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NASA Scientific and Technical Aerospace Reports

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temperature <strong>and</strong> relative humidity measurements. The archived data are available at:http: //croc.gsfc.nasa.gov/shadoz. In<br />

Thompson et al., accuracies <strong>and</strong> imprecisions in the SHADOZ 1998- 2000 dataset were examined using ground-based<br />

instruments <strong>and</strong> the TOMS total ozone measurement (version 7) as references. Small variations in ozonesonde technique<br />

introduced possible biases from station-to-station. SHADOZ total ozone column amounts are now compared to version 8<br />

TOMS; discrepancies between the two datasets are reduced 2\% on average. An evaluation of ozone variations among the<br />

stations is made using the results of a series of chamber simulations of ozone launches (JOSIE-2000, Juelich Ozonesonde<br />

Intercomparison Experiment) in which a st<strong>and</strong>ard reference ozone instrument was employed with the various sonde techniques<br />

used in SHADOZ. A number of variations in SHADOZ ozone data are explained when differences in solution strength, data<br />

processing <strong>and</strong> instrument type (manufacturer) are taken into account.<br />

Author<br />

Atmospheric Composition; Atmospheric Temperature; Data Processing; Ozone; Pressure Measurement; Total Ozone Mapping<br />

Spectrometer; Troposphere; Stratosphere<br />

20040070945 <strong>NASA</strong> Marshall Space Flight Center, Huntsville, AL, USA<br />

Differential Velocity between Solar Wind Protons <strong>and</strong> Alpha Particles in Pressure Balance Structures<br />

Yamauchi, Yohei; Suess, Steven T.; Steinberg, John T.; Sakurai, Takashi; Journal of Geophysical Research; 2004; ISSN<br />

0148-0227; Volume 109; 1 pp.; In English; Ulysses Science Working Team Meeting, 22-23 Apr. 2004, Noordwijk,<br />

Netherl<strong>and</strong>s; No Copyright; Avail: Other Sources; Abstract Only<br />

Pressure balance structures (PBSs) are a common high-plasma beta feature in high-latitude, high-speed solar wind. They<br />

have been proposed as remnants of coronal plumes. If true, they should reflect the observation that plumes are rooted in<br />

unipolar magnetic flux concentrations in the photosphere <strong>and</strong> are heated as oppositely directed flux is advected into <strong>and</strong><br />

reconnects with the flux concentration. A minimum variance analysis (MVA) of magnetic discontinuities in PBSs showed there<br />

is a larger proportion of tangential discontinuities than in the surrounding high-speed wind, supporting the hypothesis that<br />

plasmoids or extended current sheets are formed during reconnection at the base of plumes. To further evaluate the character<br />

of magnetic field discontinuities in PBSs, differential streaming between alpha particles <strong>and</strong> protons is analyzed here for the<br />

same sample of PBSs used in the MVA. Alpha particles in high-speed wind generally have a higher radial flow speed than<br />

protons. However, if the magnetic field is folded back on itself, as in a large-amplitude Alfven wave, alpha particles will<br />

locally have a radial flow speed less than protons. This characteristic is used here to distinguish between folded back magnetic<br />

fields (which would contain rotational discontinuities) <strong>and</strong> tangential discontinuities using Ulysses high-latitude, high-speed<br />

solar wind data. The analysis indicates that almost all reversals in the radial magnetic field in PBSs are folded back field lines.<br />

This is found to also be true outside PBSs, supporting existing results for typical high-speed, high-latitude wind. There remains<br />

a small number of cases that appear not to be folds in the magnetic field <strong>and</strong> which may be flux tubes with both ends rooted<br />

in the Sun. The distinct difference in MVA results inside <strong>and</strong> outside PBSs remains unexplained.<br />

Author<br />

Alpha Particles; Protons; Solar Wind; Pressure<br />

20040073558 Naval Research Lab., Washington, DC<br />

Atmospheric Photo Ionization of Argon with a Short Pulse Laser<br />

Manheimer, Wallace; Mar. 28, 2004; 17 pp.; In English<br />

Report No.(s): AD-A422355; NRL/MR/6707--04-8751; No Copyright; Avail: CASI; A03, Hardcopy<br />

One of the goals of the NRL laser-atmospheric propagation program is to produce a plasma spot, at a controlled range<br />

with a combination of longitudinal compression of a laser pulse over long distance, followed by transverse self focusing over<br />

short distance. The ease by which one can accomplish this depends, at least in part, on the ionization mechanism. This report<br />

suggests that photo ionization of the argon component, via a four photon resonant excitation, followed by ionization of the<br />

highly excited state could be easier to accomplish than ionization of the oxygen by a direct four photon process, a seemingly<br />

more obvious choice. The reason is that the former is a resonant process, while the latter is not. While detailed calculations<br />

are not performed, initial crude calculations indicate that the rate via the argon channel could exceed the rate via the oxygen<br />

channel by several orders of magnitude.<br />

DTIC<br />

Argon; Atmospheric Circulation; Atmospheric Ionization; Gas Ionization; Pulsed Lasers<br />

144

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