Satellite Observations of Nonlinear Interactions of High Power Interactions of in the Ionosphere

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    Satellite Observations of NonlinearInteractions of in the Ionosphere

    Carl L. Siefring, Paul A. Bernhardt

    Plasma Physics Division, Naval Research Laboratory

    Washington, DC 20735

    Todd Pedersen, Air Force Research Laboratory

    Kirtland AFB, NM

    Andrew Yau, Department of Physics and Astronomy

    Institute for Space Research

    University of Calgary, Calgary, Canada

    Jan Bergman, IRFU, Upsalla, Sweden

    Hanna Rothkeahl, Space Research Centre, Polish Academy of

    Sciences, Warsaw, Poland

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    CubeSat Observations at 300 km Altitude

    HF Signal from High Power Radio Waves

    Near Vertical Transmissions

    Reflected Below F-Layer Peak

    Low Altitude Expendable Satellites Needed

    Ionospheric Modification Effects

    High Power Radio Waves

    Enhanced Electron Densities

    Elevated Energetic Electron Fluxes

    Plasma Wave Generation

    ELF/VLF Wave Detection

    Spacecraft Opportunities

    Canadian ePOP

    NRL MiniHFR

    Swedish PSI

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    Satellite Observations of CurrentIonospheric Modification Facilities

    Jicamarca

    Arecibo

    Conjugate

    SatelliteOrbit

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    Arecibo HF Facility Antenna Gain at

    8.175 MHz Giving 220 MegaWatts ERP

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    IncoherentScatter

    Observations

    of F-RegionHeating

    Showing

    IonosphericHole

    Scatter From IonAcoustic Waves

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    In Situ

    Measurementsby NRL IFH

    Rocket

    Electron

    DensityCavities

    fplasma ~ fpump

    HighFrequency

    WaveSpectrum

    LowFrequency

    WaveSpectrum

    Reference:Bernhardt, Siefring,Rodriguez, Haas,

    Baumback, Romero,Solin, Djuth, Duncan,

    Pollack, Sulzer,The ionospheric

    focused heating

    experiment,J. Geophys. Res., 100,17,331-17,345, 1995.

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    Electron Acceleration and Irregularity Formation 2ndHarmonic of the Electron Cyclotron Frequency

    HAARP ArtificialAurora

    2.85 MHz

    3.6 MWTransmitterPower

    March 2009

    Artificial PlasmaLayers

    2nd HarmonicResonance

    ElectronBernstein WaveAcceleration

    Ref.: ToddPedersen (AFRL)

    A ifi i ll P d d Pl L

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    Artificially Produced Plasma LayersNear 200 km Altitude

    Source: Todd Pedersen et al. 3009, Creation of ArtificialIonospheric Layers Using HighPower HF Waves

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    HAARP Instrument Experiments withInstrumented Satellites

    HAARPFacility

    PERCSOrbit

    HAARPHF Beam

    HAARP Antenna Array

    PERCS Operational Utility

    Absolute Measurement of HAARP Antenna Pattern from 2.8 to 10 MHz Precise Measurements of Plasma Waves Generated by HAARP

    Satellite

    Orbit

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    Satellite Support of Nonlinear

    Excitation of the Ionosphere

    High Power Radio Waves

    Stimulated Electromagnetic and ElectrostaticEmissions (SEE) for Radio Receiver

    Instrument (RRI) Electron Acceleration

    Enhanced Airglow

    Ion Acceleration Electron Density Irregularities

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    Cassiope

    Anti-Ram Face

    BoomsDeployed

    SEI

    CERTO

    MGF

    IRM

    RRI

    CASCADE

    Horn

    FOV

    RAM

    Star Trackers

    GAP-O Antenna

    Cassiope

    Anti-Ram Face

    BoomsDeployed

    SEI

    CERTO

    MGF

    IRM

    RRI

    CASCADE

    Horn

    FOV

    RAM

    Star Trackers

    GAP-O Antenna

    e-POP/CASSIOPEMicro-Satellite:

    Instrument Payload

    Imaging particle instruments forunprecedented resolution on satellites

    IRM: Imaging rapid ion massspectrometer

    SEI: Suprathermal electron imager

    NMS: Neutral mass and velocityspectrometer

    Auroral imager and wave receiver-transmitter for first micro-satellite

    measurements FAI: Fast auroral imager

    RRI: Radio receiver instrument

    CERTO: Coherent electromagneticradio tomography

    Integrated instrument control/datahandling, and science-quality orbit-attitude system data to maximizescience return

    MGF: Magnetometer

    GAP: Differential GPS Attitude and

    Position System

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    ePOP CASSIOPE Mission Overview Inclination: 80 Degrees

    Orbit: 300 x 1500 km Lifetime: > 1 Year Initial Apogee Over Northern Latitudes Orbit Decay Over 2 Years

    110 km at Apogee 12 km at Perigee Initial Argument of Perigee: 270 degrees

    Launch: Late 2012

    3-Axis Agile Spacecraft Noon/Midnight Orbit 2 kRad per year with 0.0825 Inch Shielding Spacecraft Critical Design Review April 2005

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    100 Hz to 18 MHz

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    Earth Coverage by ePOP/CASSIOPEin a 80 Inclination ORBIT

    HAARP

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    Space-Based, Diagnostic Requirements forHAARP Measurements

    Measurement Importance Diagnostic ePOP Instrument

    ELF/VLF Waves Very High Receiver Covering1 Hz to 30 kHz

    RRI10 Hz to 30 kHz

    Field Aligned VLF DuctsArtificial and Natural

    High In SituElectronDensity Probe

    SEI(102 to 106 cm-3)

    Elevated F-RegionElectron Temperature

    as Duct Signature

    Moderate Thermal ElectronDetector 0.0 to 0.3 eV

    SEI(0 to 200 eV)

    Optical Emissions fromPrecipitation

    Moderate Photo DetectorN21P, 630, 557.7,427.8, 777.4 nm

    FAI(630 to 850 nm)

    Suprathermal ElectronFluxes

    Moderate Energetic ElectronDetector

    SEI(0 to 200 eV)

    Modulated HAARPPump Wave

    Moderate HF Receiver/Antenna(3 to 9 MHz)

    RRI(1-18 MHz, 30 kHz

    Bandwidth)

    Note: RRI = Radio Receiver Instrument, SEI = Suprathermal Electron Imager, FAI = Fast Auroral Imager,

    CERTO = Coherent Electromagnetic Radio Tomography, IRM = Rapid Ion Mass Spectrometer

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    EPOP Booms Deployed

    (Looking at underside of lower deck plate)

    Nadir

    Ram

    IRM Boom

    SEIBoom

    CERTO

    Boom

    MGF Boom

    RRI Boom

    Base Deck

    Plate

    I h i H ti Si l ti

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    Ionospheric Heating Simulationson Field Line Above Transmitter

    3 3.5 4 4.5 5 5.5 6

    2

    3

    4

    5

    3 3.5 4 4.5 5 5.5 6

    250

    500

    750

    1000

    1250

    1500

    1750

    2000

    3 3.5 4 4.5 5 5.5 6

    250

    500

    750

    1000

    1250

    1500

    1750

    2000

    3 3.5 4 4.5 5 5.5 6

    250

    500

    750

    1000

    1250

    1500

    1750

    20003 3.5 4 4.5 5 5.5 6

    1.5

    2

    2.5

    3

    3 3.5 4 4.5 5 5.5 6

    1.5

    2

    2.5

    3

    3.5

    2000

    1500

    1000

    500

    2000

    1500

    1000

    500

    2000

    1500

    1000

    500

    5.0

    4.0

    3.0

    2.0

    3.0

    2.5

    2.0

    1.5

    3.5

    3.0

    2.5

    2.0

    1.5

    ElectronDensity

    (104

    cm-3)

    ElectronTemperature

    (103

    K)

    IonTemperature

    (103

    K)

    0300 0330 0400 0430 0500 0530 0600

    Local Time (Hours-Minutes)

    0300 0330 0400 0430 0500 0530 0600

    Local Time (Hours-Minutes)

    Electron Density

    ElectronTemperature

    IonTemperature

    1 HourHeatingPeriod

    1 HourHeatingPeriodSatellite

    Altitude

    Altitude(km)

    Altitude(km)

    Altitude(km)

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    JOINT CERTO and GPS-GAPOPERATIONS ON CASSIOPE

    From GPS

    Satellite

    Ground Receivers

    A i E i POP E i M d

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    Active Experiments ePOP Experiment ModesPaul A. Bernhardt, NRL

    Experiment

    Instrument

    Modulated

    HeaterWave

    Generation(MHWG)

    HF

    HeaterArtificialAurora(HAA)

    HF Heater

    StimulatedElectromagneticEmission (SEE)

    HF Heater

    PlasmaTemperature

    Enhancements(PTE)

    RRI VLF/ELF 0~5 MHz 0~5 MHz HF WavesSEI Yes WPI WPI IonMode

    FAI No Yes No NoCER No CERALLC No No

    IRM No No No IRMTISNMS No No No No

    GAP No No No No

    MGF No No No NoAltitude

    Requirements< 800 km < 800 km < 350 km Any

    Pointing At Event At Event Event Z-Nadir

    Note: RRI = Radio Receiver Instrument, SEI = Suprathermal Electron Imager, FAI = Fast Auroral Imager,

    CERTO = Coherent Electromagnetic Radio Tomography, IRM = Rapid Ion Mass Spectrometer, GAP =

    Differential GPS Attitude and Position System, MGF = Magnetometer

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    Miniature HF Receiver(MiniHFR)

    Miniature HF Receiver

    Power: 5 and 3.3 V available @ 5 W total power (continuous operation)

    Volume 3 boards = 3 to 5 cm of stack

    Mass 800 g

    Pointing accuracy need 20 deg (dependent on link margin analysis) Pointing direction

    highest gain of antennas collinear with the ram direction

    highest gain in nadir direction for receiving ground beacons

    Shadowing/ field of view/aperture size no deployables within thehighest gain of antennas

    TT&C need through C&DH/Radio and down to the ground TBD bps

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    GEOMETRY FORHF CubeSat MEASUREMENTS

    Miniature HF

    RECEIVER

    LEO ORBIT

    N

    S

    Ground HFTransmitters

    Ionosphere

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    Amp

    Amp

    Amp

    Amp

    HighImpedance

    Antennas

    CubeSat

    Buss

    MiniHFR Design

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    CubeSat Implementation of MiniHFR

    MiniHRFReceiver

    30 cm

    10 cm

    19 cm

    ShortAntenna

    To Ground HF Receivers

    10 cm

    StowedConfiguration

    ADC B1

    DSP B2

    HF

    ReceiverBoards

    (a) (b)

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    CubeSat Payload Guide

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    IRFUUppsala

    PSIPlasmaScience

    Instruments

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    EFVS for PSI

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    Deployable Electric FieldAntenna

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    LP for PSI

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    SMILE for PSI

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    SRC Ultra-Lightweight AntennaHanna Rothkeahl, Space Research Centre, Polish Academy of Sciences,

    Bartycka 18A, Warsaw, Poland 00-716

    SRC Ultra Lightweight Antenna

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    SRC Ultra-Lightweight Antenna

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    Summary

    High Power HF Waves in the Ionosphere Nonlinear Wave Interactions

    In Situ ES and EM Wave Generation High Frequency

    Low Frequency

    MiniSat Sensor Platform ePOP (2012 Launch)

    8 Plasma, Neutral and Wave Sensors

    PicoSat (CubeSat) Sensors NRL Miniature HF Receiver (MiniHFR)

    30 Day Lifetime

    Nano Sat or MicroSat Sensors IRFU PSI

    S C