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Global scale observations of δD(H2)




                          Anneke M. Batenburg
  Gerben Pieterse, Sylvia Walter, Ingeborg Levin, Martina Schmidt, Armin
                  Jordan, Samuel Hammer, Camille Yver,
Tanja J. Schuck, Angela K. Baker, Andreas Zahn, Carl A. M. Brenninkmeijer,
                          and Thomas Röckmann
Introduction   H2 sources and sinks
H2 budget with isotope
                    signatures
Introduction
Two new δD(H2) datasets


     Time series from six globally
     distributed background
     stations
     (Batenburg et al., Atmos. Chem. Phys., 11, 6985-6999, 2011)



     Observations in the tropopause
     region
     (Batenburg et al., Atmos. Chem. Phys., 12, 4633-4646, 2012)
Background station time series   The EUROHYDROS network
Background station time series   Time series
Background station time series   Highlight: Alert
Background station time series   Latitudinal gradients
Background station time series   Relative sink contribution
Two new δD(H2) datasets


     Time series from six globally
     distributed background stations
     (Batenburg et al., Atmos. Chem. Phys., 11, 6985-6999, 2011)




     Observations in the
     tropopause region
     (Batenburg et al., Atmos. Chem. Phys., 12, 4633-4646, 2012)
Observations around the TP   In the stratosphere




                                     Röckmann et al. (2003)
Observations around the TP   In the stratosphere
In the stratosphere
                                          Rahn et al. (2003)
Observations around the TP
Observations around the TP          In the stratosphere

                             Result of
                             stratospheric
                             processing:
                             • H2 mixing ratio
                               changes little
                             • δD increases
                               dramatically.
Observations around the TP         Stratospheric input




                             Pieterse et al., Atmos. Chem. Phys., 11, 7001-7026, 2011
Observations around the TP   Geographical coverage
Observations around the TP   Example: Caracas flights
Observations around the TP   Stratospheric samples
Observations around the TP   Stratospheric samples
Observations around the TP   Stratospheric samples
Observations around the TP   Monsoon samples
To sum up:

Ground station δD(H2) data
• show variation with season and latitude.
• contain source/sink information.




δD(H2) data from TP region
• yield better parameterization of δD(H2) in STE
• may show new source over India
Latest TM5 results


                   Isotope data help in
δD(H2) in models




                   distinguishing
                   between different
                   plausible scenarios


                   Pieterse et al., Reassessing
                   the variability in atmospheric
                   H2 using the two-way nested
                   TM5 model, submitted to
                   JGR
δD(H2) in models   Improved budget
Introduction   Future H2 use and leakage
Introduction           Isotope δ notation




               The δD(H2) value represents the deuterium-to-
               hydrogen ratio in the H2 relative to a standard
               (Vienna Standard Mean Ocean Water
               (VSMOW)).
CARIBIC measurement container
                              Mass 1.5 ton   Deployment monthly
 Observations around the TP


                                                                    Cargo door




Airbus
A 340-600
D-AIHE


                                                 Air inlet system
                                                 Permanent part
Observations around the TP   Monsoon samples

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Batenburg agu 2012_11_26