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Arecibo Survey(s) of the Magellanic Stream: Past & Future. Snezana Stanimirovic (UC Berkeley). Recent Arecibo HI observations of the Magellanic Stream Results and Motivation for Future Surveys Future Surveys of the Magellanic Stream with ALFA Baseline Removal & Standing Wave Concerns.
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Arecibo Survey(s) of the Magellanic Stream: Past & Future Snezana Stanimirovic (UC Berkeley) • Recent Arecibo HI observations of the Magellanic Stream • Results and Motivation for Future Surveys • Future Surveys of the Magellanic Stream with ALFA • Baseline Removal & Standing Wave Concerns People involved: J. Dickey (Univ. of Minnesota), M. Krco (Colgate Univ.), A. Brooks (Columbia Univ.), A. Hedden (Univ. of Arizona)
HI Observational Perspective Parkes Multibeam data, 15 arcmin Putman et al. (2002) MS V MS VI Arecibo data, 3 arcmin Stanimirovic et al. (2002) Old Parkes data, 15 arcmin Mathewson & Ford (1984)
Recent Arecibo (305 m) HI Observations • Hidden Beast of a Mapping Machine!!! • All spatial scales ! • Good spatial resolution, 3-4 arcmin. • Great sensitivity • Allows fast mapping • On-the-fly mapping of many small maps (10’x10’): drive in RA (4’’/s), step in Dec (2’) and record data every 30 sec. • B=6.25 MHz, N=1024, Δv ~ 1 km/s, final θ ~ 4 arcmin. • Data processing performed completely in IDL. • Calibration, baseline removal by fitting a polynomial. • Maps combined during the gridding process using AO_Gridzilla. • Philosophy: Calibrate quickly, make maps & follow interesting features! Maps produced almost in real time!
MS VI: Morphology & Velocity Field Velocity Channels Broad velocity profiles DEC • Broad line profiles. • Compression fronts, head-tail morphology, velocity gradients. • Blending of clumps & their interaction with the surrounding medium. RA
Main Results: • Complex and interesting morphology found far away from the Magellanic Clouds.Bow-shock-like features, head-tail morphology, interesting velocity gradients. • Magellanic Stream as a thermometer for the outer Halo: • We have investigated confinement mechanism of several isolated Stream clumps. • Clumps are not in free expansion. They can not be gravitationally stable unless large amounts of dark matter are involved. • Clump properties are the easiest explained with external pressure confinement by the hot Galactic Halo gas. • Upper limit on the Halo density can be estimated. • Fully sampled, large-scale survey of the northern Stream will find many more clumps and allow building of a 2-D distribution of the Galactic Halo density.
Clumps Must be Confined by the Hot Galactic Halo gas ! nh ~ 10 -3 cm-3 at z ~ 15 kpc nh~ 3x10-4 cm-3 at z ~ 45 kpc
Future GALFA Survey(s) of the Magellanic Stream: an example • To survey whole northern part of the Stream visible from Arecibo: • (l=90 +/-10 deg, b=-55 to -20 deg) ~ 800 square degrees • B ~ 6 MHz • N ~ 2k • S ~ 0.1 K (or less) • scanning in RA with rate of 12 “/sec and stepping in Dec by 4.5’ requires 75 min per square degree or 1200—1400 hours for the whole survey. • As lines are broad a good technique for baseline removal is essential.
Arecibo Baselines: an example Multiple standing waves whose cancellation is a real challenge.
Best Technique for Baseline Removal ? • Position switching: - using nearby reference spectrum, e.g. Lizano et al. (1988) - using ‘empty’ edge spectra - difficult when sources are very extended • Polynomial fitting --- hard when profiles are broad • Frequency switching --- currently not possible due to complex spectral standing waves - Briggs et al. (1997) were able to characterize standing waves pre- upgrade and successfully remove them from drift-scan data - standing wave serious characterization hasn’t been done after the upgrade - Salter & Ghosh (2001): successfully characterized standing waves due to a point source in the main beam - Stanimirovic & Salter (2002): explored freq. switching and signal recovery algorithms Serious concern and requires serious investigation.