mixing ratios correlate with air mass origin from southwest NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 10

  11. Trajectory Analysis • HYSPLIT trajectories (120h backward) for each individual sample are grouped by the direction from with they approach Taunus Observatory (> 50% of time spent in respective sector) • four main sectors were identified: northwest (slow and fast trajectories) west (slow and fast trajectories) southwest (slow trajectories) east (slow trajectories) NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 11

  12. Trajectory Analysis • For most substances investigated highest mixing ratios are measured in air masses arriving from the southwest sector. • Background conditions are experienced when air mass transport towards the site is from the northwest. NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 12

  13. Future Development: in-situ GC-TOF-MS • In summer 2017, an in-situ GC-MS system will be installed. • Measurements will be every 2h (following AGAGE protocol) • The mass spectrometer to be deployed is a medium resolution time-of-flight mass spectrometer • Large substance range: 90+ known species in the chromatogram • High measurement precision: 0.2-1.5% typical (multiple species) 0.15% at best (CFC-12) • Linear detector tested up to 5 ppb (25 ng) CFC-12 (~4 orders of magnitude) • Open data format • Complete mass scan will allow retrospective analysis (digital air archive) Obersteiner et al., Atmos. Meas. Tech. 2016 NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 13

  14. Summary • We started regular collection of air samples at Taunus Observatory in 2013 • Our measurement are linked to global networks through flask sampling at Mace Head (Ireland) • Mace Head represents baseline for Taunus Observatory • Trajectory analysis shows a distinct polluted / clean air sector • Data from a medium-polluted site have the potential to better constrain European emission estimates • Data from Taunus Observatory will be used for inversion modelling • In summer 2017, an in-situ GC-TOF-MS system will be installed – rapid growth of the dataset • Measurements will be every 2h (following AGAGE protocol) – now we have one data point per week • Complete mass scan of the TOF-MS will allow retrospective analysis (digital air archive) NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 14

  15. Thank you for your attention!

  16. Instrumentation: Stream Selection Unit • sample selection with multiposition Valve (Valco) • stream selection (sample, blank, calibration gas) with pressure operated on/off valves (Valco) • drying tube Mg(ClO 4 ) 2 • 2 x 2l reference volume for sample volume determination • mass flow controller for sample flow regulation (Bronkhorst) NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 16

  17. Instrumentation: Preconcentration Unit • sample enrichment is done on a sample loop filled with HayeSep D • sample loop is embedded into a cooled aluminium block • cooling works cryogen-free, based on a Stirling Cooler • trapping at -80 ° C (flow 150 ml/min) • desorption at ca. +200 ° C NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 17

  18. Instrumentation: Gas Chromatography • column: 30m GasPro PLOT column (7.5m pre-column, 22.5m main column), inner diameter 0.32mm • total duration: 17.95 min, backflush after 12.6 min • oven temperature 50 – 200 ° C • carrier gas: purified Helium 6.0 NOAA ESRL Global Monitoring Annual Conference 23/24 May 2017 18

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