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Observational constraints from the<br />
Lecture Universität Heidelberg WS 11/12<br />
Dr. Christoph Mordasini<br />
Lecture 1 Part II<br />
Solar System<br />
and from<br />
Extrasolar Planets<br />
mordasini@mpia.de Mentor Prof. T. Henning
1. Introduction<br />
Lecture overview<br />
2. Planet formation paradigm<br />
3. Structure of the Solar System<br />
4. The surprise: 51 Peg b<br />
5. Detection techniques: radial velocity, transits,<br />
direct imaging, (microlensing, timing, astrometry)<br />
6. Properties of extrasolar <strong>planets</strong>: mass, distance,<br />
<strong>eccentric</strong>ity distributions, metallicity effect, mass-<br />
radius diagram, ...
6. Properties of extrasolar <strong>planets</strong>
692 <strong>planets</strong><br />
Current status<br />
Candidates detected by radial velocity or astrometry<br />
524 planetary systems<br />
640 <strong>planets</strong><br />
76 multiple planet systems<br />
Transiting <strong>planets</strong><br />
171 planetary systems<br />
184 <strong>planets</strong><br />
14 multiple planet systems<br />
Candidates detected by microlensing<br />
12 planetary systems<br />
13 <strong>planets</strong><br />
1 multiple planet systems<br />
Candidates detected by imaging<br />
22 planetary systems<br />
25 <strong>planets</strong><br />
1 multiple planet systems<br />
Candidates detected by timing<br />
9 planetary systems<br />
14 <strong>planets</strong><br />
4 multiple planet systems<br />
+ 1235 planet candidates from<br />
the KEPLER satellite (transit)<br />
Extra-solar planet encyclopedia (http://exoplanet.eu/)<br />
9.11.2011
Different techniques - different constraints<br />
direct imaging
A quickly progressing field<br />
•Incredible wealth of data provided by already flying space mission (e.g. CoRoT and Kepler).<br />
More to come.<br />
•Field observationally driven. Formation theory struggles to keep up... Observation and theory<br />
often don’t match well.<br />
•Common characteristic: provide observations of a large number of exo<strong>planets</strong>. This data<br />
should therefore be treated as a statistical ensemble. This could help.<br />
Venus<br />
Earth<br />
Mars<br />
Jupiter<br />
Saturn<br />
Uranus<br />
Neptune
Overview on observed exoplanet properties<br />
• Extrasolar <strong>planets</strong> exhibit a very large diversity (all techniques).<br />
• Frequencies -Low mass close-in <strong>planets</strong>: approx. 50 % (radial velocity)<br />
-Jovian <strong>planets</strong> inside a few AU: approx. 10-15 % (rv)<br />
-Hot Jupiters: 0.5-1% (rv, transits)<br />
-Cold Neptunes are common (microlensing)<br />
-Overall (FGK stars): any mass, P
Today, formation theory cannot explain all these<br />
observed characteristics in one coherent picture.<br />
But at least for some observations, theory can give us<br />
ideas about possible mechanisms responsible for them.
6.1 a-M diagram
Diversity & structures in the a-M diagram<br />
Radial velocity<br />
& Transits<br />
J. Schneider’s exoplanet.eu<br />
~2010 (already outdated!)<br />
Microlensing<br />
Direct imaging<br />
Diversity<br />
- close-in giant <strong>planets</strong><br />
- evaporating <strong>planets</strong><br />
- <strong>eccentric</strong> <strong>planets</strong><br />
- super Jupiters<br />
- Hot Neptunes & Super Earth<br />
- pile-ups and voids:<br />
planetary desert<br />
period valley<br />
- <strong>planets</strong> at large distances<br />
HARPS high<br />
precision<br />
sample 2011
Frequency of planet types<br />
Bias-corrected frequency (at least one planet per star) in the a-M (or equivalently period-mass)<br />
plane found by high precision RV around solar like FGK stars.<br />
Close in <strong>planets</strong>: P
6.2 Mass distribution
∼15 MJup, with an upper mass limit corresponding to the (vanishing) tail of<br />
mass distribution. The planet mass distribution is shown in Fig. 1 and follows<br />
wer law, dN/dM ∝ M −1.05 54), 55) affected very little by the unknown sin i. 41)<br />
paucity of companions with Msin i greater than 12 MJup confirms the presence<br />
“brown dwarf desert” 54) for companions with orbital periods up to a decade.<br />
Marcy et al. 2005<br />
Number of Planets<br />
20<br />
15<br />
10<br />
5<br />
Planet Mass Distribution<br />
dN/dM ! M −1.05<br />
104 Planets<br />
Keck, Lick, AAT<br />
0<br />
0 2 4 6 8 10 12 14<br />
M sin i (MJUP) 1. The histogram of 104 planet masses (Msin i) found in the uniform 3 m s −1 Doppler survey<br />
f 1330 stars at Lick, Keck, and the AAT telescopes. The bin size is 0.5 MJup. The distribution<br />
f planet masses rises as M −1.05 from 10 MJup down to Saturn masses, with incompleteness at<br />
ower masses.<br />
Mass distribution: old versions (giants)<br />
•mass distribution from RV observations.<br />
HARPS<br />
•rising towards smaller masses. No obs. bias: smaller masses are more difficult to detect.<br />
•beware of uncorrected (biased) distributions!<br />
•frequency of Jovian <strong>planets</strong> falls as about M -1 .<br />
•maximum of giant planet masses at about 1 Jupiter mass.<br />
•HARPS gave around 2007 the first hint of a second population of low mass <strong>planets</strong>.<br />
?<br />
Udry et al. 2007
Mass distribution II: new view (w. low masses)<br />
Mayor et al. 2011<br />
uncorrected for obs. bias corrected for obs. bias<br />
Mayor et al. 2011<br />
•RV: thanks to 1 m/s precision observations, a new huge population of low mass <strong>planets</strong><br />
has emerged in the last few years (mostly <strong>planets</strong> found by HARPS).<br />
•bi (tri?) modal distribution: minimum at about 30 Earth masses. Imprint of formation?<br />
•neptunian bump: strong increase between 30-15 ME.<br />
•overall maximum at small masses<br />
•more than 50% of solar-type stars harbor at least one planet of any mass and with<br />
period up to 100 days (!)
Grether & Lineweaver 2006<br />
Mass distribution III: upper boundary<br />
desert<br />
• less than 0.6 % of Sun-like stars have<br />
a brown-dwarf companion: so called<br />
“Brown dwarf desert”<br />
•mass distribution function shows a<br />
lack of objects between 25-45 MJ.<br />
Upper end of planet mass distribution?<br />
•Nothing particular is seen at 13 MJ (Dburning<br />
limit).<br />
Sahlmann et al. 2010<br />
Segresan et al.<br />
A distinction of BD vs. <strong>planets</strong> based on formation<br />
seems advisable, but difficult to realize in practice.
6.3 Semimajor axis distribution
ative points of view invoke in situ formation (Bodenheimer, Hubickyj & Lissauer<br />
000), possibly triggered through disk instabilities (Boss 1997, Durisen et al. 2007).<br />
ote however that, even in such cases, subsequent disk-planet interactions leading to<br />
N<br />
20<br />
15<br />
10<br />
5<br />
0<br />
Udry & Santos 2007<br />
dry· Santos<br />
Semimajor axis distribution I: giants<br />
Msini>0.75 MJ<br />
Msini
m Kepler 13<br />
Number of Planets per Star<br />
0.1000<br />
0.0100<br />
0.0010<br />
Transits<br />
P 0 = 1.7 days<br />
P 0 = 2.2 days<br />
0.0001<br />
0.68 1.2 2.0 3.4 5.9 10 17 29 50<br />
Orbital Period (days)<br />
Howard et al. 2011<br />
Semimajor axis distribution II:<br />
P 0 = 7.0 days<br />
low mass/radius <strong>planets</strong><br />
2!4 R E<br />
4!8 R E<br />
8!32 R E<br />
ig. 7.— Measured planet occurrence (filled circles) as a funcn<br />
of orbital period with best-fit models (solid curves) overlaid.<br />
ese models are power laws with exponential cutoffs belowachareristic<br />
RVperiod,<br />
P0 (see text and equation 8). P0 increases with<br />
reasing planet radius, suggesting that the migration and parkmechanism<br />
that deposits <strong>planets</strong> close-in depends on planet<br />
ius. Colors correspond to the same ranges of radii as in Figure<br />
The occurrence measurements (filled circles) are the same as in<br />
ure 6, however for clarity the 2–32 R⊕ measurements and fit<br />
excluded here. As before, only stars in the solar subset (Table<br />
and <strong>planets</strong> with Rp > 2 R⊕ were used to compute occurrence.<br />
e integrated occurrence to P = 50 days is given in<br />
ble 4.<br />
4. STELLAR EFFECTIVE TEMPERATURE<br />
4.1. Planet Occurrence<br />
n the previous section we considered only GK stars<br />
th properties consistent with those listed in Table 1.<br />
particular, only stars with Teff =4100–6100Kwere<br />
Mayor et al. 2011<br />
ed to compute planet occurrence. Here we expand this<br />
Cut off below P0:<br />
-small radii 2-4 Re: P0 = 7 days<br />
-large radii >4 Re : P0 = 2 days.<br />
Neptunian and smaller sized further out than giant <strong>planets</strong>.<br />
No pile up at 3 days. Consistent with earlier results from<br />
high precision RV. Lovis et al. 2009 estimated 10 days.<br />
Different stopping mechanism?<br />
Msini
6.4 Eccentricity distribution
Eccentricity distribution<br />
Mayor et al. 2011<br />
•high and even very high <strong>eccentric</strong>ities are common among exo<strong>planets</strong>. This is very different<br />
than in the Solar System.<br />
•mean <strong>eccentric</strong>ity for giants: 0.28 > any planet of the Solar System.<br />
•lower mass <strong>planets</strong> seem to have lower (but still quite high) e 10 MJ), dynamical interactions in a cluster
6.5 Metallicity
Mordasini et al. 2009<br />
Stellar metallicity<br />
•[Fe/H]: iron content of the star ([Fe/H]=0: solar composition, [Fe/H]=0.5: ~ 3 times more<br />
iron than the sun).<br />
•Iron serves as a proxy for the overall metal content in the star (scaled solar composition).<br />
•Stars in the the solar neighborhood have a distribution of metallicities which is roughly<br />
Gaussian around zero.<br />
•Other parts in the galaxies can have completely different [Fe/H] distributions. These stars<br />
can also have a non-scaled solar composition (e.g. thick disk stars).<br />
•There exists also a galactic metallicity gradient (higher [Fe/H] towards the center).
N. Santos et al. (2005)<br />
Metallicity effect for giant <strong>planets</strong><br />
search sample (all stars)<br />
stars with giant <strong>planets</strong><br />
•the detection probability for giant <strong>planets</strong> is a strongly increasing function of the host star<br />
metallicity.<br />
•No hot Jupiters found in globular cluster 47 Tuc ([Fe/H]=-0.76). Expected for solar neighborhood<br />
frequency (~0.5%): seven discoveries.<br />
•Best known star-planet correlation for exo<strong>planets</strong>. Important constraint for formation.<br />
•Explanation:<br />
• <strong>planets</strong> form more readily in metal rich systems (primordial hypothesis). Likely.<br />
• falling in <strong>planets</strong> have enriched the star (pollution hypothesis)
No metallicity effect for low mass <strong>planets</strong><br />
Mayor et al. 2011<br />
•HARPS high precision sample: [Fe/H] for giant gaseous <strong>planets</strong> (black), for <strong>planets</strong> less<br />
massive than 30 ME (red), and for the global combined sample stars (blue).<br />
•No metallicity effect for low mass <strong>planets</strong>.<br />
•Even absence of low mass <strong>planets</strong> at high [Fe/H]?<br />
•Natural outcome in the core accretion formation model.<br />
?<br />
?<br />
Mayor et al. 2011
Sousa et al. 2011<br />
Metallicity effect as function of mass<br />
•The division between metalophile and not<br />
metalophile <strong>planets</strong> coincides with a minimum in<br />
the planetary mass function. (ca. 30 ME)<br />
•Different populations: Giant <strong>planets</strong> (w. gas<br />
runaway accretion) vs. Neptunian <strong>planets</strong>.<br />
•Correlation with other elemental abundances in<br />
the stars are less clear (maybe Lithium-planet<br />
anticorrelation).
6.6 Stellar mass
Influence of the host star mass<br />
•Equal bin in log(Mstar)<br />
• M dwarfs<br />
• solar stars<br />
• intermediate masses<br />
•Planetary system mass / star number<br />
=> mass of planetary material scales with<br />
Mstar<br />
•Planets around more massive stars are<br />
more massive and more frequent.<br />
•RV bias underestimate the last bin.<br />
•The Neptunian vs Jovian planet ratio is<br />
higher around M dwarfs.<br />
•Consistent with a correlation of stellar<br />
mass, protoplanetary disk mass, and<br />
(giant) planet formation probability.
6.7 Multiplicity
Multiplicity<br />
•Fraction of giant <strong>planets</strong> in multiple systems: ~25%. Incomplete...<br />
•Fraction of low mass <strong>planets</strong> in multiple systems: ~70%<br />
•Hot Jupiters seem to be lonely. Formation? Disk cleaning? Kozai?<br />
•HD10180: up to 7 <strong>planets</strong> (RV)<br />
HD10180 a[AU] Msini<br />
(b) 0.02 1.4<br />
c 0.06 13.2<br />
d 0.13 11.9<br />
e 0.27 25.4<br />
f 0.49 23.6<br />
g 1.4 21.4<br />
h 3.4 65.3<br />
Lovis et al. 2011<br />
•Eccentricities 0-0.15<br />
•Solar like star Fe/H=0.08, M=1.06 Msun<br />
•Some period ratios are fairly close to integer or<br />
half-integer values, but no mean-motion<br />
resonances.<br />
•Roughly regularly spaced on a logarithmic scale<br />
•Kepler-11: six transiting <strong>planets</strong><br />
Kepler-11 a[AU] Msini<br />
b 0.09 4.3<br />
c 0.11 13.5<br />
d 0.15 6.1<br />
e 0.19 8.4<br />
f 0.25 2.3<br />
g 0.46
numbers=distance in mutual Hill spheres.<br />
Packed systems<br />
Lovis et al. 2011<br />
•Low mass <strong>planets</strong> seem to follow a radius exclusion law: they cannot be too close together<br />
when measured in mutual Hill spheres.<br />
•Many systems seem to be dynamically packed. Could not add another planet.<br />
•Numerical simulations show that systems with 3–5 <strong>planets</strong> and masses between a few ME<br />
and a few MJ, separations between adjacent <strong>planets</strong> should be of at least 7–9 mutual Hill radii<br />
to ensure stability on a 10-Gyr timescale.<br />
•Additional stability islands exist at resonances.<br />
•Dynamical evolution of the systems. Ejection/collision of surplus <strong>planets</strong>.
Kepler multiple systems<br />
•Kepler has detected a lot of systems with multiple<br />
1<br />
transiting planet candidates.<br />
•The distribution of observed period ratios shows<br />
0.6<br />
that the majority of candidate pairs are neither in nor<br />
near low-order mean motion resonances. 0.4<br />
•Nonetheless, there is a small but statistically<br />
0<br />
significant excesses of pairs both in resonance and<br />
spaced slightly further apart, particularly near 2:1.<br />
N/N TOT<br />
N/N TOT < 5<br />
•Resonant capture due during migration?<br />
Lissauer et al. 2011<br />
1<br />
0<br />
1 1.5 2 2.5 3 3.5 4 4.5 5<br />
0.8<br />
0.2<br />
Slope of Cumulative Period Ratio<br />
500<br />
450<br />
400<br />
350<br />
300<br />
250<br />
200<br />
150<br />
100<br />
Period Ratio<br />
Kepler adjacent pairings<br />
RV adjacent pairings<br />
1 10 100<br />
50<br />
Period Ratio<br />
Kepler adjacent pairings<br />
RV adjacent pairings<br />
Fig. 6.— Cumulative fraction of neighboring planet pairs for Kepler candidate multiplanet sy<br />
–46–<br />
Kepler adjacent pairings<br />
RV adjacent pairings<br />
0<br />
1 1.5 2 2.5 3<br />
Period Ratio<br />
3.5 4 4.5 5<br />
Fig. 7.— Slope of the cumulative fraction of Kepler neighboring planet pairs (solid black curve) an<br />
multiplanet systems detected via radial velocity (dashed red curve) with period ratio exceeding th
6.8 Radius distribution
or stems directly from 35% rms uncertainty<br />
the KIC, which propagates directly to 35%<br />
in Rp. We assumed a central transit over<br />
ar diameter in equation (2). For randomly<br />
Planet Occurrence from Kepler 9<br />
Planet Occurrence ! d<br />
0.001 0.002 0.004 0.0079 0.016 0.032 0.063 0.13 0.25 0.50 1.0<br />
2 ransiting orientations, the f/dlogP/dlogR average duration<br />
p<br />
π/4 times the duration of a central transit.<br />
0.000035 0.00007 0.00014 0.00028 0.00056 0.0011 0.0022 0.0044 0.0088 0.018 0.035<br />
rrection reduces our Planet Occurrence SNR! in fcell equation (1) by<br />
32<br />
π/4, i.e. a true signal-to-noise ratio threshtead<br />
of 10.0. This is still a very conservative<br />
1 (9) 0.0042<br />
1 (15) 0.0075<br />
1 (52) 0.026<br />
58036 0.00015<br />
58030 0.00026<br />
58020 0.00090<br />
16 reshold. Additionally, our method does not<br />
2 (11) 0.0054 4 (39) 0.019 6 (69) 0.034 1 (15) 0.0071 1 (28) 0.014 1 (25) 0.012 3 (168) 0.082<br />
58031 0.00019 58028 0.00067 58022 0.0012 58017 0.00025 58009 0.00049 58004 0.00043 57997 0.0029<br />
the small fraction of transits that are graz-<br />
e reduced 1 (2) 0.0010 significance. 1 (6) 0.0029 4 (34) 0.017 3 (25) 0.012 1 (15) We 0.0076 3 (70) assumed 0.034 4 (154) 0.076 perfect<br />
58018 0.00004 58009 0.00010 58004 0.00058 57998 0.00043 57988 0.00027 57981 0.0012 57963 0.0026<br />
8<br />
r σCDPP values computed for 3 hr intervals.<br />
Planet Radius, R p (R E)<br />
1 (6) 0.0029 1 (9) 0.0044 7 (73) 0.036 4 (74) 0.037 2 (31) 0.015 4 (160) 0.079 5 (278) 0.14<br />
57982 0.00010 57967 0.00015 57942 0.0012 57903 0.0013 57859 0.00053 57804 0.0028 57738 0.0048<br />
derestimate σCDPP for a 6 hr interval (ap-<br />
1 (4) 0.0021<br />
4 (45) 0.022 2 (18) 0.0087 4 (60) 0.030 5 (153) 0.076 6 (208) 0.10 5 (198) 0.099<br />
57907 0.00007<br />
57808 0.00078 57749 0.00030 57653 0.0010 57538 0.0027 57429 0.0036 57240 0.0035<br />
the duration 4 of a P = 50 day transit) by<br />
3 (20) 0.010 9 (104) 0.052 21 (353) 0.18 23 (607) 0.31 16 (591) 0.30 17 (799) 0.43<br />
se are minor corrections 57442 0.00035 57262 0.0018 57001 0.0062 and 56605 0.011 affect 55834 0.011 54371 the 0.015 nu-<br />
denominator of equation (2) nearly equally.<br />
2<br />
3 (21)<br />
56665<br />
0.011 7 (64)<br />
0.00037 55966<br />
0.032 21 (269)<br />
0.0011 54585<br />
0.15 31 (521)<br />
0.0051 52260<br />
0.30 36 (893)<br />
0.010 48639<br />
0.53 34 (1101)<br />
0.019 43318<br />
0.79 18 (749)<br />
0.028 36296<br />
1 (5) 0.0026 3 (17) 0.012 11 (85) 0.060 19 (262) 0.22 11 (159) 0.16 16 (375) 0.43 12 (410) 0.83 7 (295) 0.76<br />
urrence 52618 as 0.00009 49170 a 0.00042 Function 44059 0.0021 37278 0.0079 29498 of 0.0056 Planet 21606 0.015 14712 Radius<br />
0.029 9157 0.027<br />
0.61<br />
0.021<br />
Number o<br />
Kepler<br />
0.001<br />
results<br />
Number of Planets per Star with P < 50 days<br />
1.0 1.4 2.0 2.8 4.0 5.7 8.0 11.3 16.0 22.6<br />
Planet Radius (RE) 3 (10) 0.0075 1 (10) 0.011 4 (50) 0.067 6 (59) 0.22 1 (18) 0.062 3 (85) 0.81 2 (41) 0.95<br />
1 30446 0.00026 22540 0.00040 15445 0.0023 9764 0.0077 5784 0.0022 3170 0.028 1605 0.033<br />
0.68 1.2 2.0 3.4 5.9 10 17 29 50<br />
Orbital Period, P (days)<br />
Fig. 4.— Planet occurrence as a function of planet radius and orbital period for P 10 are shown as black dots. The phase space is divided into a grid of logarithmically spaced cells within which planet occurrence<br />
is computed. Only stars in the “solar subset” (see selection criteria in Table 1) were used to compute occurrence. Cell color indicates<br />
planet occurrence with the color scale on the top in two sets of units,occurrencepercellandoccurrenceperlogarithmicarea unit. White<br />
cells contain no detected <strong>planets</strong>. Planet occurrence measurements are incomplete and likely contain systematic errors inthehatched<br />
region (Rp < 2 R⊕). Annotations in white text within each cell list occurrence statistics: upper left—the number of detected <strong>planets</strong><br />
with SNR > 10, npl,cell, andinparenthesesthenumberofaugmented<strong>planets</strong>correcting for non-transiting geometries, npl,aug,cell; lower<br />
left—the number of stars surveyed by Kepler around which a hypothetical transiting planet with Rp and P values from the middle of the<br />
cell could be detected with SNR > 10; lower right—fcell, planetoccurrence,correctedforgeometryanddetectionincompleteness; upper<br />
right—d2 urrence varies by three orders of magnitude<br />
0.00<br />
s-period plane (Figure 4). To isolate the de- Howard et al. 2011<br />
these parameters, we first considered planet<br />
Planet Radius (RE) s•Only a function reliable of planet KEPLER radius, candidates marginalizing around bright, main sequence GK stars.<br />
ets f/dlog10 P/dlog10 Rp, planetoccurrenceperlogarithmicareaunit(dlog10 P dlog10 Rp =28.5gridcells).<br />
•Correct with P for < observational 50 days. We computed bias. Complete oc- to p=50 d, and R > 2 RE.<br />
ng equation (2)<br />
•decrease with<br />
for cells<br />
period<br />
with the ranges of<br />
re 4 but for all periods less than 50 days.<br />
valent •decrease to summing with the size occurrence (S/N) values in<br />
ng•Diagonal rows of cells band to obtain of increasing the occurrence planet frequency. for<br />
n a radius interval with P < 50 days. The<br />
tribution •Strong<br />
of<br />
increase<br />
planet radii<br />
towards<br />
(Figure<br />
small<br />
5) increases<br />
radius. Reminiscent of RV results.<br />
with •But decreasing absolute fraction Rp. less than HARPS. Radius - mass relationship? Does HARPS detect high<br />
eddensity this distribution <strong>planets</strong> that of planet KEPLER occurrence cannot with see?<br />
0.12<br />
0.10<br />
0.08<br />
0.06<br />
0.04<br />
0.02<br />
Incompleteness<br />
1.0 1.4 2.0 2.8 4.0 5.7 8.0 11.3 16.0 22.6<br />
Fig. 5.— Planet occurrence as a function of planet radius for<br />
<strong>planets</strong> with P
6.9 Mass-Radius diagram
M-R: Giant <strong>planets</strong><br />
•During evolution on Gyrs, giant <strong>planets</strong> contract and cool.<br />
•The more massive the core, the smaller the total radius.<br />
•Many transiting Hot Jupiters are bloated <strong>planets</strong>: not explainable by standard<br />
internal structure modeling. Energy source must act deep in the interior. Several<br />
mechanism proposed for explanation.<br />
•Some giant exo<strong>planets</strong> seem to contain very large amounts of metals (>100 ME)
M-R: Low mass <strong>planets</strong><br />
Kepler-11 b,c,d,e,f<br />
Kepler 10b<br />
Corot-7b<br />
•Diversity: very different radii for a given M. Some are clearly rocky <strong>planets</strong>.<br />
•Observational constraints on the internal composition.<br />
•Migration?<br />
•Problem: degeneracy. different composition can give the same M-R.<br />
•e.g. Ice=rock + some H2/He. Spectra of atmospheres can help to distinguish: Water vapor<br />
atmosphere has a smaller scale height than a H2/He atmosphere.<br />
•Close in <strong>planets</strong>! Evaporation (atmospheric escape) could play an important role on Gyrs.<br />
•Must consider formation and evolution.<br />
•Origin unknown... low mass <strong>planets</strong> from the beginning or boiled down giant <strong>planets</strong>?
Additional observations
Direct imaging: <strong>planets</strong> form hot<br />
Janson et al. 2011<br />
•The two competing models<br />
for giant planet formation, core<br />
accretion and direct collapse,<br />
predict different initial<br />
conditions for planet evolution.<br />
•For direct collapse, <strong>planets</strong><br />
should initially be very hot.<br />
•For core accretion, they can<br />
also be cold.<br />
•Observations point to a “Hot<br />
start”.<br />
•This could help to distinguish<br />
formation models.
Transits: correlation planetary core mass<br />
Guillot et al.<br />
and stellar metallicity<br />
•Transit observations & RV mass measurements show that the core mass<br />
of giant <strong>planets</strong>, and the stellar metallicity are positively correlated.<br />
•This is reproduced by core accretion models.<br />
•Recent observations maybe even indicate that that all giant <strong>planets</strong><br />
contain at least 10 ME of metals.<br />
•For direct collapse, <strong>planets</strong> can result both enriched and depleted.<br />
Miller & Fortney 2010
Questions?