Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory
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Головна астрономічна обсерваторія НАН України
2003
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irk-123456789-785962015-03-20T03:02:27Z Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory Jockers, K. Plenary Sessions 2003 Article Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory / K. Jockers // Кинематика и физика небесных тел. — 2003. — Т. 19, № 4-додаток. — С. 36-42. — Бібліогр.: 4 назв. — англ. 0233-7665 http://dspace.nbuv.gov.ua/handle/123456789/78596 en Кинематика и физика небесных тел Головна астрономічна обсерваторія НАН України |
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Jockers, K. |
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Jockers, K. |
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Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory |
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Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory |
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Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory |
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Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory |
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Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory |
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six years of observing with the two-channel focal reducer of mpae at the terskol observatory |
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Головна астрономічна обсерваторія НАН України |
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2003 |
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Plenary Sessions |
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Six years of observing with the Two-Channel Focal Reducer of MPAe at the Terskol Observatory / K. Jockers // Кинематика и физика небесных тел. — 2003. — Т. 19, № 4-додаток. — С. 36-42. — Бібліогр.: 4 назв. — англ. |
series |
Кинематика и физика небесных тел |
work_keys_str_mv |
AT jockersk sixyearsofobservingwiththetwochannelfocalreducerofmpaeattheterskolobservatory |
first_indexed |
2025-07-06T02:41:55Z |
last_indexed |
2025-07-06T02:41:55Z |
_version_ |
1836863681875410944 |
fulltext |
Figure 1. Two-
olor image of
omet C/1995 O1 (Hale-Bopp) obtained with the Two-Channel Fo
al Redu
eron April 13, 1997. The orange
olor represents the dust grains of the
ometary atmosphere. Note the dustspirals observed in this huge
omet. The blue
olor represents the distribution of
ometary ions (here the ionOH+) [1℄
31
-M
ar
-9
7
Color Polarization Pol. Color
Comet C/1995 O1 (Hale-Bopp)
max.
min.
30000 kmto SunFigure 2. Images of
olor, polarization, and polarimetri
olor as observed in
omet C/1995 O1 (Hale-Bopp)on Mar
h 31, 1997. The displayed range of dust
olor extends from 0% to 30% reddening per 1000 �A. The po-larization range is from 12% to 20%. The polarimetri
olor Pred � Pblue, measured at 642 and 443 nm, rangesfrom 1% to 5%
36
SIX YEARS OF OBSERVING WITH THE TWO-CHANNEL FOCALREDUCER OF MPAE AT THE TERSKOL OBSERVATORYK. Jo
kers
2003Max-Plan
k-Institut f�ur AeronomieD-37191 Katlenburg-Lindau, Germanye-mail: jo
kers�linmpi.mpg.deØÅÑÒÜ ËÅÒ ÍÀÁËÞÄÅÍÈÉ Ñ ÄÂÓÕÊÀÍÀËÜÍÛÌ ÔÎÊÀËÜÍÛÌ �ÅÄÓÊÒÎ�ÎÌÈÍÑÒÈÒÓÒÀ ÀÝ�ÎÍÎÌÈÈÌ. ÏËÀÍÊÀ ÍÀ ÎÁÑÅ�ÂÀÒÎ�ÈÈ ÒÅ�ÑÊÎË, Éîêêåðñ Ê. � 1996 ã. íà ïèê Òåðñêîë áûë äîñòàâëåí äâóõêàíàëüíûé �îêàëüíûé ðåäóêòîð Èíñòèòóòààýðîíîìèè Ì. Ïëàíêà äëÿ èñïîëüçîâàíèÿ íà 2-ì òåëåñêîïå ñèñòåìû �è÷è�Êðåòüåíà�Êóäý.Ýòîò ïðèáîð ÿâëÿåòñÿ åäèíñòâåííûì íà ýòîì òåëåñêîïå óñòðîéñòâîì ïîëó÷åíèÿ ýëåêòðîííîãîèçîáðàæåíèÿ. Èñïîëüçóÿ êîìïëåêñ �2-ì òåëåñêîï�2-êàíàëüíûé �îêàëüíûé ðåäóêòîð�, ó÷åíûå�åðìàíèè â ñîòðóäíè÷åñòâå ñ ðóññêèìè, óêðàèíñêèìè è áîëãàðñêèìè àñòðîíîìàìè çàíèìàëèñüèçó÷åíèåì ãàçà è ïûëè â êîìåòàõ, ïðîâîäèëè ïîëÿðèìåòðèþ àñòåðîèäîâ è êîìåòíîãî ãàçà, àòàêæå âûïîëíÿëè ðàáîòû ïî àñòðîìåòðèè è �îòîìåòðèè âíóòðåííèõ ñïóòíèêîâ Þïèòåðà.Êðîìå òîãî, èññëåäîâàëèñü ìîð�îëîãèÿ è ñâåòèìîñòü ïëàçìåííîãî òîðà ñïóòíèêà ÞïèòåðàÈî ñ öåëüþ îïðåäåëåíèÿ åãî �èçè÷åñêèõ õàðàêòåðèñòèê.  äîêëàäå äàåòñÿ êðàòêîå îïèñà-íèå �îêàëüíîãî ðåäóêòîðà, âîçìîæíîñòè êîìïëåêñà �2-ì òåëåñêîï�2-êàíàëüíûé �îêàëüíûéðåäóêòîð� äåìîíñòðèðóþòñÿ íà ðåçóëüòàòàõ 6-ëåòíåãî ïåðèîäà íàáëþäåíèé.In 1996 the Two-Channel Fo
al Redu
er of the Max-Plan
k-Institut f�ur Aeronomie was brought toTerskol Peak for the use at the 2-m Zeiss Rit
hey-Chr�etien-Coud�e teles
ope. Sin
e then it has beenthe only ele
troni
imaging devi
e available at this teles
ope. Using the 2-m teles
ope, the Germanside, in
ollaboration with Russian, Ukrainian and Bulgarian astronomers, has studied gas and dustin
omets,
ondu
ted polarimetry of
ometary dust and asteroids, and astrometry and photometryof the inner Jovian satellites. The morphology and brightness of the plasma torus of the Joviansatellite Io has been investigated in order to derive its physi
al properties. The fo
al redu
er isbriefly des
ribed, and the
apabilities of the teles
ope�fo
al redu
er
ombination are demonstratedwith results obtained during the six years of observing.INTRODUCTIONIn 1996 the Max-Plan
k-Institut fur Aeronomie (MPAe) and the International Centre for Astronomi
al,Medi
al and E
ologi
al Resear
h (ICAMER) have agreed on the joint use of the Two-Channel Fo
alRedu
er of MPAe at the 2-m RCC Zeiss teles
ope of ICAMER. Sin
e then six years have passed by.On o
asion of the 10th anniversary of the foundation of ICAMER a brief overview of the resultsa
hieved by the German side within the framework of the above agreement is presented below.THE TWO-CHANNEL FOCAL REDUCER AT THE 2-m RCC ZEISS TELESCOPEOF THE TERSKOL OBSERVATORYThe primary aim of teles
opi
astronomi
al observations is to get a
lose-up view on a
elestial obje
t.One, therefore, might think that magnifying power, or, if we speak in terms of photography, fo
al lengthis the primary �gure of merit for an astronomi
al teles
ope or, more a
urately, for the
ombinationof a teles
ope with a modern solid state
amera employing CCD dete
tors. There are two mainreasons why this is not the
ase. First, a teles
ope represents a \light bu
ket", i.e., must
olle
t asmany photons as possible. The larger the diameter of its primary mirror the more light of a feebleastronomi
al obje
t is
olle
ted and, for a given magni�
ation, the less time it will take to obtaina de
ent image of the obje
t. On the other hand, the more light enters the teles
ope, if the exposuretime is �xed, the larger
an be the magni�
ation of the image we want to get. The se
ond fa
tor limitingthe magni�
ation of a large opti
al ground-based teles
ope is atmospheri
turbulen
e. Even withthe sometimes ex
ellent atmospheri
onditions at the Terskol Observatory atmospheri
turbulen
edoes not allow to get a resolution mu
h better than 1/20000 of a degree, i.e., 0.18 ar
se
. To optimizethe s
ar
e and expensive observing time available at large teles
opes it is, therefore, important to37
adjust the fo
al length of a given teles
ope to the task of the observations. In its Cassegrain fo
usthe 2-m RCC teles
ope of the Terskol Observatory has a fo
al length optimized to the best
onditionsof atmospheri
turbulen
e. The Two-Channel Fo
al Redu
er of MPAe [2℄ redu
es this fo
al lengthby a fa
tor of 2.86 to a resolution of about 1 ar
se
. This allows to obtain sharp images even undernon-optimum
onditions of atmospheri
turbulen
e. At the same time the light gathering powerin
reases by the square of the same fa
tor (2.862 = 8.2), i.e., less time is needed to get a well-exposedimage. As an additional feature the fo
al redu
er has two
hannels to allow simultaneous images intwo
olors. In this respe
t the instrument falls short of an ordinary television
amera whi
h has three
olor
hannels. But in
omparison with a television
amera, whi
h is restri
ted to the natural
olorsof the human eye, the fo
al redu
er allows �lters of wide or narrow bandwidth to be used. In thisway the astronomi
al obje
ts
an be observed in the light of important atoms, mole
ules or ions, orin windows free from su
h lines (
ontinuum windows), as ne
essary for the investigated obje
t.GAS AND DUST IN COMETSA
omet is a \dirty snowball" of a size of about one kilometer. A
ording to present understand-ing
omets were formed from the protoplanetary dust
loud about 4.6 billion years ago at aboutthe distan
e of present-day planet Neptun. During this long time almost all
omets remained at largedistan
es from the Sun and have always been very
old. Therefore, in
ontrast to the inner, earthlikeplanets,
omets preserved the volatile materials of the early solar system whi
h were lost or modi�edin the inner solar system where the earthlike planets formed. Despite of most
omets being unobserv-able in the deep voids of the solar system, some are s
attered by disturban
es of planets or stars intothe inner solar system. When they approa
h the Sun their surfa
e temperature in
reases and theysublimate their volatile materials (i
es). The dust grains (the \dirt" of the dirty snowball) are draggedalong with the gases and form the so-
alled dust
oma and dust tail of a
omet. The gas mole
ulesof the sublimated i
es form the gas
oma. They are later ionized, intera
t with the solar wind andform the
ometary ion tail. Despite of the small
ometary nu
leus, whi
h
annot be resolved withground-based teles
opes, the
oma and in parti
ular the dust and ion tails
an have a size of manymillion km and be observed not only in teles
opes but also with naked eye. Comet Hale-Bopp wasone of these naked-eye obje
ts in spring 1997. In Figure 1 (see page 36) two simultaneous images ofthis
omet, taken with the Two-Channel Fo
al Redu
er, have been
ombined into a single two-
olorimage. The blue, stru
tured envelopes in the image are representing the
ometary ion tail. The ar
sform through intera
tion with the solar wind. The yellow oval in the image is
ometary dust. A dustspiral is visible. Dust grains with spe
ial properties leave a
tive areas of the
ometary nu
leus and aredragged into a spiral by the rotation of the nu
leus.We
an obtain more information about the dust of
omet Hale-Bopp, if besides of investigatingdust images we also determine dust
olor (
hange of dust brightness with wavelength) and polarization.Images of dust
olor, polarization and \polarimetri
olor", i.e., the wavelength dependen
e of pola-rization, are shown in Figure 2 (see page 36). The bluer
olor and redu
ed polarization at the
omet's
enter as
ompared to its surroundings has been interpreted as a slow evaporation of a
ompa
t organi
mantle from a sili
ate
ore of the dust grains as the parti
les leave the
ool nu
leus surfa
e and areheated by solar radiation [3℄.POLARIMETRY OF ASTEROIDSAsteroids are small bodies in the inner solar system. Most of them orbit the Sun between the planetsMars and Jupiter. They are thought to be left-overs from the small body population (\planetesimals")from whi
h the planets are built. When giant planet Jupiter formed, its gravity in
reased the relativevelo
ities of neighbouring planetesimals. As a
onsequen
e, instead of
oales
ing and forming anotherplanet, they started to destru
t ea
h other. There is eviden
e for great
ollisions between asteroids.Their present-day population is said to be in
ollisional equilibrium, i.e., as a result of
ollisionssmaller and smaller fragments are
onstantly being formed. These fragments orbit not only betweenMars and Jupiter but some of them approa
h the earth quite
losely. One of these obje
ts is asteroid33342 whi
h, like most
ometary nu
lei, has a size of about 1 km and approa
hed the earth in Mid-De
ember 2001 to 0.0125 AU. A
ampaign was organized in order to measure the polarization ofthis obje
t over a wide range of phase angles (angle Sun-obje
t-Earth). Data were obtained fromthe Crimean Astrophysi
al Observatory, the Grakovo station of Kharkov University Observatory and,last not least, from Terskol Peak. The 2-m teles
ope was used when the asteroid was still faint.38
Figure 3. Degree of polarization versus phase angle as observed in asteroid 33342 from several
ooperatingobservatoriesThe results (see Fig. 3) indi
ate that the asteroid is of the rare E type (metalli
type) with very lowpolarization. This will help to interpret other data of this asteroid, like, e.g., the �rst radar dataobtained with the help of the Crimean Evpatoria radar.THE INNER JOVIAN SATELLITESThe four large satellites of Jupiter, Io, Europa, Ganymede and Callisto, dis
overed by Galileo, werethe �rst obje
ts known to revolve around another
elestial body di�erent from Earth or Sun. Insidethe innermost of the Galilean satellites, Io, whi
h is at a distan
e of 5.905 Jovian radii from Jupiter's
enter, are the inner satellites Thebe, Amalthea, Adrasthea and Metis with semimajor axes of 3.11,2.54, 1.81 and 1.79 Jovian radii and mean radii of 49.3, 83.5, 8.2 and 21.5 km, respe
tively. The largestone, Amalthea, was dis
overed by Barnard in 1892. The other three were dete
ted only duringthe Voyager mission 1979/80. For ground-based observations they are, like the Jovian ring, normallyhidden in the glare of the bright disk of Jupiter. In the last years we have been able to observethem routinely. This is possible partly be
ause of the ex
ellent transparen
y of the sky at the highaltitude site of Terskol Peak, partly be
ause spe
ial measures were taken. They are observed mainly inthe methane absorption band at 890 nm, where the disk of Jupiter is
omparatively dark. In addition,like in a
oronograph, a Lyot-stop suppresses the di�ra
tion pattern of Jupiter
aused by the teles
opeopti
s. An elaborate mask at Cassegrain fo
us
onsisting of bla
k glasses of di�erent thi
kness andabsorptivity suppresses the light of Jupiter and of the Galilean satellites, but nevertheless allows theirimaging together with the faint inner satellites. This is very important as the images of the innersatellites must be related to
alibration obje
ts. The remaining halo of s
attered light from Jupiter
an be determined from the images and is subtra
ted during data redu
tion. Sample images areshown in Fig. 4. Observation of the positions of the inner satellites relative to those of the Galileanones has allowed to get their a
urate astrometri
positions, whi
h are needed to
orre
t the orbitpredi
tions for these obje
ts [4℄. The inner Jovian satellites are under heavy bombardment by energeti
parti
les of the Jovian magnetosphere. Dust parti
les are sputtered from the satellite surfa
es andare the sour
e for the Jovian ring. To get more information on the nature of the satellite surfa
eswe have obtained integral photometry of the satellites. In
ontrast to the existing spa
e observationsour observations refer to small phase angles. Observations at very small angles provide the mostuseful information about the physi
al stru
ture and texture of the surfa
e layer of the satellite. Dueto adverse weather
onditions, the minimum angle so far observed is 1.42Æ. The maximum phaseangle was 8.16Æ. The obtained photometri
data allow to measure separately the brightness of bothhemispheres with respe
t to the orbital motion of the satellite, i.e., the brightness of the leading andtrailing hemispheres. This investigation may help to understand better the
hara
ter of the intera
tionbetween the satellites and the Jovian magnetosphere. For all satellites the leading hemispheres arebrighter than the trailing ones, despite of the fa
t that the orbital periods of Thebe and Amalthea39
Figure 4. The inner Jovian satellites revealed. The satellite Ganymed is behind a weakly absorbing bla
k glass,and planet Jupiter itself behind a strongly absorbing glassare larger than Jupiter's rotation period, i.e., the magneti
ally bound energeti
parti
les hit thesesatellites on their trailing side, while for Metis the orbital period is smaller, i.e., the parti
les impingeon its leading side. The albedos of Amalthea, Thebe and Metis de
rease with their orbital distan
efrom Jupiter.THE IO TORUSAnother elusive obje
t in Jupiter's satellite system is the Io torus. The innermost Galilean satelliteIo is heated by gravitational intera
tion with Jupiter and the other Galilean moons. This
ausesits vol
ani
a
tivity. Most of its surfa
e is
overed by SO2 frost and there is also a very thin SO2atmosphere. The satellite Io orbits in the Jovian magnetosphere, a vast region of
orotating ionized40
Figure 5. The Io torus, imaged in the forbidden lines of S+ ([S II℄) and S++ ([S III℄)gas. This magnetospheri
plasma disso
iates the SO2 mole
ules, ionizes them, for
es them to rotatearound Jupiter and in this way forms the Io torus. As the magneti
dipole of Jupiter is tilted byabout 10Æ with respe
t to Jupiter's rotation axis, the Io torus is tilted in a similar way. The sulphurand oxygen ions of the Io torus radiate line emission. The strongest lines are due to S+ and S++.Observations of the torus in the light of these ions allow to determine the torus shape and its densityand temperature. Observations of the Io torus are about as diÆ
ult as the observations of the innersatellites, for the same reason of s
attered light from the bright Jovian disk. A similar setup is usedas for the inner moons. In addition, a tunable Fabry-Perot interferometer allows only a very narrowrange of wavelengths around the wavelength of the observed ion to be imaged and in this way furthersuppresses the straylight of Jupiter. Imaging of the Io torus allows to \see" part of the otherwiseinvisible Jovian magnetosphere and to determine its ele
tron density and temperature. In 1999 and2000 Jupiter's magnetosphere was investigated by the Galileo spa
e probe, and the observations ofthe torus
ondu
ted at Terskol Peak served as a supplement of the spa
e probe measurements. Fig. 5shows images of the torus from November 2000 in the light of the S+ and S++ ions. Dawn and duskare the morning and evening sides of the torus, i.e., the sides where, as seen from an observer inthe torus, the sun rises (rotational motion of the torus toward Sun) or sets (rotational motion awayfrom Sun). The ellipsoids represent the lo
ation of a ring at Io's distan
e from Jupiter in
lined asthe Io torus. An open ellipse indi
ates that we see part of an open torus. If the ellipse degenerates toa straight line, we see the torus from its side. On the left side of Fig. 5 in the third or fourth panelof the [S II℄ (S+) images we see a narrow inner ring (the
old torus) and atta
hed to it a verti
allyextended feature
alled ribbon. In the uppermost and lowermost panel of the S+ images, where wesee the torus edge-on, the ribbon
ontinues to be prominently visible. This indi
ates that it is nearlyperpendi
ular to the plane of the torus. It is
aused by warmer ions whi
h, be
ause of their highertemperature,
an move up and down along the magneti
�eld lines of Jupiter. We see from this thatthe temperature in the Io torus in
reases with distan
e from Jupiter. The [S III℄ (S++) emission
omesfrom hotter regions in the torus. In the light of this ion the
old torus is invisible. In the �rst rowof images bright areas
lose to Jupiter indi
ate straylight whi
h
ould not be properly removed fromthe images. This happens when during observations a small
loud passed through the �eld of view ofthe teles
ope. A remarkable feature is the separation of
old torus and ribbon whi
h is best visible41
in the third panel of [S II℄ (S+) images. It is not
lear what
aused this gap. It was not observed in1999, i.e., in 1999 there was a
ontinuous transition between
old torus and ribbon.OUTLOOKFor many years the Large Azimuthal Teles
ope (BTA) of the Spe
ial Astronomi
al Observatory with its6m mirror has been the largest teles
ope of the world. In re
ent years, based on the design of the BTAand improving it, a number of larger teles
opes have been built and more of these huge teles
opesare under
onstru
tion. In this new era 2m size teles
opes are
onsidered as survey teles
opes to�nd the obje
ts whi
h then will be investigated more deeply with the huge teles
opes. A properway of operation is provided in the framework of a \virtual observatory", where survey data aremade available to all astronomers for use in their di�erent �elds. Another way to
ompete withthe huge teles
opes has been to spe
ialize on obje
ts whi
h are bright enough to be observable withmedium-sized teles
opes but whi
h nevertheless have not been studied extensively. As demonstratedin this study small bodies of the solar system are suitable obje
ts partly be
ause of their temporalvariability and partly be
ause they require spe
ial observing te
hniques not always available at the hugeteles
opes. In our
ooperative program the 2-m RCC Zeiss teles
ope of the Terskol Observatory hasprodu
ed internationally
ompetitive results, and it
an do this not only in the �eld of solar systemastronomy. The present author hopes, however, that sooner or later a huge Russian teles
ope will beavailable and give the East-European astronomi
al
ommunity the resear
h tool they deserve.[1℄ Jo
kers K., Bonev T., Credner T. Observations of ions in
omets: A
ontribution towards understandingthe
omet-solar wind intera
tion // Astrophys. and Spa
e S
i.{1999.{264.{P. 227{234.[2℄ Jo
kers K., Credner T., Bonev T., et al. Exploration of the solar system with the two-
hannel fo
alredu
er at the 2m-RCC teles
ope of Pik Terskol Observatory // Kinemati
s and Physi
s of CelestialBodies. Suppl. Ser, \Astronomy in Ukraine { 2000 and Beyond (Impa
t of International Cooperation)" /Ed. Ya. S. Yatskiv.{2000.{3.{P. 13{18.[3℄ Kolokolova L., Jo
kers K., Gustafson B. �A. S., Li
htenberg G. Color and polarization as indi
ators of
omet dust properties and evolution in the near-nu
leus
oma // J. Geophys. Res.{2001.{106.{P. 10113{10127.[4℄ Kulyk I., Jo
kers K., Karpov N., Sergeev A. Astrometri
CCD observations of the inner Jovian satellitesin 1999{2000 // Astron. and Astrophys.{2002.{383.{P. 724{728.
42
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