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5.8(1.4) 4 .49(97)×10−31621(173)
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8.0(2.9) 4 .75(46)×10−31480(82)
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TrES-4b152250(37) 3.6(0.75) 1 .37(11)×10−31889(63) Td=1891(81) K
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4.5(1.0) 1 .48(16)×10−31727(83)
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5.8(1.4) 2 .61(59)×10−32112(283)
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8.0(2.9) 3 .18(44)×10−32168(197)
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WASP-1b162347(35) 3.6(0.75) 1 .17(16)×10−31678(87) Td=1719(89) K
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4.5(1.0) 2 .12(21)×10−31923(91)
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5.8(1.4) 2 .82(60)×10−32042(253)
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8.0(2.9) 4 .70(46)×10−32587(176)
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WASP-2b171661(69) 3.6(0.75) 8 .3(3.5)×10−41264(164) Td=1280(121) K
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4.5(1.0) 1 .69(17)×10−31380(53)
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5.8(1.4) 1 .92(77)×10−31299(232)
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8.0(2.9) 2 .85(59)×10−31372(154)
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WASP-4b182163(60) 3.6(0.75) 3 .19(31)×10−32156(97) Td=2146(140) K
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4.5(1.0) 3 .43(27)×10−31971(75)
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WASP-12b193213(119) 0.9(0.15) 8 .2(1.5)×10−43002(104) Td=2939(98) K
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1.25(0.16) 1 .31(28)×10−32894(149)
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1.65(0.25) 1 .76(18)×10−32823(88)
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2.15(0.32) 3 .09(13)×10−33018(51)
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3.6(0.75) 3 .79(13)×10−32704(49)
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4.5(1.0) 3 .82(19)×10−32486(68)
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5.8(1.4) 6 .29(52)×10−33167(179)
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8.0(2.9) 6 .36(67)×10−32996(229)
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WASP-18b203070(50) 3.6(0.75) 3 .1(2)×10−33000(107) Td=2998(138) K
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4.5(1.0) 3 .8(3)×10−33128(150)
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5.8(1.4) 4 .1(2)×10−33095(103)
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8.0(2.9) 4 .3(3)×10−32991(153)
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WASP-19b212581(49) 1.65(0.25) 2 .59(45)×10−32677(135) Td=2677(244) K
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XO-1b221526(24) 3.6(0.75) 8 .6(7)×10−41300(32) Td=1306(47) K
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4.5(1.0) 1 .22(9)×10−31265(34)
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5.8(1.4) 2 .61(31)×10−31546(89)
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8.0(2.9) 2 .10(29)×10−31211(87)
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XO-2231685(33) 3.6(0.75) 8 .1(1.7)×10−41447(102) Td=1431(98) K
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4.5(1.0) 9 .8(2.0)×10−41341(105)
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5.8(1.4) 1 .67(36)×10−31497(155)
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8.0(2.9) 1 .33(49)×10−31179(219)
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XO-3241982(82) 3.6(0.75) 1 .01(4)×10−31875(30) Td=1871(63) K
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4.5(1.0) 1 .43(6)×10−31965(40)
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5.8(1.4) 1 .34(49)×10−31716(330)
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8.0(2.9) 1 .50(36)×10−31625(236)
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aThe planet’s expected day-side effective temperature in the absence of reflection or recirculation ( AB= 0,ε= 0). The 1 σuncertainty is shown
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in parenthese.
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bThe bandwidth is shown in parenthese.
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cEclipse depths and phase amplitudes are unitless, since the y are measured relative to stellar flux.
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dTdandTndenote the day-side and night-side effective temperatures o f the planet, as estimated from thermal secondary eclipse de pths and
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thermal phase variations, respectively. The estimated 1 σuncertainties are shown in parentheses. The default day-si de temperature is computed
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using only observations at λ >0.8µm. Eclipse measurements at shorter wavelengths may then be u sed to estimate the planet’s albedo at those
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wavelengths, Aλ. Note that this is a spherical albedo; the geometric albedo i s given by Ag=2
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3Aλ. If —on the other hand— AB= 0 is assumed,
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then all the day-side flux is thermal, regardless of waveband , yielding the second Tdestimate.
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eWhen multiple measurements of an eclipse depth have been pub lished in a given waveband, we use the most recent observatio n. In all cases
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these observations are either explicitly agree with their o lder counterpart, or agree with the re-analyzed older data.
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1Snellen et al. (2009); Alonso et al. (2009b); Gillon et al. (2 009); Rogers et al. (2009); Deming et al. (2010),2Alonso et al. (2009a); Snellen et al.
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(2010); Gillon et al. (2010); Alonso et al. (2010); Deming et al. (2010),3Deming et al. (2007); Demory et al. (2007); Stevenson et al. ( 2010);
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Knutson et al. in prep.,4Todorov et al. (2010),5Borucki et al. (2009); Christiansen et al. (2010),6Laughlin et al. (2009),7Knutson et al.
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(2009b),8Deming et al. (2006); Knutson et al. (2007a); Barnes et al. (2 007); Charbonneau et al. (2008); Knutson et al. (2009c); Ago l et al.
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(2010),9Richardson et al. (2003); Deming et al. (2005); Cowan et al. ( 2007); Rowe et al. (2008); Knutson et al. (2008),10Sing & L´ opez-Morales
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(2009),11Snellen & Covino (2007),12Charbonneau et al. (2005); Knutson et al. (2007b),13O’Donovan et al. (2010); Croll et al. (2010a);
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Kipping & Bakos (2010b),14Fressin et al. (2010); Croll et al. (2010b); Christiansen et al. (2010b),15Knutson et al. (2009a),16,17Wheatley et al.
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(2010),18Beerer et al. (2010),19L´ opez-Morales et al. (2010); Campo et al. (2010); Croll et a l. (2010c),20Nymeyer et al. (2010),21Anderson et al.
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(2010),22Machalek et al. (2008),23Machalek et al. (2009),24Machalek et al. (2010)
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arXiv:1001.0013v2 [astro-ph.CO] 8 Jan 2010Astronomy& Astrophysics manuscriptno.akari˙LF˙aa˙v7 c∝circlecopyrtESO 2018
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October30,2018
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EvolutionofInfraredLuminosityfunctionsofGalaxiesint he
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AKARINEP-Deepfield
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Revealing thecosmic star formationhistory hidden by dust⋆,⋆⋆
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Tomotsugu Goto1,2,⋆⋆⋆,T.Takagi3,H.Matsuhara3,T.T.Takeuchi4,C.Pearson5,6,7, T.Wada3,T.Nakagawa3,O.Ilbert8,
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E.LeFloc’h9,S.Oyabu3, Y.Ohyama10,M.Malkan11, H.M.Lee12, M.G.Lee12,H.Inami3,13,14, N.Hwang2, H.Hanami15,
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M.Im12, K.Imai16,T.Ishigaki17,S.Serjeant7,and H.Shim12
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1Institute for Astronomy, University of Hawaii,2680 Woodla wnDrive, Honolulu, HI,96822, USA
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e-mail:tomo@ifa.hawaii.edu
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2National Astronomical Observatory, 2-21-1 Osawa,Mitaka, Tokyo, 181-8588,Japan
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3Institute of Space and Astronautical Science, JapanAerosp ace Exploration Agency, Sagamihara,Kanagawa 229-8510
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4Institute for Advanced Research, Nagoya University, Furo- cho, Chikusa-ku, Nagoya 464-8601
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5Rutherford Appleton Laboratory, Chilton, Didcot,Oxfords hire OX110QX, UK
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6Department of Physics,Universityof Lethbridge, 4401 Univ ersity Drive,Lethbridge, AlbertaT1J 1B1, Canada
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7Astrophysics Group, Department of Physics, The OpenUniver sity, MiltonKeynes, MK76AA, UK
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8Laboratoire d’Astrophysique de Marseille, BP8,Traverse d u Siphon, 13376 Marseille Cedex 12, France
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9CEA-Saclay,Service d’Astrophysique, France
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10Academia Sinica,Institute of Astronomyand Astrophysics, Taiwan
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11Department of Physicsand Astronomy, UCLA,Los Angeles, CA, 90095-1547 USA
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12Department of Physics& Astronomy, FPRD,Seoul National Uni versity, Shillim-Dong,Kwanak-Gu, Seoul 151-742, Korea
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13Spitzer Science Center,California Institute ofTechnolog y, Pasadena, CA91125
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14Department of Astronomical Science,The Graduate Universi tyfor Advanced Studies
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15Physics Section,Facultyof Humanities and SocialSciences , Iwate University, Morioka, 020-8550
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16TOMER&D Inc. Kawasaki, Kanagawa 2130012, Japan
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17Asahikawa National College of Technology, 2-1-6 2-joShunk ohdai, Asahikawa-shi, Hokkaido 071-8142
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Received September 15, 2009; accepted December 16, 2009
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ABSTRACT
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Aims.Dust-obscured star-formation becomes much more important with increasing intensity, and increasing redshift. We aim to
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reveal cosmic star-formationhistoryobscured bydust usin g deep infraredobservation withthe AKARI.
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Methods. We construct restframe 8 µm, 12µm, and total infrared (TIR) luminosity functions (LFs) at 0.15< z <2.2using 4128
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infraredsources intheAKARINEP-Deepfield.Acontinuous fil tercoverage inthemid-IRwavelength(2.4,3.2,4.1,7,9,11 , 15,18,
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and 24µm) by the AKARI satellite allows us to estimate restframe 8 µm and 12 µm luminosities without using a large extrapolation
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based ona SEDfit,which was the largestuncertainty inprevio us work.
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Results. Wehavefoundthatall8 µm(0.38< z <2.2),12µm(0.15< z <1.16),andTIRLFs( 0.2< z <1.6),showacontinuous
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andstrongevolutiontowardhigher redshift.Intermsofcos micinfraredluminositydensity( ΩIR),whichwasobtainedbyintegrating
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analytic fits to the LFs,we found a good agreement withprevio us work at z <1.2. We found the ΩIRevolves as ∝(1+z)4.4±1.0.
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Whenweseparatecontributionsto ΩIRbyLIRGsandULIRGs,wefoundmoreIRluminoussourcesareinc reasinglymoreimportant
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