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Space Weather: The Sun, Magnetosphere, Ionosphere.

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Presentation on theme: "Space Weather: The Sun, Magnetosphere, Ionosphere."— Presentation transcript:

1 Space Weather: The Sun, Magnetosphere, Ionosphere

2 Source of Space Weather / Ionospheric Disturbances: The Sun

3 The Sun: The Sun for a a couple months in 2001 Facts (approximate values): 149 million kilometers away Diameter: 1.4 million km Mass: 2.0x10 30 kg 4.5 billion years old 11 Year sunspot cycle Surface temp. 5,900 K. Rotation Period: 27 days at equator

4 Close-up of a Sun Spot

5 Local Internal Dynamics Animation showing our present understanding Coronal “loops” on the Sun

6 Coronal Mass Ejections Super prominence EUV images of Sun with corona as observed from SOHO

7 Coronal Mass Ejection Causing the Aurora

8 Magnetosphere Other effects include satellite damage, power outages, GPS errors, radio interruptions, etc.

9 The Magnetosphere

10 The Aurora As seen from space As seen in Alaska

11 Solar Flares EUV X-RAY “ White Light ” Extreme Ultraviolet (EUV)X-ray Flare

12 Troposphere Stratosphere Mesosphere Thermosphere D-Region E-Region F 1 -Region F 2 -Region Neutral AtmosphereDaytimeNighttime Height 100 km 200 km 300 km    Mt. Everest

13 Formation of the Ionosphere EUV Light Neutral Atoms Positively Charged Ion Free Electrons, these reflect radio waves Photo-ionization SUN   A (Atom)  A + (Ion) + e - (electron) Photo-ionization occurs when Extreme Ultraviolet (EUV) from the Sun strikes neutral atoms to produce positively charged Ions Types of Atoms: primarily Oxygen & Nitrogen Types of Molecules: O 2, N 2, NO

14 Two Types of Recombination: Molecule A 2   Ion X + Charge Exchange X + + A 2  AX + + A AX + A Dissociation Recombination AX + + e -  A + X o Single Atom A Neutral Atom X Radiative Recombination X + + e -  A + Radiated Energy  A Ion X + e-e- Dissociation recombination, 2 steps: Radiative recombination, 1 step: Electron splits AX + apart

15       When ions are “ let go ” they oscillate in simple harmonic motion at an Angular Frequency   2 = N e 2 /  0 m N = Electron Density e = Charge on electron m = Mass of an electron  0 = Permittivity of free space Angular Plasma Frequency (maximum usable frequency): f N = 2  /  f N = Plasma frequency in Hertz f N 2 = 80.5 NSubstituting Atomic Constants f c  9 x 10 -6 √ N m f c = Critical Frequency, N m = Electron density Reflectivity of the Ionosphere

16 Electron Density vs. Height D - Region 90 Km, Lower following solar flare 1.5x10 4 N e /cm3 (noon) Absent at Night E - Region 110 Km 1.5x10 5 N e /cm3 (noon) 1.0x10 4 N e /cm3 (Night) F1 - Region 200 Km 2.5x10 5 N e /cm3 (noon) Absent at night F2 - Region 300 Km 10 6 N e /cm3 (noon) 10 5 N e /cm3 (Midnight) Source: “ The Ionosphere: Communications, Surveillance, and Direction Finding ” Leo F. McNamara1991 ISBN: 0-89464-040-2

17 Maximum Useable Frequency The Maximum Useable Frequency (MUF) is the largest frequency that can be reflected by the ionosphere at vertical incidence Source: “ The Ionosphere: Communications, Surveillance, and Direction Finding ” Leo F. McNamara1991 ISBN: 0-89464-040-2

18 Variability of the Ionosphere Diurnal (Thru the day) Seasonal (Thru the year) Location (Geographic & Geomagnetic) Solar Activity (Solar Cycles & Disturbances) Height (at different layers) Source: “ The Ionosphere: Communications, Surveillance, and Direction Finding ” Leo F. McNamara1991 ISBN: 0-89464-040-2


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