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Lecture22-11-14-2006-ASTR111-Weigel-Revised

Course: ASTR 111, Fall 2008
School: George Mason
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the In news: Moonquakes In the news: Moonquakes http://science.nasa.gov/headlines/y2006/15mar_moonquakes.htm?list802911 Four types of vibration Deep 700 km below surface (tides) Vibrations (meteorites) Thermal expansion after deep freeze Shallow (20-30 km) below surface 1972-1977 (28 up to 5.5 on Richter scale) Outline for 14 November (Tuesday) Jupiter and Saturn Orbit Surface Atmosphere Rings...

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the In news: Moonquakes In the news: Moonquakes http://science.nasa.gov/headlines/y2006/15mar_moonquakes.htm?list802911 Four types of vibration Deep 700 km below surface (tides) Vibrations (meteorites) Thermal expansion after deep freeze Shallow (20-30 km) below surface 1972-1977 (28 up to 5.5 on Richter scale) Outline for 14 November (Tuesday) Jupiter and Saturn Orbit Surface Atmosphere Rings Moons Atmospheres gravity and escape velocity Atmospheres gravity and escape velocity Atmospheres The visible "surfaces" of Jupiter and Saturn are actually the tops of their clouds How do we know this? The light "spots" are actually "holes" if we look in them (not with a telescope, but with a spectrometer), we see radiation that differs from the rest of the planet. That is, the sun sends out its nearly blackbody spectrum, and what we see reflected tell us about what is in the atmosphere. The rapid rotation of the planets twists the clouds into dark belts and light zones that run parallel to the equator The key difference between these two is ... Jupiter's rings are more disorganized. The key similarity is that they both have light and dark colored rings. The outer layers of both planets' atmospheres show differential rotation How do we measure rotation? On the Sun, we just watch a sunspot. The Sun is rotating and for this reason we see sunspots return to the same place with respect to our view every 27 days. Near the poles it takes up to 35 days. On Jupiter, the same thing. the equatorial regions rotate slightly faster than the polar regions. For Jupiter, the difference is a few minutes For both Jupiter and Saturn, the polar rotation rate is nearly the same as the internal rotation rate Atmospheres The rapid rotation of the planets twists the clouds into dark belts and light zones that run parallel to the equator Atmospheres The visible "surfaces" of Jupiter and Saturn are actually the tops of their clouds The chemical composition of Jupiter and Saturn is hard to measure. Why? Atmospheres The outer layers of both planets' atmospheres show differential rotation The equatorial regions rotate slightly faster than the polar regions Atmospheres For both Jupiter and Saturn, the polar rotation rate is nearly the same as the internal rotation rate Spacecraft images show remarkable activity in the clouds of Jupiter and Saturn Storms The colored ovals visible in the Jovian atmosphere represent gigantic storms Some, such as the Great Red Spot, are quite stable and persist for many years Storms in Saturn's atmosphere seem to be shorter-lived In the news: Hurricane on Saturn? http://saturn.jpl.nasa.gov/multimedia/videos/video-details.cfm?videoID=136 vortex Hurricane-like at Saturn's south pole, where the vertical structure of the clouds is highlighted by shadows. Such a storm, with a well-developed eye ringed by towering clouds, is a phenomenon never before seen on another planet. Both Jupiter and Saturn emit more energy than they receive from the Sun. What does this tell us? The internal heat of Jupiter and Saturn has a major effect on the planets' atmospheres If Jupiter and Saturn formed at the same time, which should be emitting more heat? Saturn's atmosphere contains less helium than Jupiter's atmosphere This lower abundance may be the result of helium raining downward into the planet Helium "rainfall" may also account for Saturn's surprisingly strong heat output Outline for 14 November (Tuesday) Jupiter and Saturn Orbit Surface Atmosphere Rings Moons Saturn's rings are composed of numerous icy fragments, while Jupiter's rings are made of small rocky particles The principal rings of Saturn are composed of numerous particles of ice and ice-coated rock ranging in size from a few micrometers to about 10 m Jupiter's faint rings are composed of a relatively small amount of small, dark, rocky particles that reflect very little light Earth-based observations reveal three broad rings encircling Saturn Why can't the rings be solid? Roche limit Images from http://en.wikipedia.org/wiki/Roche_limit Something is Fishy How can a planet be solid? Saturn is circled by a system of thin, broad rings lying in the plane of the planet's equator This system is tilted away from the plane of Saturn's orbit, which causes the rings to be seen at various angl...

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George Mason - ASTR - 111
http:/www.theonion.com/content/node/32096Can't . keep . up . http:/space.newscientist.com/article.ns?id=dn10573&feedId=online-news_rss20Review Technique Jupiter's atmosphere: mostly H2 and He. Almost no H20 or CO2, which are greenhouse gasses .
George Mason - ASTR - 111
Note: Yesterday I sent an email about review notes (that included a practice exam) Exam is Tuesday Bring your student ID Latecomers: you may not enter after the first student has turned in their examOutline for 19 October (Thursday) Comments o
George Mason - ASTR - 111
Astronomy 111, Section 001, Fall 2006 Examination #2 ReviewRevised Version (includes someall solutions and a few corrections)o oooExam #2 will have 50 questions 25 questions will cover knowledge of the keyword definitions listed in the lectu
George Mason - CSI - 769
CSI 769/ASTR769 Fall 2005 Topics in Space Weather Project: Sun-Earth Chain Activities in Halloween Storms Phase 1: Physical Processes on the SunPhase 1 Assignment Date: Oct. 4, 2005 Phase 1 Due Date: Oct. 11, 2005 Requirements 1. Identify and descri
George Mason - CSI - 12
Topics in Space WeatherLecture 12IonosphereRobert R. Meier School of Computational Sciences George Mason Universityrmeier@gmu.eduCSI 76922 November 20051Topics Photoionization & Photoelectrons Photoionization & Chapman Layer Ionospheri
George Mason - CSI - 769
Topics in Space WeatherLecture 12IonosphereRobert R. Meier School of Computational Sciences George Mason Universityrmeier@gmu.eduCSI 76922 November 20051Topics Photoionization & Photoelectrons Photoionization & Chapman Layer Ionospheri
George Mason - CSI - 04
Space Weather Magnetic Field Origins Helioseismology Dynamo Theory1Motivation Solar magnetic fields are the driver of space weather; without the magnetic field there is no space weather. Can someone tell me why that is? Magnetic fields originat
George Mason - CSI - 769
Space Weather Magnetic Field Origins Helioseismology Dynamo Theory1Motivation Solar magnetic fields are the driver of space weather; without the magnetic field there is no space weather. Can someone tell me why that is? Magnetic fields originat
George Mason - CSI - 06
Heliosphere - Lectures 6October 04, 2005 Space Weather Course Corotating Interaction Region, Magnetic Clouds, Interplanetary Shocks, Shocks and Discontinuities Chapter 6-Gombosi (Shocks and Discontinuities) Chapter 6 - Kallenrode (The Solar Wind) (S
George Mason - CSI - 769
Heliosphere - Lectures 6October 04, 2005 Space Weather Course Corotating Interaction Region, Magnetic Clouds, Interplanetary Shocks, Shocks and Discontinuities Chapter 6-Gombosi (Shocks and Discontinuities) Chapter 6 - Kallenrode (The Solar Wind) (S
George Mason - CSI - 01
The Magnetosphere and PlasmasphereCSI 769 3rd section, Oct. Nov. 2005 J. Guillory Lecture 8 (Oct.25) Bow shock scattering; Magnetosphere structure, charged particle orbits Advance reading: Gombosi Ch.1 & 6 (and/or Parks Ch. 4, 8 &10). and Sci.
George Mason - CSI - 769
The Magnetosphere and PlasmasphereCSI 769 3rd section, Oct. Nov. 2005 J. Guillory Lecture 8 (Oct.25) Bow shock scattering; Magnetosphere structure, charged particle orbits Advance reading: Gombosi Ch.1 & 6 (and/or Parks Ch. 4, 8 &10). and Sci.
George Mason - CSI - 07
The Magnetosphere and PlasmasphereCSI 769 3rd section, Oct. Nov. 2005 J. Guillory Lecture 7 (Oct.18) Bow shock scattering; Magnetosphere structure, charged particle orbits Advance reading: Gombosi Ch.1 & 6 (and/or Parks Ch. 4, 8 &10), Tascione
George Mason - CSI - 769
The Magnetosphere and PlasmasphereCSI 769 3rd section, Oct. Nov. 2005 J. Guillory Lecture 7 (Oct.18) Bow shock scattering; Magnetosphere structure, charged particle orbits Advance reading: Gombosi Ch.1 & 6 (and/or Parks Ch. 4, 8 &10), Tascione
George Mason - CSI - 769
CSI 769/ASTR 769Topics in Space WeatherMid-term Exam (Take-Home) Assignment Date: Oct. 25, 2005 Due: Nov. 1, 2005Answer each of the following five questions. Each question contributes 20 points to the score. 1. Plasma- (1) Calculate and plot the
George Mason - CSI - 769
Homework for Upper Atmosphere-Ionosphere Section- Robert Meier 11/22/05 3- Assume an isothermal atmosphere consisting of atomic oxygen only. Use the following parameters: T= 600 K zo = 140 km atomic oxygen density at zo = 2.9 x 1010 cm-3 Solar flux a
George Mason - CSI - 769
Homework for Upper Atmosphere-Ionosphere Section- Robert Meier 1. Calculate the atmospheric N2, O2, and O number densities for the following conditions: November 27, 2003 Latitude = 45. Longitude = 0. Local Time = 12. Altitude = 120., 150., 200., 300
George Mason - CSI - 769
Magnetosphere Homework Assignment, 10/25/05 1. Look up typical magnetotail storm-period data (Bfield strength, particle densities, particle temperatures) from, e.g., IMP 8 data. 2. Use these data along with Fig. 5.6 of Tascione to estimate the order
George Mason - CSI - 769
CSI 769/PHYS 590 Solar AtmosphereHome work assignment #4 Assignment Date: Oct. 13, 2004 Due Date: Oct. 20, 2004 One important parameter of magnetized plasma is its value, which is defined as the ratio between the gas pressure and the magnetic press
George Mason - CSI - 769
CSI769/ASTR769Fall 2005Topics in Space Weather SyllabusPrerequisites: permission of instructor Credits: 3 Date: Tuesday Time: 7:20 PM to 10:00 PM Place: Enterprise Hall 76, Fairfax Campus Instructors:Jie Zhang Art Poland S&T 1 - 111 DKH 1014G (
George Mason - CSI - 769
CSI 769/ASTR769 Fall 2005 Topics in Space Weather Homework AssignmentHomework assignment #1 Assignment Date: Sep. 6, 2005 Due Date: Sep. 13, 2005 1. Emission Wavelength of solar atmosphere. Using the Wien's Law (T = hc/k) (formula 1.10.6 in Aschwand
George Mason - CSI - 769
CSI 769/ASTR769 Fall 2005 Topics in Space Weather Project: Sun-Earth Chain Activities in Halloween Storms Phase 3: MagnetosphereAssignment Date: Nov. 2, 2005 Due: The end of the semester This part of the project focuses on the energetics of the Hall
George Mason - CSI - 769
CSI 769/ASTR769 Fall 2005 Topics in Space Weather Project: Sun-Earth Chain Activities in Halloween Storms An Overview1. Objective The objective of this project is to help students comprehend the space weather system that involves energy and mass flo
George Mason - CSI - 769
HW 1 Heliosphere Septemeber 27 Due one day after next class, October 051. Consider a 10 MeV proton in interplanetary space. Determine its gyroradius; gyration period, and the wave numbers of Alfven waves in resonance with the proton (assume differe
George Mason - CDAW - 4
Working Group 4"We predict Success"Biggest Issues Forecasts "R" Us - what needs to be forecasted? Probabalistic forecasts - Can we give the forecasters an edge?Some questions MHD codes have large potential difference between hemispheres durin
George Mason - CDAW - 2
WG2 SummaryBroke into ring current/plasmasphere and radiation-belt subgroups RING CURRENT Identified events for addressing science questions What is the relative importance of the convection electric, penetration electric field, and variations of th
George Mason - CDAW - 2
WG2 Science Questions Radiation belt: 1. Which solar wind drivers are most geoeffective at radiation belt electron enhancements: high speed solar wind streams, CIRs, CMEs including magnetic cloud and shock categories? While we may know the general an
George Mason - CDAW - 2
WG1 + WG2 Joint Session Science Topics: Radiation belt: 1. Which solar wind drivers are most geoeffective at radiation belt electron enhancements: high speed solar wind streams, CIRs, CMEs including magnetic cloud and shock categories? While we may k
George Mason - CDAW - 2
INTRODUCTION: There are two types of data provided for the Polar EFI instrument.1) The raw spin-period E-Field, B-Field, SC potential and position data from the spacecraft.2) The T(ransformed) data which corrects E for vxB and subtracts
George Mason - CDAW - 2
MAXIS Balloon summary plots and event information provide by R. Millan (Robyn.Millan@dartmouth.edu 603-646-3969).Summary plots show 10 second averaged X-ray countrate between 20-1300 keV and 180-1300 keV as measured by the MAXIS germanium detector
George Mason - CDAW - 1
* * GLOBAL ATTRIBUTES * * TITLE WIND> Solar Wind Parameters PROJECT ISTP>International Solar-Terrestrial Physics DISCIPLINE Space Phy
George Mason - CDAW - 1
Solar Sources of Large Geomagnetic Storms During Solar Cycle 23A. Gopalswamy (NASA/GSFC) B. Michalek, H. Xie, S. Yashiro (CUA) R. A. Howard (NRL)LWS CDAW StormsGMU March 14-16 2005Objective To identify the solar sources of large (Dst < -100
George Mason - CDAW - 1
WG1 + WG4 Joint Session Science Topics: Sun Storm Relationships: 1) How does the probability of observing major magnetic storms change with time, and what is the underlying physics, e.g., - Season (e.g., Is there a seasonal variation in the rate of
George Mason - CDAW - 1
#GMS Date Time DST Org Date Time Spd Loc1996/10/23 05:00 -105 CIR 1997/04/22 00:00 -107 CME 04/16 07:35 87 S30E19 & no radio1997/05/15 13:00 -115 CME 05/12 05:30 464 N21W08 *19970512 0515 19970514 1600 12000 801
George Mason - CDAW - 1
Andrei Zhukov, 09/03/2005Columns of the file events_SW_Sun_AZ.xls:1 - event number2 - event date, year-month-day3 - brief description of the solar wind (SW) geoeffective structures: ICME =Interplanetary CME; CIR = Corotating Interaction Regi
George Mason - CDAW - 1
Event: 48*cme1:2001/11/19 19:54:16 361* 1.19572 111flare:S19E04 C3.6 AR 9704 2001/11/19 20:09**cme2:2001/11/21 14:06:05 518* 1.11228 360flare:S14W19 C4.7 AR 9704 2001/11/21 14:58**cme3:2001/11/22 20:30:33 1443*
George Mason - CDAW - 1
Event: 17*cme1:1998/11/05 02:41:16 568* 2.10587 180flare:N19W11 C5.4 AR 8375 1998/11/05 03:00**cme2:1998/11/06 02:18:05 405* 2.17363 160flare:N19W24 C4.4 AR 8375 1998/11/06 02:43**cme3:1998/11/06 09:54:06 278*
George Mason - CDAW - 1
Event: 27*cme1:2000/07/11 13:27:23 1078* 1.01722 360flare:N18E27 X1 AR 9077 2000/07/11 13:10**cme2:2000/07/12 11:06:05 1124* 1.00315 144flare:N17E27 X1.9 AR 9077 2000/07/12 10:37**cme3:2000/07/14 10:54:07 1674*
George Mason - CDAW - 1
114368543.000 2003 229.20999 229 05 02 23 54.0 51.3 18.1 0.3 114374639.000 2003 229.28055 229 06 43 59 55.2 51.6 18.1 0.3 114380735.000 2003 229.35110 229 08 25 35 56.5 51.8 18
George Mason - CDAW - 1
120667383.000 2003 302.11322 302 02 43 03 32.0 114.7 37.1 1.0 120679555.000 2003 302.25412 302 06 05 55 36.2 115.3 37.1 1.0 120685651.000 2003 302.32468 302 07 47 31 40.4 115.8 37
George Mason - CDAW - 1
mdimovie_casexx.mpg: MDI magnetogram movie (3-day interval). casexx notes event xx.coronalhole_casexx.gif: Upper panel: Configuration of magentic field inferred by a Potential Field Source Surface model (PFSS) using a Wilcox
George Mason - CDAW - 1
153067292.000 2004 312.11218 312 02 41 32 29.1 313.6 0.0 0.0 153073388.000 2004 312.18274 312 04 23 08 30.9 314.3 0.0 0.0 153079483.000 2004 312.25327 312 06 04 43 33.5 315.0 0
George Mason - CDAW - 1
Event: 26
George Mason - CDAW - 1
Event: 10
George Mason - CDAW - 1
Event: 14
George Mason - CDAW - 3
WG3 Ionospheric Storms Summary ReportThe main overarching science question in WG3 was:"How does the TEC respond to geomagnetic storms, and what are the physical mechanisms that control the response. An initial series of sub-questions were assemble
George Mason - CDAW - 4
Questions for Working Group 4: Forecasting Magnetic StormsProbabilistic MethodsGeometric properties of magnetic storms How do we define the occurrence of a magnetic storm? How does the probability of observing a magnetic storm change
George Mason - CDAW - 3
WG3/2 Joint Session Science Questions WG2/3 joint session science questions (Tuesday AM): 1. What is controlling the response of the penetration electric field to the expansion of the convective electric field and the degree of shielding/overshieldin
George Mason - CDAW - 3
From Tim.Fuller-Rowell@noaa.gov Wed Mar 9 11:17:45 2005Return-Path: <Tim.Fuller-Rowell@noaa.gov>Received: from cripplecreek.sec.noaa.gov (cripplecreek.sec.noaa.gov[140.172.225.11]) by sv01.scs.gmu.edu (8.13.1/8.12.8) with ESMTP idj29GHiJi01928
George Mason - CDAW - 4
From rmcpherron@igpp.ucla.edu Sat Feb 19 21:55:27 2005Return-Path: <rmcpherron@igpp.ucla.edu>Received: from terra.igpp.ucla.edu (terra.igpp.ucla.edu [128.97.94.1]) bysv01.scs.gmu.edu (8.12.11/8.12.8) with ESMTP id j1K2tQm8002286 for<jiez@scs.gm
George Mason - CDAW - 3
DOY UTH Longitude LTH orbit 299 22.9330 69.1257 3.54135 10197 300 0.549622 44.5481 3.51950 10198 300 2.17044 20.1346 3.51275 10199 300
George Mason - CDAW - 3
Introduction by Attila Komjathy-Colleagues,In the corresponding directories below you will find the JPL GPS-derived TEC data in the *.dump files. Please find below the description of the individual columns. We also generated VTEC movies using
George Mason - USE - 556
CLASS 9 USE 650 - Environmental Law EPA and OSHA Regulation of Asbestos Background a s Asbestos is a naturally occurring mineral Properties: incombustibility, noise absorption, and resistance to electrical current, corrosion, and bacterial attack Use
George Mason - CS - 112
Here are some practice questions! If you are unsure ofthe answers, type these programs in and try them!(Answers to 14 and 15: 14. A 15. C)1. What are the bugs in the following program (at least 4):#include <iostream.h>void Main(){int numb
George Mason - CS - 112
Quiz 1 Study GuideDisclaimer: Study Guides are provided as an aid only andare not comprehensive.Chapter 1-programming languages and compilerssalient history noteshardware and software fundamentalsalgorithms and problem solvingChapter 2--
George Mason - CS - 112
Assignment 4-Classes due by midnight, 4/6Read chapter 6 before starting.Introduction-Write a program to play a treasure hunt game. Generaterandom numbers to create the coordinates for the buriedtreasure. The user is allowed MAXTRIES gues
George Mason - CS - 112
CS 112 Spring 2002 Programming Assignment 6Due by midnight, 5/4Note: no late work will be accepted after midnight 5/7.Linked lists - read chapter 14 before beginning-A printer "queue" is a list of print jobs waiting toprint. Your job is to i
George Mason - CS - 112
Given:struct record /declared a record structure to be used in a linked list{string name;int id;record * next; /pointer field used to store the address of/another record};typedef record * recordPtr; /declares a type that can be used
George Mason - CS - 112
Clue 5Your name:Your lab section number: 2_Type pwd and make note of the current directory. Copy this file to your directory. Do this by typing:cd (where are you now?)cp /pub/ftp/amarchan/cs112/practice/clue5J.txt .(. is a short
George Mason - CS - 112
Computer Science Department Honor Code Policy for Programming ProjectsUnless otherwise stated, at the time that an assignment or project isgiven, all work handed in for credit is to be the result of individual effort. (In some classes group
George Mason - CS - 112
From daemon Tue Feb 4 11:49:51 1997Received: from portal.gmu.edu by osf1.gmu.edu; (5.65v3.2/1.1.8.2/07Sep94-1001AM/GMUv3)id AA27289; Tue, 4 Feb 1997 11:49:38 -0500Received: from localhost by gmu.edu; (5.65v3.2/1.1.3.9/GMUv7)id AA13036; Tue, 4