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Titel |
On the consistency of the formation of polar stratospheric clouds (PSCs) and their chemical impact : in situ measurements and modeling approach. |
VerfasserIn |
A. Grossel, N. Huret, V. Catoire, G. Berthet, J.-B. Renard, C. Robert, B. Gaubicher |
Konferenz |
EGU General Assembly 2009
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Medientyp |
Artikel
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Sprache |
Englisch
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Digitales Dokument |
PDF |
Erschienen |
In: GRA - Volume 11 (2009) |
Datensatznummer |
250028078
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Zusammenfassung |
A balloon campaign at Kiruna (Sweden, 67.9Ë S-21.1Ë E) was conducted in January 2006
within the frame of the ENVISAT satellite validation. In situ measurements of gas mixing
ratios and particle size distributions were obtained simultaneously in the Arctic stratosphere.
In situ vertical profiles of O3, CO, CH4, CO2, N2O, NO2,HNO3 and HCl were provided by
the SPIRALE balloon-borne infrared spectrometer between 13 and 27.3 km with high vertical
resolution (~5m). The optical aerosol counter STAC was mounted on board the payload,
allowing in situ characterization of the vertical particle distribution in six size bins between
0.4 and 2.0 μm.
Very complex structures are observed on the HNO3 and HCl vertical profiles with very
low values in the 20.7–22 km layer. Correlations, especially for O3-HNO3, are used
to characterize specific layers and to identify different processes leading to the
observations. The correlations curves obtained show the presence of denitrified
layer. The high vertical resolution enables the identification of possibly localized
renitrification.
Clusters of backward trajectories have been calculated to investigate the thermal histories
of the sampled air masses. During the week before the measurements, low temperatures close
to the nitric acid trihydrate (NAT) saturation temperature were encountered along backward
trajectories.
The MIPLASMO (Microphysical and Photochemical Lagrangian Stratospheric Model of
Ozone, Riviere et al. 2003) has been then used to investigate PSC formation and the impact of
sedimenting particles on chemistry. Several homogeneous nucleation rates proposed in the
literature have been tested to address the question of NAT formation above the ice nucleation
temperature.
Riviere, E.D., Terao, Y. and Nakajima, H., 2003, A lagrangian method to study
stratospheric nitric acid variations in the polar regions as measured by the Improved Limb
Atmospheric Spectrometer. J. Geophys. Res, 108, 4718. |
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