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Activity Report
The group has continued its work in the areas of atomic and molecular spectroscopy, and
the development of Fourier transform spectrometers that operate in the ultra-violet and
vacuum ultra-violet regions of the spectrum. These instruments, of uniquely high resolving power,
efficiency and range, are being used to provide the data needed for the
better understanding of the atmospheres both of stars and of the earth.
Laboratory Astrophysics
The spectra of stars are usually extremely complex: all the elements of the
periodic table may contribute, each in more than one stage of ionisation
and blends of several lines are the rule rather than the exception. Much
of the spectral data in the literature (atomic energy levels, transition
wavelengths, oscillator strengths and hyperfine structure)
is too inaccurate and incomplete to
resolve these blends, especially in the ultra-violet. We have recently
published new analyses of the spectra of three cosmically abundant species,
Fe, Ni, Ti and Co; work is in progress on Mn I, Cr I, V I and V II. A recently acquired
Penning discharge source has allowed spectra of doubly ionised species
to be recorded, of importance for hot stars. Studies in progress include
Fe III, Mn III and Ni III. The spectral range of our instruments in well
matched to that of the high resolution spectrograph on the Hubble Space
Telescope, as a result of which our data on the spectra of elements such
as Pt and Pb have been used to establish isotopic abundance anomalies in hot stars.
New accurate atomic data is vital for reliable interpretation
of high resolution astrophysical spectra,
such as those recorded with the UHRF (Ultra High
Resolution Facility) on the Anglo-Australian telescope, and in the future
with the planned HROS (High Resolution Optical Spectrograph) on GEMINI.
More details of atomic spectroscopy projects for astrophysics applications:
Group research report: Atomic Spectroscopy
Juliet C. Pickering: Research summary
Anne P. Thorne: Research summary
Richard Blackwell-Whitehead: Research Summary
Molecular Spectroscopy of Atmospheric Relevance
Our work on molecules relevant to the terrestrial atmosphere concentrates on spectral
line parameter analysis giving essential data for precise analysis of observations made
from downward looking satellites and is important for studies of the greenhouse effect
and global warming. Measurements of the SO2 bands in the near and middle UV, required
for planetary and terrestrial atmospheres and measurements of molecular oxygen in the
visible have been completed. The spectral analysis of the visible O2 data included the
two most abundant oxygen isotopomers and yielded results of unprecedented precision.
Molecular constants and line parameters in the visible oxygen A band
(Fig. 1) were measured,
and this data is of direct application to atmospheric pollution
measurements, and the accurate modelling of the penetration of solar radiation into the upper
atmosphere. Furthermore, the oxygen data is of crucial importance for the remote sensing
of cloud-top height and coverage for satellite based measurement of atmospheric ozone and
other atmospheric trace gases, and so of application to European satellite systems such as
GOME (Global Ozone
Monitoring Experiment) and
SCIAMACHY
(Scanning Imaging Absorption Spectrometer for Atmospheric Chartography).
A study, collaborating with J.W.Brault, ( U.S.A), of the very weak O2 Delta bands in the
near-infrared is also being carried out.
Projects funded by ESA and NERC (with University
College London and the Molecular Spectroscopy Facility at
Rutherford Appleton Laboratory, (RAL) investigate the water vapour spectra in the near-infrared and
visible spectral regions aiming to provide precise spectral line parameters, as well as
data on weak, previously unobserved, spectral absorptions. The results of these studies
not only add a significant amount of weak lines to the water database, but also identified
serious errors in the line intensities in the existing database. In collaboration with
J.Haigh and W.Zhong (SPAT, IC), the new data has been included in atmospheric radiative
transfer calculations and showed, that it will substantially increase the calculated
absorption of solar energy in climate models by a moist cloud-free atmosphere. This data
will significantly contribute to the solution of the so-called "missing absorber problem"
and will have a large impact on the modelling of atmospheric radiative transfer and
climate.
Current studies include work on the far UV bands of SO2
for investigations of terrestial and planetary atmospheres; for example knowledge of
SO2 absorption cross-sections enables SO2 to be used to monitor volcanic activity on Io, a
moon of Jupiter. Further work is
planned on weak absorptions of water in the visible and near-infrared, which may have a
significant contribution to the earth's solar radiation budget and may explain the existing
serious discrepancies between the observed and modelled atmospheric radiation budgets,
an effect which is much larger than the probable magnitude of greenhouse effects and thus
has an impact on the credibility of this very serious topic. These programmes involve
collaborative work with the CfA Atomic and
Molecular Physics Laboratory at the
Harvard-Smithsonian Center for Astrophysics,
Wellesley College, U.S.A., the Theoretical
Atomic and Molecular Physics and Astrophysics Group at the
University College London and the
Spectroscopy and Remote Sensing Group at the
Rutherford Appleton Laboratory.
Group Research Report: Molecular Spectroscopy
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