Bit of Administration.

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Bit of Administration. Washburn Observatory Thursday, 8:30-9:30 Portfolios Due Thursday, April 29,, because of possible TAA strike Put in box outside 6522 Sterling All 5 must be securely bound together, including ones already graded Late portfolios will lose credit Lab 3 Due Thursday, April 29,, because of possible TAA strike Put in box outside 6522 Sterling Problem 5, HW 1 is a good starting point for the lab questions Note typo in Question 3 - Jupiter => Saturn

THE EXTRA-SOLAR PLANET PROJECT Phase 1: Last week s quiz. Phase 2 : A Web-Lecture on Extra-Solar Planets. Learn about extra-solar planets and have opportunity to earn 5 pts extra credit. 2 pts for evaluation questions 3 pts for success on quiz Preparation for next week s discussion sections (5/3-5/7). Access: http://eteach.engr.wisc.edu/meibom/espp/index.html Speed: 300 Kbps, 100 Kbps, and 37 Kbps. The hardware requirements for viewing the lecture are: A computer with connection to the Internet. Computer speakers or headphones. The software requirements for viewing the lecture are: Windows Operating System. Internet Explorer version 5.5 or later. Power Point 2002 or later ("Power Point Animation plug-in"). Campus computer-labs: http://www.doit.wisc.edu/computerlabs/index.asp Bring headphones!

Asteroids

Asteroids QuickTime and a Cinepak decompressor are needed to see this picture.

Asteroids 150,000 catalogued as many as grains of sand on the beach Size - few km typical, 1000 km largest (half Pluto)

Asteroids 150,000 catalogued, as many as grains of sand on the beach Size - few km typical, 1000 km largest (half Pluto) Density - 2-3 gm/cm 3 Note: About as expected for rock in low gravity Shape - Irregular because of low mass => low gravity

Asteroids Orbits

Asteroids Orbits - Earth-Crossing Asteroids

Comets

Comets 10 km Nucleus Plasma (Gas) Tail Ices and Rock Icy Planetesimal Coma Dust Tail

Comets Orbital Properties Long period comets P 10 5-10 6 yr => A 10,000 AU Elliptical to hyperbolic orbits Come from all directions - isotropic

Comets - Oort Cloud Perturbations by passing stars cause comets to fall in Origin of long-period comets 1 trillion comets

Comets Orbital Properties Long period comets P 10 5-10 6 yr => A 10,000 AU Elliptical to hyperbolic orbits Come from all directions - isotropic Short period comets P P < 200 yr => A < 50 AU Highly elliptical In ecliptic plane

Kuiper Belt Objects

Kuiper Belt Objects

Kuiper Belt Objects Triton Sedna Pluto and Charon 650 KBOs discovered 100,000 with radii > 10 km

Comets - Evolutionary Picture

Oort Cloud Primordial Icy Planetesimals Jupiter Forms Rocky Planetesimals Icy Planetesimals Fragmented Icy Planetesimals (KBOs) Kuiper Belt

Comets Periodic Comets - e.g., Halley s Comet Highly elliptical P < 200 yr Put into short periods by Jupiter

Comets Periodic Comets - e.g., Halley s Comet Highly elliptical P < 200 yr Put into short periods by Jupiter Fragmented after many passages around Sun

Meteors Showers - debris of old comets Earth orbit Past Comet

Meteors Types - Processed Meteorites Stony Meteorites 93% Just like crust of Earth Iron Meteorites 6 % Crystallization patterns => long cooling times

Meteors Types - Primitive Meteorites Stony, with trace of pure metallic flakes Carbonaceous chondrites Carbon compounds, and even water

Summary Asteroids Rocky Planetesimals Comets Long - Period = Icy Planetesimals Short - Period = Fragmented KBOs Pluto, Sedna,, Triton, Kuiper Belt Objects Icy Planetesimals Meteors Primitive Meteors = Rocky Planetesimals Processed Iron and Stony Meteorites Fragmented asteroids Meteor Showers Fragmented comets