The origin of the neutral-hydrogen HVCs has been an enigma for the last 36 years. The main problem in the study of these objects are the distances: they are unknown for most of the HVCs and, therefore, few of the basic physical properties of the clouds can be determined. For a review of problems and progress, see Wakker & van Woerden ([1997]).
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Figure 1:
Sky distribution of the 6848 HV components detected from the IAR
H I survey with velocities
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The northern sky has been surveyed several times looking for HVCs (see Table 1
in the review of Wakker & van Woerden [1997]). Recently,
Hartmann & Burton ([1997]) finished
the Leiden-Dwingeloo HI survey made with a finer grid and higher velocity
resolution than previous ones. This survey can be used for the creation of
a catalogue for all the anomalous-velocity gas. However, for the southern sky
the investigation of HVCs was restricted to the use of old surveys. It was
first surveyed for HVCs by Mathewson et al. [1974]), using the 18-m
reflector at the Parkes Observatory of CSIRO (HPBW
48
),
every 2.5 to 5 degrees in declination and moderate
sensitivity (typically 0.3 K). The main result of this survey was the finding
of the extended HI complex known as the Magellanic Stream. Later, Bajaja et al.
([1985]) made a new survey using the 30-m IAR dish (HPBW
34
), on a 2
2
grid and a detection limit of
0.08-0.10 K. As a result of these observations, a large number of small
clouds was discovered. As we can see, a drawback of these surveys was the fact
that the antenna beams were smaller than the observed grid spacing.
More recently, Putman & Gibson ([1999a], [1999b]) presented
the first
results from their complete, fully sampled, southern sky survey for HVCs, as
part of the HI Parkes All-Sky Survey (
). As they mentioned,
their initial results are revealing intricate details in the spatial structure
of southern HVCs, a large population of compact HVCs, and
filamentary connections between previously assumed discrete clumps. Thus,
until these data become of public domain, the data available at present
on HVCs are quite insufficient for statistical purposes.
We decided to use the new general HI survey from the
southern hemisphere, recently completed by Arnal et al. ([2000]), to make
a more complete and homogeneous new survey of HVCs which will provide reliable
and unbiased statistical information on these enigmatic objects.
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Figure 2: LSR velocity-longitude diagrams from the IAR data for a) the northern and b) southern hemisphere |
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Figure 3: a) LSR and b) GSR velocity-longitude diagrams from the IAR and Hulsbosch & Wakker's ([1988]) data |
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