PHYS 2070 – Observational Astronomy Lee Clement.  “Dirty snowball”  Nucleus ▪ Rock ▪ Dust ▪ Water ice ▪ Frozen gases ▪ eg. CO 2  Blasted by the Sun.

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Presentation transcript:

PHYS 2070 – Observational Astronomy Lee Clement

 “Dirty snowball”  Nucleus ▪ Rock ▪ Dust ▪ Water ice ▪ Frozen gases ▪ eg. CO 2  Blasted by the Sun  Coma ▪ Fuzzy temporary atmosphere Flyby image of comet Wild 2 Source: NASA

 Has two tails  Dust tail ▪ Solar radiation knocking dust away from the coma  Gas/ Ion tail ▪ Solar wind ▪ High-speed charged particles Comet Structure Source: Wikimedia Commons (Translated from Finnish)

 Small(ish) nucleus  16km across on average Half the size of Winnipeg  HUGE coma  Can be 1.6 million km across ▪ Bigger than the Sun! Source: CBC -one-great-city-wide.jpg Source: NASA

 Size in the sky  Depends on size and distance  Usually 1 – 3 arcminutes across  Magnitude  Varies  Usually around 9 – 13 magnitude Comet Hale-Bopp Source: Wikimedia Commons _hires_adj.jpg _hires_adj.jpg

 Eye candy  Very old  Earliest record of material from the nebula our solar system formed from  4.6 billion years old  Could be the source of Earth’s water  Maybe even organic molecules!  Great bombardment  Rosetta Mission (ESA) Comet McNaught Source: NASA The Pacific Ocean from the ISS Source: NASA 7/hires/iss007e10807.jpg

 Look at them  Watching the tails and comas  Fly by them  Pick up debris and analyze composition  Look at nucleus  Eg. Stardust mission  Throw stuff at them  Analyze ejecta  Eg. Deep Impact mission Deep Impact Source: NASA

 Kuiper Belt  Short period comets ▪ Orbital periods < 200 years ▪ Eg. Halley’s Comet  Oort Cloud  Long period comets ▪ Orbital periods > 200 years ▪ Some we have only seen once Source: NASA

 Theoretical  Jan Oort, 1950  Where do long period comets come from?  Spherical cloud of icy chunks  Probably 0.1 – 2 trillion of them  Leftover material from the formation of the solar system  “Storage” of future comets ▪ Knocked out of place by ▪ Passing stars ▪ Molecular clouds ▪ Tidal interactions with the Milky Way

 The “edge” of our solar system  Where the Sun stops having any significant gravitational or physical influence  5,000 – 100,000 AU radius ▪ % the radius of the Milky Way! ▪ Kuiper Belt’s radius is only 30 – 55 AU Source: Wikimedia Commons sys(PNG-fin)1.png

 Problems:  Sparse ▪ Volume ~ 4.2 x AU 3  Small  Not very luminous  Really far away (5,000 – 100,000 AU) ▪ Pluto is only 30 – 40 AU from the Sun

 Cosmic Microwave Background Radiation  Leftover “backdrop” from the Big Bang  Look for asymmetries to determine: ▪ Mass ▪ Distance ▪ Size distribution  Babich D, Blake CH, Steinhardt CL What can the cosmic microwave background tell us about the outer solar system? ApJ. 669 :  Babich D, Loeb A Imprint of distortions in the oort cloud on the CMB anisotropies. NewA. 14 :

 Kepler Mission  Space observatory designed to detect planets in other solar systems ▪ Transit method  Could be able to detect Oort Cloud objects as well  Ofek EO, Nakar E Detectability of oort cloud objects using kepler. ApJL. 711 : L7-L11

Babich D, Blake CH, Steinhardt CL What can the cosmic microwave background tell us about the outer solar system? ApJ. 669 : Babich D, Loeb A Imprint of distortions in the Oort Cloud on the CMB anisotropies. NewA. 14 : Cain F, Gay P Pluto and the icy outer solar system. Podcast. European Space Agency Rosetta's frequently asked questions. NASA Comets. NASA Kuiper Belt & Oort Cloud. NASA Comet. Ofek EO, Nakar E Detectability of Oort Cloud objects using Kepler. ApJL. 711 : L7-L11