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The thesis is devoted to the study of the Antarctic polar vortex, mainly by analyzing data collected during APE-GAIA (1999) and ASHOE (1994) campaigns and recorded by the ADEOS satellite (1996-1997), and to improvement of the chromato-graphic processing schemes. A general introduction and overview of the campaigns and instruments relevant to the present work are given in Chapters 1 and 2. A relatively large part of the thesis (Chapters 3-5) is on improvement of the analysis of raw chromatographic data recorded during in-flight measurements of the trace gases. A Gaussian non-straight-base-line method, i.e. the Gaussian processing scheme (Chapter 3), is developed for better evaluation of the chromatographic peak size. Furthermore, a statistical cross-correlation method (Chapter 5) based on statistical behaviour of the whole chromatogram series fNchrg recorded, e.g., during a research flight or laboratory calibration, is developed and applied to measure the low-concentration trace gases. As demonstrated for HAGAR's chromatograms (HAGAR - High Altitude Gas Analyzer), the combination of the Gaussian fitting scheme for individual chromatograms and the statistical cross-correlation method for a series of subsequent chromatograms considerably improves and stabilizes quantitative analysis of in-flight chromatographic data. In this case, the detection accuracy of weak and noisy chromatographic signals can be improved by up to 40 %. A particular attention is paid to the in-flight two-standard calibration method. For this method, a special procedure, that allows to evaluate and effectively remove a weak background chromatographic signal associated with residual molecules in the carrier gas N2, is proposed and coded (Chapter 4). The developed approaches and methods are completely automized and, therefore, can be used for processing of in-flight chromatograms of recent and future field campaigns. The main part of the thesis (Chapters 6-8) deals with a two-dimensional quasi-Lagrangian coordinate system ... , based on a long-lived stratospheric trace gas i, and its systematic use for i = N2O in order to describe the structure of a well-developed Antarctic polar vortex, linearization and compactization of the tracer-tracer correlations in the polar vortex core (i.e. the stratospheric dynamics in this area), and the differential ozone losses in the Antarctic polar vortex area. In the coordinate system ... (...-method, Chapter 6), which refers to a well-developed polar vortex, the mixing ratio Âi is the vertical coordinate and ... = .... i is the reference profile in the vortex core) is the meridional coordinate. The quasi-Lagrangian coordinates ... are much more long-lived comparing with the standard quasi-isentropic coordinates, potential temperature ... and equivalent latitude ..e, do not require explicit reference to geographic space, and therefore well-suited for studying the dynamics of the Antarctic polar vortex and the relevant ozone loss processes. By using the introduced coordinate system ... to analyze the well-developed Antarctic vortex investigated in the APE-GAIA campaign, it is shown, in concurrence with the conclusion of A. M. Lee et al. (2001), that the Antarctic vortex area can be described in terms of the well-mixed and well-isolated vortex core, relatively wide vortex boundary region and adjoining surf zone. In this case, the reference profile ... i , which is compact in a well-developed and isolated polar vortex core [J. B. Greenblatt et al. (2002)], can be found by combining airborne (and/or balloon) data with high-altitude satellite measurements. A criterion, which uses the local in-situ measurements of Âi = Âi(£) and attributes the inner vortex edge to a rapid change (±-step) in the meridional pro¯le of the mixing ratio..., is developed in Chapter 6 to determine the (Antarctic) inner vortex edge. In turn, the outer vortex edge of a well-developed Antarctic vortex is proposed to attribute to the position of a local maximum of ...H2O in the polar vortex area. For a well-developed Antarctic vortex, the ...-parametrization of tracer-tracer correlations allows to distinguish the tracer-tracer inter-relationships in the vortex core, vortex boundary region and surf zone (Chapter 7). This is clearly illustrated by analyzing the tracer-tracer relationships Âi ¡ ÂN2O obtained from the in-situ data of the APE-GAIA campaign for i = CFCl3 (CFC-11), CF2Cl2 (CFC-12), CBrClF2 (H-1211) and SF6. The solitary anomalous points in the ...CFC11 ¡ ÂN2O correlation, observed in the Antarctic vortex core during the APE-GAIA and ASHOE campaigns, are interpreted in terms of small-scale localized differential descent. As detailed in Chapter 8, the quasi-Lagrangian coordinate system fÂN2O; ¢ÂN2Og is an effective tool for evaluation of the differential ozone losses in the polar vortex area. With this purpose, a two-parametric reference function ...O3 = F(...), which characterizes the unperturbed O3 distribution in the early winter polar vortex area, is introduced to separate and quantify in terms of the meridional coordinate ...2O the differential ozone losses in the vortex core and vortex boundary region. The method is applied to analyze the ozone depletion in the Antarctic stratosphere during the austral spring 1999 (APE-GAIA campaign). In Chapter 9, the main results of the thesis are summarized.
The high energy loss of heavy ions in matter as well as the small angular scattering makes heavy ion beams an excellent tool to produce almost cylindrical and homogeneously excited volumes in matter. This aspect can be used to pump short wavelength lasers. In an experiment performed at the GSI (Gesellschaft für Schwerionenforschung, Darmstadt, Germany) ion accelerator facility in December 2005 the well-known KrF* excimer laser was pumped with an intense high energy uranium beam. Pulses of an uranium beam with initial particle energy of 250 MeV per nucleon, provided by heavy-ion-synchrotron SIS-18, were delivered to the HHT-target station and then stopped inside a gas laser cell. The maximum beam intensity reached in the experiment was 2,5·109 particles per pulse, which resulted in 34 J/g specific energy deposited in the laser gas. By applying electron cooling and a bunch compression technique at SIS-18, the beam pulses were compressed down to 110 ns (FWHM). A mixture of an excimer laser premix gas (95,5% Kr + 0,5% F2) and a buffer gas (Ar 4.8) was used as the laser gas in proportions of 35/65 and 60/40, respectively. The gas pressure inside the laser cell was varied in the range of 1,2÷2 bar in continues flow mode. The experimental setup consisted of a 1 m long stainless steel tube with a number of diagnostic viewports and two mirror adjustment units. The optical cavity was formed by a flat, Alcoated mirror at the beam entrance and a second dielectrically coated, highly reflective mirror with 3 m radius of curvature at a distance of 1,3 m. A beam of heavy ions has been used to pump a short wavelength gas laser for the first time. Laser effect on the KrF* laser transition (λ = 248 nm) has been successfully demonstrated. Laser threshold for this specific setup was reached with a beam intensity of 1,2·109 particles per pulse. Laser action has been clearly proofed by the following methods: appearance of the laser line, spectral narrowing of the laser line, temporal narrowing of the laser signal, non-linear response of the laser output intensity on the pumping power, and cavity disalignment effect. An energy of the laser pulse of about 2 mJ was measured for an ion beam intensity of 2·109 particles per pulse. The time delay of the onset of the laser emission with respect to the pumping pulse was measured as a function of ion beam intensity. The dependence of spontaneous emission spectra on the gas pressure in a range of 1,3÷2 bar was observed and the optimal gas pressure for laser experiments in the sense of laser efficiency was concluded. As a next step in studying short wavelength lasers pumped with heavy ion beams it is planned to reduce the laser wavelength down to the VUV region of the spectrum, and to proceed to the excimer lasers of the pure rare gases: Xe2 * (λ = 172 nm), Kr2 * (λ = 146 nm), Ar2 * (λ = 126 nm), Ne2 * (λ = 83 nm) and He2 * (λ = 80 nm). We believe that the use of heavy ion beams as a pumping source may lead to new pumping schemes on the higher lying level transitions and considerably shorter wavelengths (XUV and X-ray spectral region), which rely on the high cross sections for multiple ionization of the target species.