Observations of Mesoscale and Microscale Space Weather Processes on - - PowerPoint PPT Presentation

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Observations of Mesoscale and Microscale Space Weather Processes on - - PowerPoint PPT Presentation

Observations of Mesoscale and Microscale Space Weather Processes on the Canadian CASSIOPE Enhanced Polar Outflow Probe (e-POP) Andrew W. Yau 1 , H. Gordon James 2 1 University of Calgary, Canada 2 Communications Research Centre, Canada e-POP


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Andrew W. Yau1, H. Gordon James2

1University of Calgary, Canada 2Communications Research Centre,

Canada

Observations of Mesoscale and Microscale Space Weather Processes on the Canadian CASSIOPE Enhanced Polar Outflow Probe (e-POP)

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CASSIOPE

e-POP Science Payload: to study space storms – plasma outflows, radio propagation, aurora, and ionosphere non-uniformities Small-Sat Bus: Generic, low-cost satellite bus to address needs of future Canadian small-satellite missions Cascade Technology Payload: to demonstrate high bandwidth store-and- forward data delivery

= + +

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Outline

  • 1. e-POP Science Targets

Physics of space weather effects in ionosphere-thermosphere

  • 2. Meso-/Micro-scale Space Weather Processes

Existing Observations

  • 3. e-POP Instruments & Measurements
  • 4. Planned e-POP Studies of Space Weather Processes
  • 5. Conclusions
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e-POP Science Targets

Physics of space weather effects is overarching theme.

  • Ion acceleration and outflow

Meso-scale outflow; micro-scale wave particle interaction

  • Ionospheric irregularities and scintillations

3D irregularities; GPS occultation

  • Effects on radio wave propagation

Trans-ionospheric radio wave propagation

  • Thermospheric expansion

Thermosphere heating, composition changes, and escape

  • Aurora

Small-scale auroral and auroral current structures

SuperDARN GPS

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  • 2. Meso-scale and micro-scale

space weather processes

Existing Observations

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Thermal and Suprathermal Ion Outflows

Observations (Cully et al. 2003) Suprathermal (>10 eV) >16000 km (DE-1) Suprathermal (>15 eV) < 9000 km (Polar) Thermal (<20 eV) <9000 km; (Akebono) Physical Significance Outflow rate increases >10-fold at high Kp Significant H+ acceleration above 9000 km Significant O+ acceleration below 9000 km

Large-scale depletion of ionosphere!? Space weather effects?

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Ion Heating and Lower Hybrid Solitary Structure

Observations 10- to 100-m ion heating and lower hybrid solitary structures Transversely accelerated ions

Heated ions at several eV 63±25 m width

LHSS signatures

Density depletion ∼15%; ∼10 ms Associated w/ TAI and/or BB VLF

Physical Significance Large field and acceleration at small scale Affect larger-scale space weather effects?

40 ms

Ion distributions at 980 km (Burchill et al., 2004) “Spikelet” electric fields at ~600 km (LaBelle et al. 1986)

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Small-scale Auroral Structures

<Wavelength> = 4 km

415 curls Maxium: 18 km

<Speed> = 10 km/s

311 non-zero velocity curls IBC III/IV: 13 km/s IBC I/II: 6 km/s Maximum: 90 km/s

<Lifetime> = 2.3 s

301 curls IBC III/IV: 0.9 s IBC I/II: 4.8 s Maximum 46 s

← 10.1 km→

Observations Auroral spatial scales: 10-100 km (bands), to 0.1-1 km (curtains) Auroral curls Scale ∼ 4 km; ∼2 s Anti-clockwise rotation; 10 km/s Physical Significance Are small (sub-km) structures important?

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Thermospheric Response to Magnetic Storms

Observations Thermosphere expansion (temperature and density increase) in magnetic storms Equatorial propagation of expansion More localized response to substorms Physical Significance Large neutral wind; composition change Anomalous orbit decay in polar LEO

From CHAMP at 410 km (Sutton et al. 2005)

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  • 3. e-POP Instruments and

Measurements

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e-POP Mission Approach

In-situ, small-scale plasma, waves, fields at highest resolution Radio wave propagation: ionospheric irregularities in 3D Fast imaging of meso-scale auroral morphology Polar orbit in key transition region (325 × 1500 km; 80° inclination) 3-axis stabilized S/C for imaging and high-resolution measurements Large data capacity (TB storage, >10GB/day, >300 Mbps downlink)

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e-POP Instrument Principal Investigators

  • Dr. Paul Bernhardt

Naval Research Laboratory, USA CER Coherent EM radio tomography

  • Dr. Richard Langley

University of New Brunswick GAP GPS attitude/profiling experiment

  • Dr. Donald Wallis

Magnametrics and University of Calgary MGF Magnetic field instrument

  • Dr. Gordon James

Communications Research Centre RRI Radio receiver instrument

  • Drs. Sandy Murphree and Leroy Cogger

University of Calgary FAI Fast auroral imager

  • Dr. Hajime Hayakawa

JAXA/ISAS, Japan NMS Neutral mass/velocity spectrometer

  • Dr. David Knudsen

University of Calgary SEI Suprathermal electron imager

  • Dr. Peter Amerl

University of Calgary IRM Imaging ion mass spectrometer

Principal Investigator Science Instrument

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e-POP Plasma Outflow Instruments:

IRM, SEI, NMS, MGF will measure ions, electrons, neutrals, and electrical currents. ions Space storm results in electrical current and plasma outflow in the ionosphere. Electrons neutrals

IRM SEI MGF NMS

electrons

will measures ions, electrons, and neutrals at up to 10-ms resolution

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  • 4. Planned e-POP Studies of

Space Weather Processes

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Examples of Planned e-POP Studies

  • Detailed dynamical characteristics of polar wind; Role of escaping

atmospheric photoelectrons

  • Exosphere neutral outflows: Role of polar wind, charge exchange,

and other acceleration processes

  • Micro-scale ion heating/energization characteristics: Connections

between aurora, ion energization and upflow

  • Wave particle interaction associated with ion energization: detailed

wave propagation characteristics

  • Plasma instabilities: creation of F-region density structure, growth

and saturation of instabilities, constraints on flow

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Planned e-POP Observations and Studies

  • In-situ Observations*

– Plasma, Neutral, Magnetic Field Radio (Electric Field) – Optical (IR and visible) imaging – Radio occultation (GPS, beacon)

  • Coordinated ground observations*

– Radio: SuperDARN, CADI etc – Others: CGSM, … – Active Experiment: HAARP etc

  • Data assimilation and modeling*

– Kinetic, MHD, …

* Collaborative opportunities being pursued

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E-POP Science Team & Participating Organizations

Communications Research Centre: HG James, P Prikryl Royal Military College: JM Noel

  • U. Alberta: R Rankin, C Watt
  • U. Athabasca: M Connors
  • U. Calgary: P Amerl, L Cogger, E Donovan, D Knudsen, JS

Murphree, T Trondsen, D Wallis, A Yau

  • U. New Brunswick: A Hamza, PT Jayachandran, D Kim, R Langley
  • U. Saskatchewan: G Hussey, S Koustov, G Sofko, JP St Maurice
  • U. Victoria: R Horita
  • U. Western Ontario: L Kagan, J MacDougall

York U: J Laframboise, J McMahon JAXA/ISAS, Japan: T Abe, H Hayakawa, K Tsuruda NRL, USA: P Bernhardt, C Siefring UNH, USA: M Lessard