Earth’s Magnetosphere NASA Goddard Space Flight Center

Slides:



Advertisements
Similar presentations
ASEN 5335 Aerospace Environments -- Magnetospheres
Advertisements

Recap and Space Weather In the Magnetosphere (II) Yihua Zheng June 5, 2013 SW REDI.
Anti-Parallel Merging and Component Reconnection: Role in Magnetospheric Dynamics M.M Kuznetsova, M. Hesse, L. Rastaetter NASA/GSFC T. I. Gombosi University.
4/18 6:08 UT 4/17 6:09 UT Average polar cap flux North cap South cap… South cap South enter (need to modify search so we are here) South exit SAA Kress,
Formation of the Magnetosphere 1 Solar Wind. Formation of the Magnetosphere 2 Solar Wind Bow Shock Magnetosheath.
ESS 7 Lecture 14 October 31, 2008 Magnetic Storms
Magnetopause flow vortices revealed during high speed solar wind streams Mona Kessel (NASA GSFC), Yaireska Collado-Vega (University of Puerto Rico), Xi.
Space Weather. Coronal loops Intense magnetic field lines trap plasma main_TRACE_loop_arcade_lg.jpg.
Solar wind interaction with the comet Halley and Venus
Solar wind-magnetosphere coupling Magnetic reconnection In most solar system environments magnetic fields are “frozen” to the plasma - different plasmas.
Earth’s Radiation Belt Xi Shao Department of Astronomy, University Of Maryland, College Park, MD
Storm-Time Dynamics of the Inner Magnetosphere: Observations of Sources and Transport Michelle F. Thomsen Los Alamos National Laboratory 27 June 2003.
O. M. Shalabiea Department of Physics, Northern Borders University, KSA.
Or A Comparison of the Magnetospheres between Jupiter and Earth.
Reinisch_ Solar Terrestrial Relations (Cravens, Physics of Solar Systems Plasmas, Cambridge U.P.) Lecture 1- Space Environment –Matter in.
Lecture 3 Introduction to Magnetic Storms. An isolated substorm is caused by a brief (30-60 min) pulse of southward IMF. Magnetospheric storms are large,
CISM Advisory Council Meeting 4 March 2003 Magnetospheric Modeling Mary K. Hudson and the CISM Magnetospheric Modeling Team.
Magnetospheric Morphology Prepared by Prajwal Kulkarni and Naoshin Haque Stanford University, Stanford, CA IHY Workshop on Advancing VLF through the Global.
Center for Space Environment Modeling W. Manchester 1, I. Roussev, I.V. Sokolov 1, 1 University of Michigan AGU Berkeley March.
EFFECTS of the TERRESTRIAL MAGNETOSPHERE on RADIATION HAZARD on MOON MISSIONS R. Koleva, B. Tomov, T. Dachev, Yu. Matviichuk, Pl. Dimitrov, Space and Solar-Terrestrial.
Magnetometer Tutorial PowerPoint March, 2007 THEMIS: The Science Behind Magnetometer Signatures Laura Peticolas GEONS workshop.
RT Modelling of CMEs Using WSA- ENLIL Cone Model
S. Elkington, June 11, 2009 An overview of Earth’s magnetosphere and its coupling with the solar wind Scot R. Elkington LASP, University of Colorado
Recap and Space Weather In the Magnetosphere (II) Yihua Zheng June 5, 2014 SW REDI.
The Sun and the Heliosphere: some basic concepts…
D. Sibeck, R. Millan, H. Spence
Introduction to Space Weather
Finite Gyroradius Effect in Space and Laboratory 1. Radiation belt (Ring current) 2. Auroral phenomena (Substorm current) 3. Shock acceleration and upstream.
Space Weather from Coronal Holes and High Speed Streams M. Leila Mays (NASA/GSFC and CUA) SW REDISW REDI 2014 June 2-13.
National Aeronautics and Space Administration NASA Goddard Space Flight Center Software Engineering Division Overview of Significant SWx Events.
Response of the Polar Cusp and the Magnetotail to CIRs Studied by a Multispacecraft Wavelet Analysis Axel Korth 1, Ezequiel Echer 2, Fernando L. Guarnieri.
Sun, Moon, Earth, How do they work together to help life survive? Magnetosphere.
Nowcast model of low energy electrons (1-150 keV) for surface charging hazards Natalia Ganushkina Finnish Meteorological Institute, Helsinki, Finland.
9 May MESSENGER First Flyby Magnetospheric Results J. A. Slavin and the MESSENGER Team BepiColombo SERENA Team Meeting Santa Fe, New Mexico 11 May.
Global Simulation of Interaction of the Solar Wind with the Earth's Magnetosphere and Ionosphere Tatsuki Ogino Solar-Terrestrial Environment Laboratory.
Space Weather: Magnetic Storms 31 October 2011 William J. Burke Air Force Research Laboratory/Space Vehicles Directorate Boston College Institute for Scientific.
Earth’s Magnetosphere — A very quick introduction Weichao Tu - LASP of CU-Boulder CEDAR-GEM Joint Workshop - Santa Fe, NM - 06/26/2011.
Space Environment SSE-120 Please type in your questions and raise your hand so we can answer it during class.
Response of the Magnetosphere and Ionosphere to Solar Wind Dynamic Pressure Pulse KYUNG SUN PARK 1, TATSUKI OGINO 2, and DAE-YOUNG LEE 3 1 School of Space.
Energy conversion at Saturn’s magnetosphere: from dayside reconnection to kronian substorms Dr. Caitríona Jackman Uppsala, May 22 nd 2008.
Introduction to Space Weather Jie Zhang CSI 662 / PHYS 660 Fall, 2009 Copyright © Magnetosphere: Geomagnetic Activties Nov. 5, 2009.
PARTICLES IN THE MAGNETOSPHERE
1 Space technology course : Space Radiation Environment and its Effects on Spacecraft Components and Systems Space radiation environment Space Radiation.
Publications in Comparative Magnetospheres Siscoe, G. L.: Towards a comparative theory of magnetospheres, in Solar System Plasma Physics, Vol. II, edited.
Space Weather in Earth’s magnetosphere MODELS  DATA  TOOLS  SYSTEMS  SERVICES  INNOVATIVE SOLUTIONS Space Weather Researc h Center Masha Kuznetsova.
NASA NAG Structure and Dynamics of the Near Earth Large-Scale Electric Field During Major Geomagnetic Storms P-I John R. Wygant Assoc. Professor.
Magnetic reconnection in the magnetotail: Geotail observations T. Nagai Tokyo Institute of Technology World Space Environment Forum 2005 May 4, 2005 Wednesday.
What is a geomagnetic storm? A very efficient exchange of energy from the solar wind into the space environment surrounding Earth; These storms result.
The large scale convection electric field, ring current energization, and plasmasphere erosion in the June 1, 2013 storm Scott Thaller Van Allen Probes.
The effects of the solar wind on Saturn’s space environment
Storm-dependent Radiation Belt Dynamics Mei-Ching Fok NASA Goddard Space Flight Center, USA Richard Horne, Nigel Meredith, Sarah Glauert British Antarctic.
ASEN 5335 Aerospace Environments -- Magnetospheres 1 As the magnetized solar wind flows past the Earth, the plasma interacts with Earth’s magnetic field.
Earth’s Magnetosphere Space Weather Training Kennedy Space Center Space Weather Research Center.
On-Line Visualization Ring Current / Radiation Belt.
Source and seed populations for relativistic electrons: Their roles in radiation belt changes A. N. Jaynes1, D. N. Baker1, H. J. Singer2, J. V. Rodriguez3,4.
The Magnetosphere Feifei Jiang, UCLA
ARTEMIS – solar wind/ shocks
Global MHD Simulations of Dayside Magnetopause Dynamics.
Introduction to Space Weather Interplanetary Transients
Date Day Topic Instructor Due
Effects of Dipole Tilt Angle on Geomagnetic Activities
Solar Wind Transients and SEPs
The Not-So-Calm After the Storm:
Extreme Events In The Earth’s Electron Radiation Belts
Introduction to Space Weather
Introduction to Space Weather
Magnetosphere: Bow Shock Substorm and Storm
Richard B. Horne British Antarctic Survey Cambridge UK
Added-Value Users of ACE Real Time Solar Wind (RTSW) Data
Magnetosphere: Structure and Properties
Presentation transcript:

Earth’s Magnetosphere NASA Goddard Space Flight Center Presented by: Dr. Yaireska (Yari) Collado-Vega Space Weather Research Center CCMC/SWRC SW REDI 2015 NASA Goddard Space Flight Center In this presentation I will be talking about the Sun and its activity in relations to the space weather (http://iswa3.ccmc.gsfc.nasa.gov/wiki/index.php/Glossary/_space_weather)

Magnetic Field of the Earth The Earth's magnetic field is similar to that of a bar magnet tilted 11 degrees from the spin axis of the Earth. The magnitude of the magnetic field varies over the surface of the Earth in the range 0.3 to 0.6 Gauss. The Earth's magnetic field is similar to that of a bar magnet. The magnitude varies over the surface of the Earth in the range 0.3 to 0.6 Gauss.

Earth’s Magnetic Field (not to scale) Magnetosphere Earth Magnetopause Sub-solar point The solar wind pushes and stretches Earth’s magnetic field into a vast, comet-shaped region called the magnetosphere. The magnetosphere and Earth’s atmosphere protect us from the solar wind and other kinds of solar and cosmic radiation. Solar wind – Earth’s magnetic field field interaction flatten the nose (dayside – towards the sun) and drag field lines to the tail (night-side – away from the sun). The magnetopause separates Earth's magnetic domain from the solar wind and its embedded interplanetary field (IMF). The three-dimensional location of the magnetopause represents a balance of pressures: Pressures of solar-origin (predominantly solar wind flow ram pressure) balance pressures of Earth-origin (predominantly outward magnetic pressure) at the magnetopause. The magnetic field is the shield that protects the Earth from the solar plasma particles because they have difficulty in moving across the magnetic field lines. If the Earth did not have the magnetic field, continuously blowing solar wind and CMEs would most likely wipe out all the life forms on the Earth. Scientists speculate that something like this could have happened on Mars, who lost its magnetic field over the time. The Sun-Earth line cross the magnetopause at the Sub-solar point. Magnetopause stand-off distance is the distance to the magnetopause sub-solar point. Under quiet conditions the magnetopause sub-solar point is about 10 to 12  Earth’s radii away from Earth. 1 RE (Earth’s radius) = 6370 km In dense solar wind or in the presence of a strong and negative solar wind magnetic field component Bz, the magnetopause can move closer and even cross geosynchronous orbit (distance about 6.7 RE). The solar wind pushes and stretches Earth’s magnetic field into comet-shaped region called the magnetosphere. The magnetosphere and Earth’s atmosphere protect us from the solar wind and other kinds of solar and cosmic radiation.

Spatial Scales 1 RE (Earth’s radius) = 6370 km Magnetosphere Earth Distances in Solar Corona are expressed in Solar radii: 1 – 20 RS Solar radius is approximately 100 times larger than the Earth’s radius. Distances in magnetosphere are expressed in Earth radii. During quit solar wind conditions the sub-solar point of the magnetosphere boundary is at about 10 RE from the Earth. The tail width is about 30-40 RE,.The tail length is 1000s RE The distance to the moon is about 60 RE, 1 RE (Earth’s radius) = 6370 km 1 RS (Solar radius) ~ 110 RE 1 AU (Distance between the Sun and the Earth ) ~ 215 RS

Magnetosphere for Southward and Northward IMF Orientation Magnetic Reconnection

Magnetosphere: Northward IMF X: Earth to Sun Z: South to North Z X Sun Red lines (closed): Magnetic field (MF) lines with both ends connected to the Earth Black lines (open): MF lines with only one end a the Earth Blue lines (interplanetary): MF lines with both ends in the interplanetary space

Magnetosphere: Southward IMF Red lines (closed): Magnetic field (MF) lines with both ends connected to the Earth Black lines (open): MF lines with only one end a the Earth Blue lines (interplanetary): MF lines with both ends in the interplanetary space

in Different Cut Planes Magnetosphere in Different Cut Planes meridional cut Y=0 Bow shock equatorial cut Z=0 Bow shock Magnetotail Magnetopause Magnetotail current sheet cross-tail cut X= -15 RE

Magnetosphere: Quiet vs. Compressed Geosynch. orbit Magnetopause

Inner Magnetosphere (up to ~ 10 RE) APL Van Allen Belts 400 keV – 6 MeV 1 nT = 10 -5 Gauss Plasmasphere 1-10 eV Ring Current 1-400 keV

Inner Magnetosphere Plasmas

Electron Total Flux. Energy 63.3 keV. Color Contour Equatorial Plane Magnetopause Geosynch. Orbit Sun Earth radius

Ring Current: Quiet vs. Active

Horne et al., 2007, Nature Physics

Magnetic Storms

Substorms

Lagrange Point – L1 Advanced Composition Explorer The Lagrangian points (/L-points) are the five positions in an orbital configuration where a spacecraft affected only by gravity can maintain its position relative to the two massive bodies (the Earth and the Sun). You can almost fit 1 solar diameter (~ 200 RE ) between the Earth and L1. Solar wind monitor ACE is positioned at L1 point. It takes about 30 – 60 min (depending on the speed of the solar wind) for the disturbance observed at L1 to reach the Earth. L1 (Solar Wind Monitor ACE location): ~ 200 RE sunward You can fit 1 Sun between the Earth and L1. 2 RS (Solar diameter) ~ 220 RE

Solar Wind Speed at ACE

Solar Wind Parameters at ACE on 04/05/2010 Magnetic field Bx, By, Bz nT X: Earth to Sun Z: North to South Velocity km/s 1 nT = 10 -5 Gauss Density part/cm3

Magnetopause Stand-off Distance Degree of compression of MP due to dynamic pressure of solar wind March 17, 2015

Kp index "planetarische Kennziffer" ( = planetary index). Geomagnetic activity index - range from 0-9 disturbance levels of magnetic field on the ground – currents Threshold Kp>=6 The Kp index indicates the magnitude of geomagnetic disturbance on a 0-9 scale, with zero being very quiet and 9 indicating a major geomagnetic storm. The index has a three-hour cadence. Higher values of Kp are associated with geomagnetic storming

Electron Flux Enhancement HSS and Radiation Belt Electron Flux Enhancement NASA/GSFC, internal use only :-)

Energetic Proton Flux >10 MeV flux by GOES spacecraft Threshold: 10 pfu >100 MeV flux by GOES spacecraft Threshold: 1 pfu

Watch the video http://missionscience.nasa.gov/sun/sunVideo_04magnetosphere.html The Earth's magnetic field is similar to that of a bar magnet tilted 11 degrees from the spin axis of the Earth. The magnitude of the magnetic varies over the surface of the Earth in the range 0.3 to 0.6 Gauss.

iSWA Layout: 07/12/2012 http://goo.gl/V0JjxV