ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B...

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Subtraction Eran Ofek Big Data Dec 17, 2015 Ω B = 0.0447 ± 0.0016 Larson+10 Eran Ofek Weizmann Institute of Science ULTRASAT Exploring the UV transient sky

Transcript of ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B...

Page 1: ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B "=0.0447"±0.0016" Larson+10" The advantages of a large FOV UV! 2. Ground based

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

Eran  Ofek  Weizmann  Institute  of  Science  

   

ULTRASAT  Exploring  the  UV  transient  sky  

Page 2: ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B "=0.0447"±0.0016" Larson+10" The advantages of a large FOV UV! 2. Ground based

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

What is ULTRASAT Capabilities

Science motivation highlight SN shock cooling and breakout GW EM counterpart …

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

Weizmann-Caltech led proposed small space mission (~$100M)

PIs: Waxman & Kulkarni JPL, ISA, IAI, ElOp

Exploring the UV transient sky Designed to:

SN shock cooling and breakout discovery & alerts Studying SN progenitors and physics Search & alert for GW EM counterparts in the UV Explore the transient sky (e.g., variability, TDE, GRB, QSO)

Page 4: ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B "=0.0447"±0.0016" Larson+10" The advantages of a large FOV UV! 2. Ground based

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

33 cm f/1 Schmidt NUV band (220-280 nm) δ-d CCD (QE~70%) Lim mag. 21.8 AB (3x300s; 5σ)

30 mag arcsec2 (in 3 months) FWHM ~24’’

FOV: 235 deg2 Volumetric rate: ~380 X GALEX ~12 X ZTF ~0.2 LSST (but in NUV)

Page 5: ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B "=0.0447"±0.0016" Larson+10" The advantages of a large FOV UV! 2. Ground based

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

GEO +300km Avoiding geocoronal lines Observing continuously 24/7 Direct & continuous communication

All data transmission

Page 6: ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B "=0.0447"±0.0016" Larson+10" The advantages of a large FOV UV! 2. Ground based

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

For several weeks - All sky survey to 22.8 AB mag. Continuous observing of the same FOV for 6 months Switching to opposite hemisphere after 6 months Mission life time: 2yr

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

Pointings

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

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Image transmission (<200s) Real time processing & alerts (<60s)

Data processing – see recent advances: Zackay & Ofek 2015a,b (+) Zackay, Ofek & Gal-Yam 2016 (-)

Page 9: ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B "=0.0447"±0.0016" Larson+10" The advantages of a large FOV UV! 2. Ground based

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

SN shock breakout & cooling GW EM counterpart search TDE, GRB, QSO, variability...

Page 10: ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B "=0.0447"±0.0016" Larson+10" The advantages of a large FOV UV! 2. Ground based

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

Shock breakout

occurs when τ~c/v Measure R*, E/M, composition

R*/c  

diffu

sion   t-­‐4/3  

L~R*2  

log  t  ~30  min   ~1  day  

Luminosity

 

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

SN shock cooling – some observations 2008D (?)

(Soderberg+08)

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

What can we learn? Stellar radius Explosion energetics (E/M) Composition

Complications: Wind/CSM but can derive CSM mass

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

Accuracy?

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

Why UV? The rise time in optical >> rise time in UV Therefore, by the time optical reach max light -> T<1eV -> complicated physics Removing the degeneracy between E/M and R* requires UV observations Probe the temperature Brighter in UV in earlier times

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

Expectations

Page 16: ULTRASAT% ExploringtheUVtransientsky%vikram/bne_talks/ofek.pdfEran Ofek! Big Data Dec 17, 2015! Ω B "=0.0447"±0.0016" Larson+10" The advantages of a large FOV UV! 2. Ground based

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

The advantages of a large FOV UV

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

The advantages of a large FOV UV 1. LIGO/VIRGO error regions ~100 deg2

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

The advantages of a large FOV UV 2. Ground based observatory can follow up on 1/16 of the ToO within 20min. ULTRASAT – can access ~48% of the sky within 20min

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

3. EM counterpart properties highly uncertain. However, models predicts UV+blue counterpart at early times <6 hr.

λ [µ]10-1 100

f λ

1036

1037

1038

bpCaFNlvh.spec

Kasen+  (unpublished)  

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

TDE (>100 event/yr) GRB (a few/yr) QSO monitoring >20,000 Stellar monitoring >200,000

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Eran Ofek Big Data Dec 17, 2015

ΩB  =  0.0447  ±  0.0016  

Larson+10  

ULTRASAT capabilities have the potential to revolutionize transient research