optical observations of high-latitude clouds

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Optical Observations of High-Latitude Clouds Adolf N. Witt University of Toledo

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Optical Observations of High-Latitude Clouds. Adolf N. Witt University of Toledo. Collaborators: Steve Mandel, Hidden Valley Obs., Soquel, CA Thomas G. Dixon, Univ. of Hertfordshire, UK Paul H. Sell, Univ. of Toledo Karl D. Gordon, Univ. of Arizona Uma P. Vijh, STScI With support from: - PowerPoint PPT Presentation

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Page 1: Optical Observations of High-Latitude Clouds

Optical Observations of High-Latitude Clouds

Adolf N. Witt

University of Toledo

Page 2: Optical Observations of High-Latitude Clouds

Collaborators:

Steve Mandel, Hidden Valley Obs., Soquel, CAThomas G. Dixon, Univ. of Hertfordshire, UKPaul H. Sell, Univ. of ToledoKarl D. Gordon, Univ. of ArizonaUma P. Vijh, STScI

With support from:

NSF Galactic Astronomy ProgramRC Optical SystemsSanta Barbara Instrument Group, Inc.Software BisqueAstrodon

Page 3: Optical Observations of High-Latitude Clouds

First optical studies of HLCs by Allan Sandage, 1976, AJ, 81, 954, with M81

Page 4: Optical Observations of High-Latitude Clouds

“Re-discovery” of HLCs by IRAS, F. J. Low et al. 1984, ApJ, 278, L19Led to new designation as “IR Cirrus”Followed by detailed studies at mm-wavelengths (CO) by Magnani et al.

Page 5: Optical Observations of High-Latitude Clouds

High-Latitude Clouds are ideal for studying the morphologyof the diffuse interstellar medium.

• Nearby, ~ 100 pc• Individual “clouds” seen in relative isolation• Little line-of-sight confusion• Free of star-formation effects• Wide range of optical depths• Atomic as well as molecular gas• Typical cloud “sizes” can be measured directly

We can see actual “clouds”

Page 6: Optical Observations of High-Latitude Clouds

Advantages of Optical Imaging Approach

• Combines high spatial resolution (arc sec) with large field of view• Sensitive to column density of dust ---> total gas column density• Insensitive to dust temperature• Independent of atomic or molecular state of the gas as long as dust-to-gas ratio is constant• Offers ideal conditions for study of dust luminescence• Direct evidence for small-scale structure on few 102 AU scale• Low cost Disadvantages (No such thing as a free lunch!!)

• Low surface brightness (few % of that of the dark night sky)

Page 7: Optical Observations of High-Latitude Clouds

Instrumentation

Remotely operated, self-guided small telescopes, equipped with CCD cameras.

Detection of diffuse, extended sources depends only on f-ratio, not aperture.

Location: New Mexico Skies Altitude ~7300 ft, near Cloudcroft, NM

Primary Goal: Determination of the optical SEDs of HLCs

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Page 8: Optical Observations of High-Latitude Clouds

Optical Bandpasses

Special BGRIHa filter set during Phase1 of our program

15-band BATC filter set during Phase 2 of our program. These filters allow the determination of a detailed cloud SED while avoiding the strongest emission features of the permanent airglow from the Earth atmosphere.

Page 9: Optical Observations of High-Latitude Clouds

What makes a high-latitude cloud shine?

• Scattering of the Galactic interstellar radiation field by dust.• Photoluminescence by nanoparticles, primarily Extended Red

Emission excited by far-UV photons from the ISRF.• H-alpha in emission, mostly from Galactic HII regions, scattered by dust in the HLCs.

This is extended red emission ---->

Page 10: Optical Observations of High-Latitude Clouds

How important is ERE?

• about 30% of total surface brightness of HLCs near 600 nm at intermediate latitudes

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ERE is relatively important, because dust scattering is not very efficient at high galactic latitudes.

Page 11: Optical Observations of High-Latitude Clouds

Here’s why:

• Illumination of HLCs comes mainly from the Milky Way

• Most of the light is scattered with scattering angles ~90 0

• HG phase function for forward-scattering grains ---> highly inefficient at ~ 90 0

• ERE is emitted isotropically, no dependence on direction of incoming illuminating radiation; depends only on density of UV radiation.

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Page 12: Optical Observations of High-Latitude Clouds

Focus: Large-Scale Cloud MorphologyMBM 12

Page 13: Optical Observations of High-Latitude Clouds

MBM 30

Page 14: Optical Observations of High-Latitude Clouds

MBM 32

Page 15: Optical Observations of High-Latitude Clouds

Focus: Small-Scale Structure in MBM 12

Linear structures ~ 500 AU wide

Page 16: Optical Observations of High-Latitude Clouds

MBM 12

Sharp edges

Page 17: Optical Observations of High-Latitude Clouds

MBM 12

Page 18: Optical Observations of High-Latitude Clouds

MBM 30

Page 19: Optical Observations of High-Latitude Clouds

Focus: Small-Scale Structure in AbsorptionM 81; Image Credit: Tony Hallas

http://www.astrophoto.com/ (with permission)

Page 20: Optical Observations of High-Latitude Clouds

M81 detail

Linear structures again; nT ~ 106 K cm-3

Page 21: Optical Observations of High-Latitude Clouds

Same M81 cirrus observed in CO by A. Heithausen2006, A&A, 450, 193

cirrus resolves into small molecular clumps

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Page 22: Optical Observations of High-Latitude Clouds

Small-area molecular clumps (SAMS) near M81

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Page 23: Optical Observations of High-Latitude Clouds

Combining optical structure data with IR and radio structure data can extend 2-D angular power spectrum (S. J. Gibson, 2006, SINS)

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We are collaborating with Steven Gibson on the analysis of our data.

Page 24: Optical Observations of High-Latitude Clouds

Conclusions

• Optical imaging data of high-latitude clouds reveal ISM morphology and small-scale structures over 3 orders of magnitude of linear scale

• Cloud morphology: Clumpy cores embedded in low-density envelope

• Small-scale structure: linear strands of high-density gas, ~500 AU

• Under special conditions (e.g. M81) structure in Galactic ISM can be observed in absorption.

• Illumination geometry of high-latitude clouds makes them ideal test beds for studies of extended red emission (ERE) in the diffuse ISM.