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Science Results Enabled by SDSS AstrometricObservations
Zeljko Ivezic1, Mario Juric2, Nick Bond2,Jeff Munn3, Robert Lupton2, et al.
1 University of Washington2Princeton University
3 USNO Flagstaff
Astrometry in the Age of the Next Generation of Large TelescopesFlagstaff, Oct 17-20, 2004
1
SDSS Astrometric Data Quality
1. Pipeline astrom developed by USNO (Pier et al. 2003)
2. Dynamic range: 14 < V < 22.5, exposure 54 sec, 5 bands
(ugriz) over 5 minutes
3. Absolute accuracy: < 50 mas
4. Relative band-to-band accuracy: ∼30 mas for sources not
limited by photon statistics, and ∼100 mas at the survey
limit
5. SDSS DR3: 141 million unique objects
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Science Results Based on SDSS AstrometricData
1. Solar System Objects: move during 5 minutes
2. Stellar Proper Motions:
• SDSS-POSS: 50 yrs baseline, g < 20, proper motion errors∼3 mas/yr
• SDSS-SDSS: 5 yrs baseline, g < 22, proper motion errors∼6 mas/yr
3. Stellar Parallaxes: ∼100 deg2, out to ∼10 pc, advantage offaint flux limit
4. Optical identifications for sources detected at other wave-lengths (FIRST, Chandra, 2MASS)
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SDSS Asteroid Observations
Moving objects in Solar System can be efficiently detected out to
∼ 20 AU even in a single scan: 5 minutes between the exposures
in the r and g bands
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Asteroids move during 5 minutes and thus appear to have pecu-
liar colors.
The images map the i-r-g filters to RGB. The data is taken in
the order riuzg, i.e. GR··B
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SDSS Asteroid Observations
• Moving objects must be efficiently found to prevent the con-
tamination of quasar candidates (and other objects with non-
stellar colors)
• Detected as moving objects with a baseline of only 5 minutes
• The sample completeness is 90%, with a contamination of 3%,
to a magnitudes fainter completeness limit than available before
• The velocity errors 2-10%, sufficient for recovery within a few
weeks
• Accurate (∼0.02 mag) 5-band photometry
• SDSS Moving Object Catalog is public at www.sdss.org
Detected 204,305 moving objects, 67,637 are identified with
known objects in Bowell’s catalog, 43,329 are unique
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Asteroid Counts
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Main SDSS Asteroid Results
• The size distribution for main-belt asteroids: measured
to a significantly smaller size limit (< 1 km) than possible
before, discovery of a change of slope at D ∼ 5 km, a smaller
number of asteroids compared to previous work by a factor
of ∼2 (N(D>1km) ∼0.75 million)
• Strong correlation between colors and position/dynamics:
Confirmation of color gradient: rocky S-type in the inner belt
vs. carbonaceous C type asteroids in the outer belt; dynam-
ical families have distinctive colors;
• Colors are correlated with the family age: space weath-
ering
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1010
1011
1012
Farinella et al. 92 (1)Farinella et al. 92 (2)Farinella et al. 92 (3)Farinella et al. 92 (4) Galileo teamDavis et al. 94Durda et al 98. ModelSAM99 ModelSDSS 2001
<----
- LARGE SIZEBUMP
<----
SMALL SIZEBUMP
D (km)
CU
MU
LAT
IVE
NU
MB
ER
> D
COMPARISON OF ASTEROID SIZE DISTR� IBUTION: OBSERVATIONS AND MODELS
The asteroid size distribution (Davis 2002, in Asteroids III).
SDSS results:1) Extended the observed range to ∼300m2) Detected the second break at ∼5 km
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The semi-major axis v. (proper) inclination for known asteroids
from Bowell’s catalog that were observed by SDSS
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The semi-major axis v. (proper) inclination for known asteroids
color-coded using measured SDSS colors
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The osculating inclination vs. semi-major axis diagram.
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What is the meaning of different color shades?
• Chemistry, of course, for the gross differences (red vs. blue),
but what about different shades of red?
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Age (Years)
Col
our
Iannini
Karin
Brangane
Agnia
Massalia
Merxia
Gefion
Rafita
Eos
Koronis
Eunomia
Maria
Sol
ar S
yste
m
0.25
0.3
0.35
0.4
0.45
0.5
0.55
0.6
0.65
10 10 10 107 8 9 10
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What is the meaning of different color shades?
• Chemistry, of course, for the gross differences (red vs. blue)
• Within a given chemical class, colors also depend on age:
SDSS colors can be used to date asteroids
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Prospects for Proper Motion Studies
• SDSS-POSS proper motions limited by the POSS astromet-ric accuracy (0.15 arcsec) resulting in proper motion accu-racy of ∼3 mas/yr; usable to g ∼ 20 (recalibrated POSSastrometry by Munn et al.)
• SDSS-SDSS proper motions with 5 years baseline accurateto ∼6 mas/yr (using only 2 epochs); usable to g ∼ 22
• SDSS-LSST proper motions will be limited by the SDSSastrometric accuracy (∼30 mas): with 15 years baselineaccurate to ∼2 mas/yr This is >100 times more sensitivethan Luyten’s catalog (a standard resource for proper mo-tion studies)!
SDSS (and especially LSST) may revolutionize proper motionbased studies of the Galactic structure (2 mas/yr correspondsto 10 km/s at 1 kpc)!
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Photometrically and Astrometrically Variable Ob-
jects
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Tangential VelocityDistributions for M dwarfs
(D<1 kpc)• Top row: l=0, b∼45, vl and vb
for D=300 pc
• Middle row: l=90, b∼45, vl for
D=300 pc and D=800 pc
• Bottom row: l=180, D=300 pc,
vl for b∼45 and b∼-45
• Note strong non-Gaussianity:
asymmetric drift
• The main advantage of SDSS-
POSS sample: probes larger dis-
tances than possible before, ac-
curate distance estimates, large
number of sources: enormous
amount of detailed information!
21
Thick Disk vs. Halo VelocityDistributions
• Top: vb, bottom: vl
• Turn-off stars selected in r vs.
g − r color diagram: black
• Further separated by u − g color
(metallicity proxy) into “halo”
(blue) and “thick disk” (red)
stars
• Note the strong lag
• Note strong non-Gaussianity:
asymmetric drift
• The main advantage of SDSS-
POSS sample: probes larger dis-
tances than possible before, ac-
curate distance estimates, large
number of sources: enormous
amount of detailed information!
22
Conclusions
• It’s good to have accurate astrometry for a lot of faint
sources across a large chunk of the sky.
23
Conclusions
• It’s good to have accurate astrometry for a lot of faint
sources across a large chunk of the sky.
• Especially when accurate multi-band photometry is also avail-
able.
24
Conclusions
• It’s good to have accurate astrometry for a lot of faint
sources across a large chunk of the sky.
• Especially when accurate multi-band photometry is also avail-
able.
• And radial velocities, and variability information, and . . .
25