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Advances in Space Research 36 (2005) 1415–1421
EUV spectroscopy for Solar Orbiter
R.A. Harrison
Space Science and Technology Department, Rutherford Appleton Laboratory, Chilton, Didcot, Oxfordshire OX11 0QX, UK
Received 28 July 2004; received in revised form 30 November 2004; accepted 10 December 2004
Abstract
Building on the success of EUV/UV spectroscopic studies fromx the SOHO mission in particular, a next generation spectroscopic
study of the Sun is included in plans for Solar Orbiter. The combination of close-up and out of ecliptic observation provides unique
possibilities for solar plasma diagnostics and these are outlined here. Technical challenges and the instrumental requirements for
such an instrument aboard Orbiter are described in detail.
� 2004 COSPAR. Published by Elsevier Ltd. All rights reserved.
Keywords: Sun; Solar activity; Solar atmosphere; EUV spectroscopy
1. Introduction
Spectroscopic observations of emission lines in the
EUV/UV region of the electromagnetic spectrum are
critical for the determination of plasma diagnostics from
the solar atmosphere, providing the necessary tools for
probing the wide solar plasma temperature range, fromtens of thousands to several million K. Analysis of the
emission lines, mainly from trace elements in the Sun�satmosphere, provides information on plasma density,
temperature, element/ion abundances, flow speeds and
the structure and evolution of atmospheric phenomena.
Such information provides a foundation for understand-
ing the physics behind a large range of solar phenomena.
Therefore, it is logical that such instrumentation shouldbe included in the Solar Orbiter strawman payload.
Current spacecraft instrumentation (SOHO, see Dom-
ingo et al., 1995, and references therein) provides EUV
spatial and spectral resolving elements of order 2 arc-
sec/pixel and 0.01 nm/pixel, respectively, and UV resolv-
ing elements of 1 arcsec/pixel and 0.002 nm/pixel. There is
no EUV or UV spectroscopic capability aboard the
NASA STEREOmission (2006 launch), the NASA Solar
0273-1177/$30 � 2004 COSPAR. Published by Elsevier Ltd. All rights reser
doi:10.1016/j.asr.2004.12.025
E-mail address: [email protected].
Dynamics Observatory (2008 launch) and the NASA
Solar Probe (currently under study). The only planned
EUV spectrometer for an approved future solar mission
at this time is the EIS instrument on Solar-B with 1 arc-
sec/pixel (750 km on the Sun) performance (Shimizu,
2002). We note that the wavelength selection of EIS is
tuned to higher temperature, coronal, plasmas, particu-larly well suited to studies of active regions and even
flares, rather than the quiet solar atmosphere in general.
Figs. 1 and 2 show a brief glimpse of the power of
EUV spectroscopy in studying the solar atmosphere.
Fig. 1 shows the Sun imaged in emission from six differ-
ent emission lines, effectively revealing six temperature
regimes at the same time, in the range 20,000 to
2,000,000 K. Fig. 2 shows a close up of an active regionon the western limb. A bright loop is clearly visible at
transition region temperatures. Analysis of the emission
line shifts show that above the loop there is a radial jet
of plasma which is spiralling outward from the Sun. The
ability to select particular emission lines for specific
analyses, to reveal temperatures, or densities, and spec-
tral analyses designed to reveal flow properties, are par-
ticularly valuable for determining the plasma propertiesof the solar atmosphere. The application of spectros-
copy in the EUV to solar phenomena is well demon-
ved.
Fig. 1. SOHO CDS images of the Sun taken in six emission lines from
helium, oxygen, magnesium and iron, representing temperatures from
20,000 K (top left) to 2,000,000 K (bottom right).
Fig. 2. A close-up of an active region loop, taken in the 250,000 K
emission line at 629 A from O V (oxygen ionised 4 times). Whilst the
left image shows the bright loop, a Doppler analysis of the emission
line reveals a spiral jet of plasma streaming vertically away from the
region.
1416 R.A. Harrison / Advances in Space Research 36 (2005) 1415–1421
strated by the publication of many hundreds of papersto date using the CDS and SUMER instruments on
SOHO (see sohowww.nascom.nasa.gov).
Solar Orbiter provides a unique platform for solar
spectroscopy, with close encounters and high latitude
Table 1
Instrument requirements and allocations
Goal
Spatial resolving element 1.0 arcsec pixels, or better
Spectral resolving element 0.02 A/pixel or better
Field of view 20 arcmin · 20 arcmin or larger
Wavelength prime bands 170–220, 580–630, >912 A
Pointing To anywhere on disc and low corona off-disc
Mass 25 kg
Telemetry 17 kbit/s
Autonomy Pre-planned sequences in deferred command sto
Stabilisation system May require active on-board system; on-ground
capabilities. SOHO has demonstrated well the power
of a combination of imaging and spectroscopy and this
has been a basic driver for the remote sensing package
on Orbiter. However, such a mission does pose signifi-
cant problems for instrument design, development and
operation, with particular issues including thermal ex-tremes, severe particle environments, a requirement for
autonomy during solar passes, and limitations on mass
and telemetry. An overview of the Solar Orbiter mission
is given by Marsch et al. (2001).
2. Instrument requirements
At this stage, the requirements for an EUV or UV
spectrometer on Solar orbiter are somewhat flexible.
However, Table 1 lists the major goals and limitations
as we understand them at present, and the allocations
for telemetry, mass, etc. Many of the items are discussed
in greater detail below.
3. Instrument optical design concept
Whilst recognising that an EUV/UV spectrometer is
an essential component of the Solar Orbiter, we must
be aware that the mission concept demands that it must
be compact and light-weight, must not be too telemetry
�thirsty� and must be able to cope with the thermal and
particle environment of such an orbit.A normal incidence system was originally envisaged
for this spectrometer, to fit within reasonable length lim-
its of the spacecraft. However, the thermal situation is
extreme, in particular for a normal incidence design.
The basic design we propose here is an off-axis normal
incidence (NIS) system where a single paraboloid pri-
mary mirror reflects the selected portion of the solar im-
age through a heat-stop to a spectrometer using avariable line spaced (VLS) grating in normal incidence.
The concept is shown in Fig. 3 The wavelength selec-
tions are geared to bright solar lines in the EUV from
a broad range of temperatures. The basic design concept
is presented by Thomas (2003).
Comment
150 km on the Sun at 0.2 AU
To separate emission lines and for flow studies
Size of active region from 0.2 AU
Prime bands to cover emission lines of interest
Co-pointed with remote sensing package
Due to spacecraft limitations
Current allocation
re No contact during solar encounters
option under study Spacecraft performance needs to be defined
Fig. 3. The basic design concept of the EUV spectrometer.
R.A. Harrison / Advances in Space Research 36 (2005) 1415–1421 1417
In this concept, the primary optical component is a
paraboloid mirror. The off-axis approach allows the
insertion of a heat-stop between the primary and the slit,
which only allows a selected area of the solar image into
the spectrometer. Most of the solar radiation is reflected
by the heat-stop out of the front aperture. Thus, thethermal challenge for this design is almost exclusively
concerned with the thermal control of the primary mir-
ror itself. We address this later.
The slit assembly lies at the focal plane, below the
heat-stop, and beyond this is the spectrometer, with a
toroidal VLS grating, forming a focus at a 2-D detector.
There is no secondary mirror, as with a Ritchey–Chret-
ien design, for example, and this helps to maintain a rea-sonable effective area. The VLS grating approach allows
good off-axis performance compared to a uniform grat-
ing, and it brings the spectrometer �arm� closer to the
axis of the instrument, making the envelope smaller.
The grating ruling spacing is yet to be decided but values
up to 4800 l/mm have been considered for design inves-
tigations. The use of a toroidal VLS grating allows a
spectrometer magnification, with values of 2.5 beingconsidered, whilst retaining optical quality.
Several wavelength bands are under consideration at
this time and have been discussed widely (e.g. Harrison
and Vial, 2001). Prime regions of the EUV spectrum
have been identified, which contain emission lines of
particular importance, and these include 170–220, 580–
630 and >912 A. These three would allow detailed stud-
ies of coronal, transition region and chromospheric plas-mas. Obtaining spectra from three such bands would be
very difficult, so we anticipate obtaining two of these
bands using either two orders or two detectors at the fo-
cus of the spectrometer.
The primary mirror presents a portion of the Sun at
the slit, and it is this mirror that can be rotated to allow
rastered images, i.e., exposures interlaced with mecha-
nism movements to build up images simultaneously inselected wavelengths. Only a small fraction of the Sun
will pass through the heat-stop to the slit assembly; pos-
sibly of order several hundredths of the disc area.
The instrument will not have independent pointing. It
will be hard-mounted with the other remote sensing
instruments, and used in conjunction with those instru-
ments. Limited independent pointing can be performedusing the primary mirror mechanism.
The instrument would include a selection of slits,
which can be chosen for particular observation pro-
grammes. In addition, it is noted that the instrument res-
olution may demand an image stabilisation system
which will involve motion of the primary mirror in re-
sponse to an external signal.
We note that what is presented here is one possibleoptical concept, which is very much based on heritage
from the SOHO-CDS instrument. At this stage, the
instruments are not yet selected. In addition, we point
out that whilst the thermal aspects of the normal inci-
dence design are being investigated, a second design op-
tion based on a grazing incidence Wolter II design is
also being considered. This would also include a variable
line spaced grating and similar detectors, but the ther-mal extremes encountered by such a design would be less
severe.
4. Resolution and the detector system
We size the instrument to an observing distance of
0.2 AU (perihelion). A spatial pixel size of 1 arcsec rep-resents 750 km on the Sun from the Earth; the same pix-
el at 0.2 AU represents 150 km. This is an order of
magnitude better than the CDS instrument pixel size
on SOHO (Harrison et al., 1995), a factor of five better
than the SUMER instrument on SOHO (Wilhelm et al.,
1995) and about half the size of the best EUV imaging
capability (TRACE, 0.5 arcsec pixels at 1 AU). Our ba-
sic aim is to achieve 1 arcsec pixel elements, recognisingthat (a) the limitations of mass and telemetry demand a
compact instrument with little complexity, in terms of
the basic optical layout, operation, and the use of mech-
anisms, etc. and (b) the novelty of the mission is really
derived from the orbital path rather than major instru-
ment advances. We must be aware that Orbiter is not
a mission that can carry the large, complex instruments
one might expect from a near-Earth mission.Initial discussions included provision for a 0.5 arcsec
pixel (75 km on the Sun). This led to the consideration
of a detector array baseline of 4k · 4k 5 lm pixels. This
would also suggest that the instrument would have a
spectral range of 4 nm at 0.001 nm/pixel. The same array
will give a spatial extent (vertical distance on the detec-
tor = slit length) of 34 arcmin. The solar diameter at
0.2 AU is 170 arcmin, i.e., we have a slit length of 0.2of the solar diameter. For a given pointing location
(spacecraft pointing), rastered imaging will be made up
1418 R.A. Harrison / Advances in Space Research 36 (2005) 1415–1421
from movement in one direction of the primary mirror.
Thus, the basic rastered �field of view� would be 34 · 34
arcmin. This would be a size somewhat larger than a
large active region, i.e., somewhat larger than the CDS
field of view on SOHO.
The demand for 0.5 arcsec pixels (5 lm) has been re-laxed, with recent studies suggesting that a target of 1.0
arcsec (150 km on the Sun) is appropriate, i.e., it leads to
an instrument option whose size and mass is more con-
sistent with the spacecraft limitations. Although further
study is required, this may result in a 2k · 2k detector of
pixel size 10 lm. A parallel discussion about the field of
view has stressed that the minimum size should be 20
arcmin · 20 arcmin.The choice of detector is dictated by the harsh parti-
cle environment which will be encountered by Solar Or-
biter, as well as mass and power constraints. The
particle environment, which will be encountered by Or-
biter, means that CCD-type detectors will most likely be
inappropriate. We may anticipate a solar wind �back-ground� proton flux some 25· that of SOHO (1/r2).
For an average flux at 1 AU, of density 9 cm�3 (averagespeed and temperature of 300 km/s and 4 · 105 K
(3.5 keV)) we expect 225 cm�3 at 0.2 AU. Thus the nom-
inal particle environment will be similar to some modest
storm events detected occasionally by SOHO.
There may also be an increased chance of encounter-
ing proton �storms�, due to vicinity, from shocks associ-
ated with mass ejection, with up to thousands of proton
hits per second. One might expect events similar to thoseexperienced by SOHO, with greater intensity, and, in
addition, some near-Sun events may be generated by lat-
eral expansion of CME disturbances. The exact intensi-
ties remain unknown. The geometrical factors and
magnetic configurations, which may play a role in defin-
ing the chance of occurrence of storms are also ill
defined.
Also, we anticipate occasional impacts from solarflare neutrons whose 15.5 min lifetime means that most
missions do not encounter them. Finally, we anticipate a
similar cosmic ray (non solar) flux similar to that at
SOHO.
The net effect is an increase in particle hits, with some
extreme conditions including occasional neutrons. The
radiation damage in CCDs is mostly caused by the cre-
ation of charge traps reducing the charge transfer effi-ciency (CTE). The radiation hardness of silicon Active
Pixel Sensor (APS) detectors is much higher because
CTE degradation is unimportant; charge is not trans-
ferred across the array using an APS detector, where
on-chip electronics allows the extraction and amplifica-
tion of charge from each pixel individually. The charge
collection efficiency (CCE) may also degrade, but at
higher radiation levels.The APS detector system is a realistic option for So-
lar Orbiter from a particle environment point of view.
We note, however, that the on-chip electronics also pro-
vides additional low mass and power advantages, com-
pared to CCDs. The APS EUV sensitivity will be
provided in the same way as with CCDs, in this case
with back-thinned devices. As with CCDs, the APS sys-
tem would need to be cooled to about �80�, using a ded-icated radiator.
The development of the APS system, specifically for
Solar Orbiter applications is discussed by Prydderch et
al. (2004).
5. Thermal issues
At 1 AU the average solar intensity is 1.371 kW/m2.
During the nominal phase of the Solar Orbiter mission,
the spacecraft occupies a 149 day orbit with aphelion
and perihelion 0.8 and 0.2 AU, respectively. Thus, every
75 days, the spacecraft will encounter a range from
2.142 kW/m2 (0.8 AU) to 34.275 kW/m2 (0.2 AU – 25
times the value at 1 AU). This presents a severe thermal
challenge, which we tackle in a number of ways.The primary mirror ‘‘sees’’ the full Sun. It is a com-
monly held view that such a mirror would only view
the instrument field of view, but the opening angle is
such that the full Sun is visible to the mirror. The limits
on instrument length do not allow provision for a colli-
mated aperture. One option being studied is the use of
an uncoated SiC mirror. SiC optical components can
run hotter than traditional components. The originalmirror size under study was a 120 mm aperture, result-
ing in the primary receiving about 390 W at 0.2 AU.
Coatings can be used to reduce the absorption (to 0.2
for gold coating), though another option is to make
the primary absorbing to reduce the thermal effects later
in the optical system. Various options are under consid-
eration. However, running the mirror at 61 �C, with a
fixed radiator temperature of 50 �C, with a SiC mirror(absoptivity 0.1), the total radiator area required is
0.19 m2, i.e., 0.43 m · 0.43 m. However, this is a preli-
minary estimate, used as an example, and it does not in-
clude the radiator area for the APS detector. It does not
include, also, any consideration of the thermal interface
to the spacecraft. If the radiator sees radiation from the
back of the spacecraft heat-shield, for example, the radi-
ator size must increase. However, this estimate does sug-gest that the radiator size will be feasible, that is, within
the footprint of the instrument.
These estimates are for the situation at 0.2 AU. How-
ever, the thermal input varies considerably over the 149
day orbit – by a factor of 16. This can produce large
temperature variations over the orbit. To cope with this,
a combination of heat-switches, heaters and heat-pipes
are being considered. However, we note that, accordingto the Solar Orbiter mission concept, the instrument will
not run its prime scientific operation outside the solar
R.A. Harrison / Advances in Space Research 36 (2005) 1415–1421 1419
encounter (30 day) periods, so it is not necessary to
strive to attain perfect optical alignment during the aph-
elion periods. Some flexing of the instrument is antici-
pated, with the best optical performance geared to the
solar encounter periods.
6. Other issues
The total allocated mass, at 25 kg, is light compared
to similar instruments in operation. For example, the
SOHO CDS instrument has a mass of 100 kg. However,
CDS is a double spectrometer with an aluminium alloy
structure, 5 individual detector systems and an indepen-dent pointing system. The spectrometer under discus-
sion here will be a single spectrometer, with a smaller
structure, made of carbon fibre, with SiC optics, one
detector system and no independent pointing system.
The Solar-B EIS instrument (Culhane et al., 2002) under
development for the Solar-B mission weighs in at 60 kg,
but is 3 m long. Thus, a mass under 30 kg for a modern
instrument 1.0–1.5 m in length appears to be a chal-lenge, but within the realms of possibility.
Preliminary mass calculations have indicated masses
of 25–30 kg but some refinement of the design and opti-
misation of the structural concept have yet to be com-
pleted. Basic decisions such as the inclusion of an
image stabilisation system need to be made.
The nominal telemetry rate for the Orbiter spectrom-
eter is 17 kbit/s. If we assume a detector image of4k · 4k pixels, at 12 bits per pixel, it will take 197 min
to read one exposure. Since each exposure will form part
of a rastered image, the raster cadence will be signifi-
cantly longer. These sobering figures stress the extreme
problem facing such instruments. The situation is better
for the 2k · 2k array, but it is still a major problem.
However, this is not a new problem.
Studies from instruments such as CDS have shownthat careful line selection is far more important than
data compression in managing the data return of such
a spectrometer. Much of the spectrum is not required.
Indeed, for specific studies, specific emission lines are re-
quired. A good rule of thumb from SOHO is that a
selection of between 6 and 15 lines is good for most sci-
entific purposes.
Let us assume a resolving element of 1.0 arcsec alonga 2k pixel slit and a nominal spectral resolution of order
0.02 A/pixel. To obtain full line widths for million K
lines, plus sufficient nearby background, one would
want to return about 0.3 A, i.e., 15 pixels. Thus, to re-
turn data for 6 emission lines along the full length of
the slit would take 127 s. Assuming a factor of 3 com-
pression, and a rastered image of 50 mirror locations,
and taking 50 pixels along the slit, to produce a final ras-ter sequence of 50 arcsec · 50 arcsec, the raster cadence
would become 2.6 min.
Such basic calculations show that with careful selec-
tion and compression, and some flexibility in the meth-
ods for selection and compression, we can achieve
reasonable data return rates. It does stress the need for
careful planning in terms of line selection and target
selection. Much depends on the particular study in ques-tion; some applications require long exposures and slow
cadences and some require rapid data return. In general,
for the latter we must use small area rasters and few
lines.
However, for many studies, we do need to consider
methods for improving the performance to avoid com-
promising the scientific return. Several options are pos-
sible, including:
� Increasing the telemetry rate: This option should be
sought from the Project in any case because the
telemetry rates are calculated on assumptions on
on-board memory (240 Gbit) and ground station sup-
port (one ground station) which were made two years
ago.
� Returning line profile parameters rather than the fullprofile information.
� Returning image differences rather than full images.
These are just three options, the first one of which is
beyond the control of the instrument study team!
Given our plan to achieve 1.0 arcsec resolution ele-
ments, we must consider the inclusion of an image sta-
bilisation system. The need for this will be dictated bythe final spacecraft stability performance. We anticipate
a stability performance which will make the inclusion of
such a system a marginal requirement. An on-board sys-
tem has been discussed with the assumption that image
pointing information be made available from the high
resolution VIM instrument and the primary mirror
would be tilted in response. This is akin to the image sta-
bilisation system used on the TRACE spacecraft. An-other option under careful consideration is to not
include an image stabilisation system at all, assuming
that the variations of the spacecraft stability occur on
timescales much less than the exposure time of the spec-
trometer and thus any corrections could be done on the
ground. Such an after-the-event correction saves mass
and has been used in small-scale event analyses quite
successfully for the SOHO CDS instrument.For the present, the latter is assumed, but both op-
tions must remain open.
EUV optical surfaces in space are renowned for expe-
riencing significant degradation in performance with
time. Under high irradiation, particularly in the ultravio-
let, any contaminant deposited on an optical surface, even
in veryminute amounts, polymerizes, so the reflectivity of
the surface drastically decreases. This effect is well knownfor synchrotron radiation optics as well as for some space
instruments, but has been well avoided by the SOHO
1420 R.A. Harrison / Advances in Space Research 36 (2005) 1415–1421
EUV/UV instruments. The degree to which the reflectiv-
ity decreases depends on the irradiation exposure and
on the partial pressure of the contaminant.
However, for Solar Orbiter the situation is more dif-
ficult than it was for SOHO; due to the changing dis-
tance from the Sun, the level of UV irradiation will behigher and the thermal environment more variable.
Even with the most stringent procedures in the han-
dling and assembling of the optical components, under
the extreme irradiation conditions at 0.2 AU, there is a
risk of a serious rapid degradation of the reflectivity, espe-
cially in the EUV. The variable thermal environment dur-
ing the orbit makes evaporation and out-gassing from
surfaces with increasing temperature unavoidable.The decreasing reflectivity could be severe for optics at
normal incidence, where the EUV reflectivity is relatively
low and the EUV absorption is high. For example, gold
could be a good candidate as an EUV coating for mirrors
at normal incidence, since it has high visible reflectivity
and also discrete EUV reflectivity, but a thin layer of con-
taminants deposited on its surface could drastically re-
duce the EUV response, and thus the effective area.It should be noted that the mirrors can be operated at
relatively high temperature and this could help to reduce
the deposition of contaminants.
It should be noted, also, that steps can be taken to re-
duce the levels of potential contamination, in space. The
most important procedure would be a long out-gassing
period prior to opening the instrument door. For the
CDS and SUMER instruments on SOHO, the out-gas-sing period was 3 months from launch, and this was a
deliberate (and successful) policy. With the inclusion
of vents allowing out-gassing materials to escape, the
long period certainly enabled the contamination to be
reduced. Such a policy must be adopted for Solar Orbi-
ter – possibly for several instruments. For efficient vent-
ing, the opening to space must be large (e.g., a partly
opened aperture door, a door specifically designed forventing, or a permanent vent) and, in addition, the
instrument interior must be preferentially heated (by
passive or active heating).
Any EUV instrumentation must be developed with
the most stringent contamination policy, both in the lab-
oratory and in operation (e.g., the out-gassing men-
tioned above). Possible effects must be assessed
thoroughly by the proposing teams and optical and pro-cedural policies adopted.
7. Operation
The spectrometer instrument requires to be Sun
pointed. It will be hard-mounted, along with the other
remote sensing instruments. The required co-alignmentaccuracy between instruments is 2 arcmin, based on
attaining a reasonable image overlap with the smallest
instrument field of view. In addition, in operation, a
pointing accuracy of 2 arcmin is required. Fine pointing
within the field of view of the instrument can be
achieved using the mirror mechanism.
Operations will be performed in pre-planned se-
quences stored, time-tagged in a deferred commandstore. The operations for an entire encounter (30 days)
should be stored in this way. The sequences will have
been selected during the period preceding the solar
encounter. The planning and the selection of sequences
will be done in concert with the other remote-sensing
instruments. Indeed, target selection and pointing will
be done as one instrument.
During the non-solar encounter periods of the orbit(the period outside the 30 days observation) the stored
observational data will be telemetered to the ground.
However, it would be highly desirable, if not essential,
to practice encounter observations – even with consider-
ably reduced telemetry – much as planetary encounter
missions do, during the non-encounter parts of the or-
bit. In addition, any telemetry allocation, however
low, for some modest synoptic observations during therest of the orbit would be desirable.
8. Final remarks
This report is necessarily both preliminary and vague.
Many decisions need to be taken before the spacecraft
and mission concept is refined, and this influences theinstrument design. Some areas of instrument develop-
ment require technical development, the outcome of
which will be exploited to the full, and we can only
anticipate the outcome of study work at this time. Even
the scientific requirements are under discussion at this
stage. However, Solar orbiter is an approved mission
and the aim is to lay the foundation for the inclusion
of an EUV spectrometer which builds upon our experi-ence gained with the SOHO mission. The instrument de-
scribed here is both innovative (for example, in the use
of APS detectors and VLS gratings) and sufficiently ro-
bust and basic, as required for a mission with such an
array of technical challenges.
References
Culhane, J.L., Doschek, G.A., Watanabe, T., Lang, J., The EUV
imaging spectrometer and its role in the Solar-B mission, in:
Pauluhn, A., Huber, M.C.E., von Steiger, R. (Eds.), The Radio-
metric Calibration of SOHO. ISSI Scientific Report, SR-002, ISSN
1608-280X.
Domingo, V., Fleck, B., Poland, A.I. The SOHO mission: an overview.
Solar Phys. 162, 1, 1995.
Harrison, R.A., Vial, J.-C., Solar Orbiter EUV/UV wavelength
selection and instrumentation, in: Proceedings of the Solar
Encounter: The First Solar Orbiter workshop, ESA SP-493, p.
151, 2001.
R.A. Harrison / Advances in Space Research 36 (2005) 1415–1421 1421
Harrison, R.A., Sawyer, E.C., Carter, M.K., et al. The Coronal
Diagnostic Spectrometer for the solar and heliospheric observa-
tory. Solar Phys. 162, 233, 1995.
Marsch, E., Antonucci, E., Bochsler, P., Bougeret, J.-L., Fleck, B.,
Harrison, R.A., Marsden, R., Schwenn, R., Vial, J.-C. Solar
orbiter, a high-resolution mission to the Sun and inner heliosphere,
in: Recent insights into the physics of the Sun and heliosphere, IAU
Symposium, vol. 203, p. 565, 2001.
Prydderch, M., Waltham, N.R., Morrissey, Q., Turchetta, R., Pool, P.
A large area CMOS monolithic active pixel sensor for extreme UV
spectroscopy and imaging, Proc. SPIE 5301, 175, 2004.
Shimizu, T. Solar-B. Adv. Space Res. 29 (12), 2009, 2002.
Thomas, R.J. Toroidal varied line-space (TVLS) gratings, Proc. SPIE
4853, 411, 2003.
Wilhelm, K., Curdt, W., Marsch SUMER – Solar Ultraviolet
Measurements of Emitted Radiation. Solar Phys. 162, 189, 1995.