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Activity 2.3 Team CarboEurope-IP Meeting, Posen, Poland, 7-12 Oktober, 2007 Flask network (A 2.3) Multiple species measurement What is expected from A 2.3 for reaching the CarboEurope IP ultimate goals? How far are we? What needs to be done?
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2.3.2.2 To develop innovative methodologies using Carbon Cycle related tracers and isotopes to attribute the CO 2 concentration in the European air shed to each of the constituent parts of the fluxes: fossil, oceanic, and terrestrial (MO8). Means to achieve objective (Activities 2.2; 2.3; 2.5; 2.6): Multiple species in situ measurements on tall towers Flask air sampling for multiple species analysis at ground stations and aircrafts Quality control program (intercomparisons; calibrations) to integrate atmospheric multiple species measurements from different laboratories Radiocarbon and CO measurements to separate the fossil fuel component General Objectives
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Objectives (5 yr plan) O2.3.1: To operate a unified co-operative European network of weekly flask sampling sites distributed among five laboratories. O2.3.2: To use flask multiple-species information to apportion the European carbon balance into components: fossil, air-sea exchange and terrestrial. O2.3.3: To develop new innovative and improvement of already existing analytical methods for measurements such as Ar/N2 (an ideal transport tracer over land); NMHC (a pollution tracer) and 13 C in CH 4 (tracer of methane sources).
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Objectives (5 yr plan) O2.3.1: To operate an unified co-operative European network of weekly flask sampling sites distributed among five laboratories. O2.3.2: To use flask multiple-species information to apportion the European carbon balance into components: fossil, air-sea exchange and terrestrial. O2.3.3: To develop new innovative and improvement of already existing analytical methods for measurements such as Ar/N2 (an ideal transport tracer over land); NMHC (a pollution tracer) and 13 C in CH 4 (tracer of methane sources).
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The running flask network O2.3.1: (NOAA sites not included)
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How far are we?
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Comparison for CO 2 (flask, online) at JFJ
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Comparison of CO 2 flask records
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Comparison of O 2 flask records Bern scaleJena scaleGroningen scale
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Valentino et al., in press
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In our view those changes can neither be explained by increased fossil fuel emissions nor by a changing biospheric activity. We favour a strong influence from the Atlantic ocean, most probably pentadal or decadal variations of circulation combined with heat storage variations.
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Jungfraujoch footprint (5 days BTraj, 5 Traj. every 4 hour) S. Nottelmann, EMPA 2007
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Measurements on Jungfraujoch, Switzerland
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S. Nottelmann, EMPA 2007 Measurements on Jungfraujoch, Switzerland
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S. Nottelmann, EMPA 2007 Measurements on Jungfraujoch, Switzerland
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S. Nottelmann, EMPA 2007 Measurements on Jungfraujoch, Switzerland
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S. Nottelmann, EMPA 2007 Measurements on Jungfraujoch, Switzerland
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S. Nottelmann, EMPA 2007 Measurements on Jungfraujoch, Switzerland
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S. Nottelmann, EMPA 2007 Measurements on Jungfraujoch, Switzerland
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S. Nottelmann, EMPA 2007 Measurements on Jungfraujoch, Switzerland
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Network is running but sometimes with rather poor data coverage due to ? ? ? Flask air measurements help to verify the calibration of continuously recorded values. In principle multi-species measurements on the same air sample allows us to disentangle processes and quantify their contributions, but the data resolution is critical in this regard. Data resolution is also a critical issue for trend and amplitude determinations as shown on Sunday during the trend meeting. I urge people to look not only at their own data, but to use others data and work with them to reach a synthesis until next year. Thank you for your attention Conclusions and the future…:
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