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Next Section: Summary and Conclusions Title/Abstract Page: The Wisconsin H Mapper Previous Section: The Wisconsin H-Alpha Mapper | Contents Page: Volume 15, Number 1 |
Between January 1997 and September 1998, WHAM will carry out one of
its primary missions, a northern sky H
survey of the warm ionized
medium. This survey will consist of approximately 33,000 spectra above
declination
, sampling the sky on a 0.
85
0.
98 grid with a 1
beam. Each spectrum has a 30 s
integration time and covers a 4.4 Å (200 km s
) spectral interval
centered near the LSR at a resolution of 0.26 Å (12 km s
). All
observations are carried out during dark of the moon to avoid
contamination by features in the solar spectrum. This survey will provide
for the first time a detailed view of the distribution and kinematics of
the diffuse ionized hydrogen through the optical H
line
comparable to the large scale survey maps of the neutral hydrogen
obtained through the radio 21 cm line.

Figure 2: WHAM H
data for
. a) the raw CCD camera image (30 s exposure); b) the spectrum
produced by annular binning of the CCD image (
denotes the
geocoronal line); c) the final, pure interstellar H
spectrum after
flat fielding, the removal of the geocoronal line, and the subtraction of
the sky background continuum. The intensities of the two blended
interstellar lines near -15 km s
and +15 km s
(LSR) are
approximately 4 R and 2 R, respectively.
Figure 2 illustrates a sample spectrum from the survey at
,
, showing both the raw CCD image and
the resulting H
spectra. The geocoronal line is the thin, bright
annulus in the CCD ``ring spectrum'', which appears as a prominent,
relatively narrow emission line in the center frame of Figure 2. The
interstellar emission is the broader feature inside the geocoronal ring,
appearing in this case to consist of two blended velocity components at
+30 km s
and +60 km s
with respect to the geocoronal line.
In general, the separation between the interstellar emission and the
geocoronal line is due to a combination of the earth's orbital velocity,
the sun's peculiar velocity, and intrinsic motions of the interstellar
gas, including Galactic differential rotation. The two interstellar
components have intensities of about 2 R and 4 R, where a Rayleigh, 1 R =
2.41
erg cm
s
sr
at H
and
corresponds to an emission measure of 2.3 cm
pc for a temperature
of 8000 K (Reynolds 1991). The geocoronal line is removed from the data
by fitting each spectrum with gaussian components and then subtracting
from the spectrum the fitted gaussian associated with the geocorona. The
resulting pure interstellar spectrum is shown in the third frame of Figure
2. The absolute intensity calibration is obtained by comparison with
standard astronomical sources (e.g., Scherb 1981).
A portion of the survey data is presented in Figure 3 as a gray scale
map of the total intensity of the interstellar H
emission. This
map, synthesized from approximately 7000 H
spectra, covers the
region of the sky between about 170
to 240
Galactic
longitude and
50
Galactic latitude. The gray scaling and
stretch have been adjusted to reveal the fainter high latitude emission
along with the brighter regions near the plane. Interstellar H
emission is detected in every direction, with intensities that range from
thousands of Rayleighs near the Orion nebula (
209
,
) and
100-200 R in Barnard's loop and the large
Ori H II region (195
,
) to
0.5 R
in some of the fainter high latitude regions (e.g., 220
,
+45
). The map reveals numerous large scale filaments superposed
on a fainter H
background. A number of ``classical'' H II regions
also dot the map near the Galactic equator. Some of the filamentary
features are associated with the Orion-Eridanus bubble (Reynolds & Ogden
1979; Sivan 1976), which fills the sky from l = 180
to
210
and
to
and includes
Barnard's Loop near its northern boundary. Many of the Orion-Eridanus
filaments appear to be correlated with emission features at 21 cm and
x-ray wavelengths (see, for example, Brown, Hartmann, & Burton 1995,
Burrows et al 1993, and Reynolds & Ogden 1979). Other filaments on
the map have no obvious correspondence to any previously known structures,
for example, the
10 R feature that extends north from l =
220
,
across the Galactic midplane to
215
, +5
or the fainter (1 R) feature rising vertically
from 226
, +10
to 229
, +50
. Narrow
velocity interval maps have also been constructed from these data,
revealing significant kinematic variations among the various emission
features (Haffner et al 1997, in preparation).

Figure 3: Total intensity map of the diffuse interstellar H
background in the Galactic anticenter region (extracted from the WHAM sky
survey). The map is in Galactic coordinates, with the Galactic equator
running horizontally through the center. The map is bounded on the left
by the
declination limit of the survey. Barnard's Loop
is the bright arc near
,
and the large
Ori H II region is centered near
,
.
The small black dots are pixels with missing data or spectra contaminated
by a bright star within the beam.
Although they have been observed via their 21 cm emission for many
years, the origin of the High Velocity Clouds (HVCs) is still not known
(Wakker et al 1996). The detection of HVCs in H
(Kutyrev &
Reynolds 1989; Songaila, Bryant, & Cowie 1989; Tufte et al 1996) and [S
II]
6716 (Tufte 1997) has opened a new window through which to
explore the nature of these objects. Furthermore, the M I and A clouds
have been found to be located far above the Galactic midplane, z =
1.5-4.4 kpc (Danly et al 1993) and 3-7 kpc (Wakker et al 1996; van
Woerden et al, private communication), respectively, making HVCs excellent
probes of the environment outside the Galactic disk. WHAM has detected
H
from the M I, M II, A, and C clouds with an intensity
0.1
R (Tufte et al, in preparation). If the H II in these clouds is produced
by photoionization, then the required ionizing flux is 1-2
10
photons cm
s
(Tufte 1997), which is about 5-10%
that required to produce the warm ionized component of the interstellar
medium in the disk. Observations in many directions toward and near the
M I cloud suggest that the H II is confined primarily to the region of 21
cm emission (at least in projection) and does not form an extended halo
about the cloud (Tufte et al 1996).
In addition to H
, WHAM is able to observe other emission
lines that probe the temperature and ionization conditions within the gas,
including [S II]
6716, [N II]
6584, [N II]
5755, He I
5876, [O I]
6300, and [O III]
5007 (Tufte et al 1996; Haffner et al 1996; Reynolds et al 1997).
Some of these lines are too faint to have been detected previously. For
example, the [O I]
6300 line intensity relative to H
is a
measure of the amount of neutral hydrogen within the warm ionized regions
and provides an important constraint on photoionization models (e.g.,
Domgörgen & Mathis 1994; Reynolds 1989). Observations with WHAM have
provided the first detections of this line from the diffuse interstellar
medium, with an intensity that varies from less than 1% to about 4% that
of the interstellar H
(Reynolds et al 1997). According to the
photoionization models (Domgörgen & Mathis 1994), these low [O
I]/H
intensity ratios suggest that most of the H
originates from density bounded, nearly fully ionized regions rather than
from partially ionized H I clouds or H II ``skins'' on the surfaces of H I
clouds.
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Next Section: Summary and Conclusions Title/Abstract Page: The Wisconsin H Mapper Previous Section: The Wisconsin H-Alpha Mapper | Contents Page: Volume 15, Number 1 |