wei wang , jacques hueber , abigale j. curtis , cédric couret

1
Halogenated Trace Gases and Volatile Organic Compounds at the Global Atmosphere Watch Global Observatory Schneefernerhaus/Zugspitze, Germany Introduction: Halocarbons and hydrocarbons (C2 - C8) are being monitored at the German GAW Global Station Zugspitze/Hohenpeissenberg, 2670 m a.s.l., Germany. At the Zugspitze summit, atmospheric monitoring has been performed since the late 1970’s. In 1998, measurements for the United Nation’s Global Atmosphere Watch program (GAW) moved to the environmental research station Schneefernerhaus, ~300 m below the summit, where they support the study of greenhouse gases, reactive gases and aerosols. In 2013, an automated, remotely controlled gas chromatography/mass spectrometry (GC/MS) analytical system was installed for the monitoring of chlorofluorocarbon and other halocarbon trace gases. Monitoring of volatile organic compounds (VOC) was added in 2015. Ozone depleting and climate-change related organic traces have been monitored for more than a decade at a network of ground-based stations within the Advanced Global Atmospheric Gases Experiment (AGAGE) program following the Montreal and Kyoto protocols, which primarily rely on MEDUSA GC/MS measurement systems. The GC/MS at Zugspitze is a much simplified instrument, providing a lower maintenance and lower cost option for the long-term monitoring of these species. 1 Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. 2 German Environment Agency, Global Atmosphere Watch Observatory Zugspitze/Hohenpeissenberg, Platform Zugspitze at Environment Research Station Schneefernerhaus, Germany Wei Wang 1 , Jacques Hueber 1 , Abigale J. Curtis 1 , Cédric Couret 2 , Ludwig Ries 2 , Detlev Helmig 1 CFC-11 CFC-113 CFC-114 CFC-115 CFC-12 CFC-13 H-1211 H-1301 H-2402 HCFC-22 HCFC-124 HCFC-141b HCFC-142b HFC-125 HFC-134a HFC-143a HFC-152a HFC-245fa HFC-365mfc methyl chloride CH2Cl2 chloroform CCl4 methyl chloroform perchloroethylene methyl bromide CH2Br2 CHBr3 methyl iodide PFC-116 PFC-218 PFC-318 SF6 SO2F2 COS ethene ethane propene propane i-butane iso-butene 1,3-butadiene 1-butene trans-2-butene n-butane cis-2-butene i-pentane 1-pentene isoprene trans-2-pentene cis-2-pentene n-pentane 2-methylpentane 3-methylpentane hexane benzene cyclohexane n-heptane toluene iso-octane octane ethylbenzene m-xylene o-xylene 1,2,4-trimethylbenzene 1,3,5-trimethylbenzene methanol ethanol acetaldehyde methyl formate actone List of compounds monitored at Zugspitze. Those with standards available for quantification are indicated in bold. The compounds in italic are very often below the detection limit. Brief description of the operation: The instrument contains two main components, a custom-built pre-concentration inlet system and an Agilent GC/MS. The inlet system is controlled by a Labview program that also acquires and stores the metadata. It is synchronized with the GC/MS system where Agilent ChemStation software is used for instrument control and data acquisition. Both systems are primarily accessed and remotely operated from our Boulder offices. On-site tests, maintenance, and other instrument work are mainly covered by two scheduled site visits each year. Local technical staff provide support when needed. Ambient samples are taken daily at 2:00 AM local time, followed by measurements of a standard and zero air. Samples (volume = 2.8 L) are dried to a dew point of -45C and pre-concentrated onto an adsorbent trap containing Carboxen 1000 and Carboxen 1016 at -40C. Analytes are then injected onto the GC column by flash heating. Over 70 compounds are identified and routinely monitored; of these, 53 are quantified based on availability of standards. Analytes include compounds regulated by the Montreal Protocol, such as CFC-11, CFC- 12, CCl 4 , HCFC-22, HFC-134a and HFC-152a. Monitored VOCs include C2-C6 alkanes, alkenes, benzene, toluene and o-xylene. Most of the halocarbons are quantified based on a NOAA standard (certification, August 2014), and a few quantifications (PFC-116, HFC-143a, HFC-125, CFC-115 and CFC-114) are based on an older NOAA standard that was reanalyzed at the University of Bristol in 2012. A NIST standard (August, 2015) is used to quantify the hydrocarbons. Results: Presented here are the time series of preliminary results of the ambient mixing ratios for a few selected compounds. The data quality of some compounds, such as H-1301, may be improved by better integration methods, which have been implemented but not yet applied to some of the data. Compared with results from the nearby Jungfraujoch/Switzerland AGAGE site, some halocarbons, such as CFC-11, CFC-115, HCFC-22, HFC-134a and CH 2 Cl 2 , show good agreement in the absolute values of the mixing ratios, seasonal cycles, day-to-day variabilities, as well as the long-term rates of change. Other compounds, including CFC-12, H-1301, H-1201, methyl chloride and methyl bromide, agree well in seasonality and long-term trends, but have a significant difference in their absolute mixing ratios. Bias in the calibration standards used in obtaining these results at both sites is likely the cause for this discrepancy, and needs to be investigated. Lastly, compounds HCFC-141b and HCFC-142b show a high abundance with highly enhanced concentrations. Air leaking from within the station building is the most likely reason because the sample intake is situated only 4 meters above the building terrace and regular lab air tests have shown large enhancements of both compounds in indoor air. This problem is currently being addressed by installing a new sampling line with the inlet much further away from the station building. The hydrocarbon results show seasonal cycles that are in agreement with other global background observations. Acknowledgements: We thank Drs. Martin Vollmer and Stefan Reimann for sharing the AGAGE Jungfraujoch station data, and Brendan Blanchard for helping with chromatogram peak integrations. Jungfraujoch Zugspitze: 47.42° N, 10.98° E 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 0 200 400 600 Mixing Ratio (pptv) Benzene 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 0 500 1000 1500 2000 Mixing Ratio (pptv) n-Butane 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 -50 0 50 100 150 200 250 300 350 Mixing Ratio (pptv) i-Butane 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 0 500 1000 1500 2000 Mixing Ratio (pptv) Propane 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 0 1000 2000 3000 Mixing Ratio (pptv) Ethane 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 60 80 100 120 140 160 Zugspitze Jungfraujoch Mixing Ratio (pptv) HFC-134a 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 20 30 40 50 60 Zugspitze Jungfraujoch Mixing Ratio (pptv) HCFC-141b 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 20 25 30 35 40 Zugspitze Jungfraujoch Mixing Ratio (pptv) HCFC-142b 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 220 230 240 250 260 Zugspitze Jungfraujoch Mixing Ratio (pptv) HCFC-22 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 3.5 4.0 4.5 5.0 Zugspitze Jungfraujoch Mixing Ratio (pptv) H-1211 2013.0 2014.0 2015.0 2016.0 2.5 3.0 3.5 4.0 4.5 5.0 Zugspitze Jungfraujoch Mixing Ratio (pptv) H-1301 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 80 90 100 110 120 Zugspitze Jungfraujoch Mixing Ratio (pptv) CCl 4 2013.0 2014.0 2015.0 2016.0 0 50 100 150 200 250 300 350 Zugspitze Jungfraujoch Mixing Ratio (pptv) CH 2 Cl 2 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 220 230 240 250 260 Zugspitze Jungfraujoch Mixing Ratio (pptv) CFC-11 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 500 510 520 530 540 550 Zugspitze Jungfraujoch Mixing Ratio (pptv) CFC-12 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 0.0 1.0 2.0 3.0 Mixing Ratio (pptv) CH 2 Br 2 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 4.0 6.0 8.0 10.0 12.0 14.0 Zugspitze Jungfraujoch Mixing Ratio (pptv) Methyl Bromide 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 7.5 8.0 8.5 9.0 9.5 Zugspitze Jungfraujoch Mixing Ratio (pptv) CFC-115 2013.0 2013.5 2014.0 2014.5 2015.0 2015.5 2016.0 2016.5 450 500 550 600 650 700 750 Zugspitze Jungfraujoch Mixing Ratio (pptv) Methyl chloride

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Page 1: Wei Wang , Jacques Hueber , Abigale J. Curtis , Cédric Couret

Halogenated Trace Gases and Volatile Organic Compounds at the Global Atmosphere Watch Global Observatory Schneefernerhaus/Zugspitze, Germany

Introduction: Halocarbons and hydrocarbons (C2 - C8) are being monitored at the German GAW Global Station Zugspitze/Hohenpeissenberg, 2670 m a.s.l., Germany. At the Zugspitze summit, atmospheric monitoring has been performed since the late 1970’s. In 1998, measurements for the United Nation’s Global Atmosphere Watch program (GAW) moved to the environmental research station Schneefernerhaus, ~300 m below the summit, where they support the study of greenhouse gases, reactive gases and aerosols. In 2013, an automated, remotely controlled gas chromatography/mass spectrometry (GC/MS) analytical system was installed for the monitoring of chlorofluorocarbon and other halocarbon trace gases. Monitoring of volatile organic compounds (VOC) was added in 2015. Ozone depleting and climate-change related organic traces have been monitored for more than a decade at a network of ground-based stations within the Advanced Global Atmospheric Gases Experiment (AGAGE) program following the Montreal and Kyoto protocols, which primarily rely on MEDUSA GC/MS measurement systems. The GC/MS at Zugspitze is a much simplified instrument, providing a lower maintenance and lower cost option for the long-term monitoring of these species.

1Institute of Arctic and Alpine Research, University of Colorado, Boulder, CO 80309, USA. 2German Environment Agency, Global Atmosphere Watch Observatory Zugspitze/Hohenpeissenberg, Platform Zugspitze at Environment Research Station Schneefernerhaus, Germany

Wei Wang1, Jacques Hueber1, Abigale J. Curtis1, Cédric Couret2, Ludwig Ries2, Detlev Helmig1

CFC-11 CFC-113 CFC-114 CFC-115 CFC-12 CFC-13 H-1211 H-1301 H-2402 HCFC-22 HCFC-124 HCFC-141b HCFC-142b HFC-125 HFC-134a HFC-143a HFC-152a HFC-245fa HFC-365mfc methyl chloride CH2Cl2 chloroform

CCl4 methyl chloroform perchloroethylene methyl bromide CH2Br2 CHBr3 methyl iodide PFC-116 PFC-218 PFC-318 SF6 SO2F2 COS ethene ethane propene propane i-butane iso-butene 1,3-butadiene 1-butene trans-2-butene n-butane cis-2-butene

i-pentane 1-pentene isoprene trans-2-pentene cis-2-pentene n-pentane 2-methylpentane 3-methylpentane hexane benzene cyclohexane n-heptane toluene iso-octane octane ethylbenzene m-xylene o-xylene 1,2,4-trimethylbenzene 1,3,5-trimethylbenzene methanol ethanol acetaldehyde methyl formate actone

List of compounds monitored at Zugspitze. Those with standards available for quantification are indicated in bold. The compounds in italic are very often below the detection limit.

Brief description of the operation: The instrument contains two main components, a custom-built pre-concentration inlet system and an Agilent GC/MS. The inlet system is controlled by a Labview program that also acquires and stores the metadata. It is synchronized with the GC/MS system where Agilent ChemStation software is used for instrument control and data acquisition. Both systems are primarily accessed and remotely operated from our Boulder offices. On-site tests, maintenance, and other instrument work are mainly covered by two scheduled site visits each year. Local technical staff provide support when needed. Ambient samples are taken daily at 2:00 AM local time, followed by measurements of a standard and zero air. Samples (volume = 2.8 L) are dried to a dew point of -45C and pre-concentrated onto an adsorbent trap containing Carboxen 1000 and Carboxen 1016 at -40C. Analytes are then injected onto the GC column by flash heating. Over 70 compounds are identified and routinely monitored; of these, 53 are quantified based on availability of standards. Analytes include compounds regulated by the Montreal Protocol, such as CFC-11, CFC-12, CCl4, HCFC-22, HFC-134a and HFC-152a. Monitored VOCs include C2-C6 alkanes, alkenes, benzene, toluene and o-xylene. Most of the halocarbons are quantified based on a NOAA standard (certification, August 2014), and a few quantifications (PFC-116, HFC-143a, HFC-125, CFC-115 and CFC-114) are based on an older NOAA standard that was reanalyzed at the University of Bristol in 2012. A NIST standard (August, 2015) is used to quantify the hydrocarbons.

Results: Presented here are the time series of preliminary results of the ambient mixing ratios for a few selected compounds. The data quality of some compounds, such as H-1301, may be improved by better integration methods, which have been implemented but not yet applied to some of the data. Compared with results from the nearby Jungfraujoch/Switzerland AGAGE site, some halocarbons, such as CFC-11, CFC-115, HCFC-22, HFC-134a and CH2Cl2, show good agreement in the absolute values of the mixing ratios, seasonal cycles, day-to-day variabilities, as well as the long-term rates of change. Other compounds, including CFC-12, H-1301, H-1201, methyl chloride and methyl bromide, agree well in seasonality and long-term trends, but have a significant difference in their absolute mixing ratios. Bias in the calibration standards used in obtaining these results at both sites is likely the cause for this discrepancy, and needs to be investigated. Lastly, compounds HCFC-141b and HCFC-142b show a high abundance with highly enhanced concentrations. Air leaking from within the station building is the most likely reason because the sample intake is situated only 4 meters above the building terrace and regular lab air tests have shown large enhancements of both compounds in indoor air. This problem is currently being addressed by installing a new sampling line with the inlet much further away from the station building. The hydrocarbon results show seasonal cycles that are in agreement with other global background observations. Acknowledgements: We thank Drs. Martin Vollmer and Stefan Reimann for sharing the AGAGE Jungfraujoch station data, and Brendan Blanchard for helping with chromatogram peak integrations.

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Methyl chloride