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Space – based Observations Techniques, Instruments and Missions for the Sun-Earth System Len Culhane Mullard Space Science Laboratory University College London. Introduction.
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Space – based Observations Techniques, Instruments and Missions for the Sun-Earth System Len Culhane Mullard Space Science Laboratory University College London
Introduction • Following a brief discussion of photons and their interaction with Earth’s atmosphere, short wavelength optics and the role of CCDs are reviewed • The difficulties posed by operating in the Space environment are outlined • Several current space solar missions are described and results sumarised • The Sun-Earth connection is discussed including - solar eruptions - nature of magnetic clouds - instruments for in-situ plasma observations - solar wind and CME influence on the Earth’s Magnetosphere
Electromagnetic Spectrum Regions of the Spectrum Quantum nature of radiation: En = hn = hc/l • Radio/Microwave • (Frequency/Wavelength) • → THz, GHz, MHz, cm, m • Infra-red/Sub-mm (Wavelength) → mm, mm • Visible/UV/EUV (Wavelength) → Å, nm • X-ray, g-ray (Photon Energy) → eV 3
Radiation and Particle Interaction in the Earth’s Atmosphere Photon absorption by Earth’s atmosphere • X-rays - E > 50keV, penetrate to • ~30 km above Earth’s surface • - can measure from balloons • In practical terms need to go to • space for these wavelengths • Better observations even for the • optical band (400-1000 nm) • - avoid atmospheric turbulence
Telescope and Spectrometer Optical Design • Normal incidence optical systems used at IR, visible and near-UV wavelengths • EUV and X-ray photons are absorbed by trivial material thicknesses • - for normal incidence, reflectivity R ~ 10- 4 at l ~ 100 Å • - refractive index n ~ 0.995 for typical metals thus allowing Total External Reflection • - for n = 1 – d, the critical angle for external reflection is given by Cos qc=1 – d ~ √2d • - at EUV and X-ray wavelengths, qcis typically 1o to 3o → grazing incidence optics • For angles of glancing incidence, q ≤ qc, rays are reflected • Reflectivity of materials at soft X-ray/EUV wavelengths can be enhanced by the use of multilayer coatings - these operate in a similar manner to Bragg crystal diffraction 5
Optical Configurations for X-ray Reflection • q ≤ qCis a highly restrictive condition for optical designs • - small q value implies figuring and polishing large areas of substrate to achieve only small Aeff • For imaging, the Abbe sine condition must be obeyed • - needs at least two reflections to avoid severe coma for off-axis rays • Wolter Type I design uses successive reflections from confocal paraboloids and hyperboloids • Fields of view of ~ 1o with resolution ≥ 0.5 arc sec represent the present state of the art • Wolter II configuration involves external • reflection from the paraboloid and is used • to feed spectrometers e.g. SOHO CDS, • because of its lower beam divergence at • the focus
Grazing Incidence X-ray Optical System • To increase the small effective aperture at grazing incidenceWolter Type I telescopes are nested • Movie shows schematic operation of the Chandra X-ray Astronomy telescope • Radiation is absorbed at normal incidence but reflected at grazing incidence for q ≤ qc 7
High Z d Low Z Multilayer Coated Optics at Normal and Grazing Incidence • Multilayer coatings allow normal incidence reflectivities ≥ 30% for the range 10 nm < l < 50 nm • Multilayer operation is similar to that of a Bragg crystal spectrometer • - crystal atoms, plane spacing d, diffract X-rays (l) at glancing incidence q following Bragg’s law: nl = 2d sin q • Alternate layers of high and low Z material, with well controlled thickness, are deposited on an optical • substrate – mirror or grating, where d is the thickness of one layer pair • Photons are reflected from thin high Z layers while low Z – low absorption, layers separate the high-Z • layers by appropriate distances with much higher reflectivities possible than for a Bragg crystal • For layer boundaries, RMS roughness of0.6 nm limits • wavelengths at normal incidence to l ≥ 8 nm • At normal incidence, the bandwidth of the reflectance curve • is Dl ~ l/NLP where NLP is number of layer pairs • Increasing NLP reduces Dl and enhances Rpeak • - absorption in the layers sets an eventual limit
EUV Multilayer Instruments for Solar Physics SOHO EIT, TRACE, SDO AIA Hinode/EIS… EUV Imaging Spectrometer 9
Photon Response in Semiconductors - Charge Coupled Devices • Photon absorption with En > EBandGap will lift an electron into the conduction band and create an • electron-hole pair – intrinsic photoconduction • CCD operation uses a Metal Oxide Semiconductor (MOS) structure which acts like a capacitor • CCDs are photon detecting pixel arrays that use intrinsic photoconduction in Si • Response has been extended to En > 10 keV and they have revolutionised Astronomy • With +ve voltage on the p-type Si, majority carrier holes • are repelled and a depletion region, depth d, is swept • free of charge • Incoming photons produce electron-hole pairs and the • electrons are attracted to the insulator under the electrode + Electrode Ground Oxide Insulator e- Depletion Region d hn P-type Si • For backside illumination, physical device depth is etched • or thinned to be as close as possible to d = (2keomrsV)1/2 • For Si resistivity, r ~ 10 – 20 W cm gives d ~ 3 – 10 mm • - complex electrode structure defines pixels and enables charge transfer Ground
Charge Coupled Devices (CCDs) as Photon Detectors • Quantum efficiency: - percentage of photons actually detected is the Quantum Efficiency (QE) of the CCD • Wavelength range: - CCDs have a wide wavelength response from ~ 1 Å (X-ray) to ~ 10,000 Å (Infra- red) with a peak sensitivity at around 7000 Å - use of back-thinning is necessary to extend the CCD wavelength response to shorter wavelengths e.g. EUV and X-ray or l ≤ 500 Å - note that 1 Å = 10 nm and E (keV) = 12.38/l (Å) • Dynamic range: - CCD dynamic range describes the minimum and maximum number of electrons that can be imaged - with more photons incident on the CCD, more electrons are collected in the MOS potential well - when no more electrons can be accommodated in the well, the pixel is saturated. 11
Environmental Challenges in Orbit • Vacuum of Space - contaminants can move from one part of an instrument to another - will preferentially deposit on cold surfaces - can cause serious degradation of optical surfaces particularly at EUV wavelengths - high voltage discharge can occur if instrument is not fully evacuated • Thermal Environment - spacecraft illuminated by Sun on one side (T~6000K) and Earth (T~300K) or space (T~4K) on the other - temperature must be controlled to ~ 10 ± 5 deg C to maintain e.g. optical alignments • Ionizing radiation - electronic components susceptible to radiation damage - radiation-hard devices must be used particularly in high dose orbits - photon and particle detectors can suffer high backgrounds 12
Rocket Launching • Chemical rocket motors (liquid or solid fuel) generally employed - electrical (ion) propulsion being developed for interplanetary missions • Primary cost driver for a launch is the payload e.g. spacecraft, mass • Cost or vehicle performance envelopes will restrict spacecraft size • Instruments will suffer severe vibration and acoustic energy inputs from the rocket motors - pre-flight vibration testing is mandatory • Mechanical shocks will also be present - caused by e.g. first stage separation, rocket motor restarts 14
Telemetry – Spacecraft Data Transmission to Earth • Downlink data rate can be a crucial constraint for solar space observations, - limits the cadence of imaging instruments - reduces the quantity of spectral information • Initial SOHO/EIT telemetry allocation was 1 kilobits/s (1 kbps) - allowed only 6 full-disk images/day but can now operate with ~ 12 minute cadence - SOHO has a standard science telemetry rate of 40 kbs • TRACE employs several different multilayer passbands - has an on-board mass memory of 700 Gbits capacity - manage memory use to achieve partial Sun image cadence of ~30 seconds • SDO has eight multilayer image channels - uses a dedicated ground station at White Sands and transmits at 150 Mbits/s - acquires and transmits eight full-sun images every 10 seconds 15
Choice of Orbit • Low Earth Orbit (LEO) - 200-1200km above Earth with orbital period of 90-100 m - orbit between atmosphere and Van-Allen radiation belts - minimizes the damaging effect of high energy particles • Sun Synchronous Orbit (SSO) - special LEO case at ~ 800km with Sun always in view e.g. TRACE, Hinode • High Earth Orbit (HEO) - above the radiation belts e.g. XMM-Newton, with apogee > 30,000km - more energy and cost to launch • Geosynchronous Orbit (SSO) - same orbital period as the sidereal period of the Earth at an altitude of 42,164 km - full time contact e.g. IUE 16
Sun-Earth Lagrange Points • Quasi-stable orbits can be maintained around the Lagrange points with minimum energy use • L2, on the anti-sun side of earth and • at a distance of 1.5 x 106 km, allows • a spacecraft to run cold (T ~ 50 K) • and to have a relatively unconstrained • view of the Universe • L1, L4 and L5 are suitable for sun-viewing • spacecraft while L2 is useful for Astronomy • L3 is difficult due to communication problems
Solar Remote Sensing • The Sun in X-rays and white light - X-ray emission from the corona is associated with photospheric activity • Access to space is essential for remote sensing observations - atmosphere absorbs X-ray and EUV emission - seeing limits visible spatial resolution to ≥ 1 arc sec for long duration observations • Spaceis also essential for long term observations of • coronal variability • Movie shows SOHO/EIT 195Å images of the corona • for the interval 10 – 23 December, 1999 • - coronal structures vary on timescales of minutes through hours to • months
Sun-Earth Observations • Solar phenomena influencing the near-Earth environment • - Solar Flares • - Coronal Mass Ejections (CMEs) • - Solar Wind • In a flare an unstable magnetic field relaxes to • a lower energy state with released energy • - accelerating particles • - heating plasma • - often causing a filament eruption and a CME • Accelerated high energy particles from the flare can • reach the Earth • CMEs are large outbursts of material detected by • coronagraphs with ~ 1015 g lost from the Sun • In-situ instruments sample the particles and • ejected plasma near the Earth
Solar Minimum pass – 1992/97 Comparison with Solar maximum pass – 1998/2003 Solar Wind Results from Ulysses Spacecraft orbit, established by gravity assist from Jupiter, allowed the first sampling of the Heliosphere out of the ecliptic plane • Near Minimum → • Average wind speed at: • high latitude ~ 700 km/s • (Polar Coronal Holes) • equator ~ 350 km/s • (Equatorial Streamers) • Abrupt transition from low to high speed ← Through Maximum Highly variable flows are observed at all heliolatitudes. Flows arise from a mixture of sources including extended polar holes, streamers, CMEs, small low latitude coronal holes
Advanced Composition Explorer (ACE) NASA mission to study Solar Wind and CMEs • This spacecraft is located at the Lagrange L1 point between Earth and Sun • Includes a set of nine instruments to sample the arriving Solar Wind and CME • plasma close to Earth. It measures in-situ: • - element composition and ion state • - plasma velocity • - particle energies • - magnetic field • Launched in August, 1997, • the spacecraft is still operating • and has fuel to continue at L1 • until ~ 2024
SOHO – cooperative project between ESA and NASA • Spacecraft is also located at the Lagrange L1 point between Earth and Sun • - 1.5 x 106 km from Earth • Includes set of 12 instruments • to study: • - Solar Interior • - Solar Atmosphere • - Extended Corona and particles • ( in-situ) • Launched in December, 1995, • the spacecraft is still • operating
SOHO EUV Imaging Telescope – Use of Multilayer Passbands • EIT has 4 different Mo/Si coatings with layer thicknesses tuned for 175 Å, 195 Å, 284 Å, 304 Å • to observe lines of Fe IX/X, Fe XII, Fe XV and He II • Rotatable quadrant shutter can select each of the four mirror sectors in turn • CHIANTI theoretical spectrum shown with a) 175 Å passband and b) resulting line intensities a) b) 24
TRACE Solar Telescope – Example of Multilayer Application • Schematic of the TRACE EUV telescope is shown below – a 0.3 m Cassegrain system • Primary and secondary mirrors are sectored in four quadrants, three with Mo2C/Si layers • Quadrant shutter allows one sector at a time to view the Corona and register images on the • CCD in the appropriate passband • Reflectivity curves are shown for two of the three quadrants – peaks at 173 Å and 195 Å • Mo2C/Si layers have enhanced performance • compared to Mo/Si
EUV Corona - TRACE Images • The four TRACE passbands obtain images of the • photosphere, chromosphere and corona for • 5000 K ≤ Te ≤ 4 MK • - image cadence:30s • - pixel size: 0.5 arcsec • - FoV: 8.5 arcmin x 8.5arcmin Fe IX 171 1 MK TRACE: AR Loops on 06 NOV 1999 H I Ly-a 10,000 K TRACE: AR Loops on 19 APR 2001 TRACE Cooling Loops Fe IX 171 1 MK Fe IX 171 1 MK 25
SOT EIS FPP XRT Japanese Hinode Spacecraft in Cooperation with US and UK • Spacecraft is in 800 km Sun-synchronous orbit • Includes set of three instruments: • - 0.5m Solar Optical Telescope (SOT) for • 150 km images and vector magnetograms • - EUV Imaging Spectrometer (EIS) for • plasma velocity, temperature and density • - X-ray Telescope (XRT) to image X-ray • emitting coronal structures • Hinode was launched in September, • 2006 • - making major advances in high resolution • structure and magnetic field studies • Instrument responsibilities: • - SOT/FPP: NAOJ, ISAS/Lockheed, HAO • - EIS: MSSL, Birmingham, RAL with US NRL • - XRT: Harvard CfA, NAOJ, ISAS 26
50000km (size of Earth) Solar Optical Telescope (SOT) on Hinode Emerging Magnetic Flux Convection 27
Hinode SOT Observation of Prominence Dynamics • Ca II H-line observations of a hedgerow prominence on the W-limb, 30-NOV-06 (Berger, 2007) • Dark channels rise vertically at ~ 10km/s • to ~ 15 Mm above the limb • Associated bright channels show related • downflows • Suggests hot rising thermal plumes and • density enhanced turbulent downflows • Current models have low-b prominence • plasma constrained to follow B field • Observation suggests turbulent B field • motion or the presence of convection in • high-b plasma
Polar Coronal Activity – XRT and EIS Jet Observations + • Hinode XRT sees • constant activity in • polar Coronal Holes • - coronal jets • First observed with • Yohkoh SXT by • Shibata et al. (1995) • Flux emerging in open magnetic field structure can produce jets • Blueshift of 30 km/s above the bright point in the polar coronal hole is interpreted as a jet caused by • reconnection (Kamio et al. 2007) 29
XRT HeII 256 FeXV 284 Hinode XRT Image EIS spectrum (1arcsec slit width) CoronalDynamics Hinode/EIS Spectral Imaging Observations • EIS scanned a 40 arcsec • wide strip with a height of • 7 arcmin • Slot images, 40 arc sec • wide, are displayed for • lines of He II and Fe XV • Resolved spectrum taken • with a 1 arcsec slit from • a pixel near the bottom of • the slit is shown • “First Light” spectrum in • early November, 2006 Wavelength (nm) 30
STEREO Mission • Solar-Terrestrial Relations Observatory • Two identical spacecraft leading and following the Earth • Launch - October, 2006 • Four instrument packages • SECCHI • PLASTIC • SWAVES • IMPACT • Goal: • Understand the origin and consequences of CMEs 32
SECCHI - US NRL Sun-Centered Imaging Package (COR-1, COR-2, EUVI) EUV Corona and 1.4 – 15 R White Light PLASTIC Instrument U. New Hampshire High Charge Ions IMPACT Solar Energetic Particles (SEP) U. Cal Berkeley Deployed SWAVES Radio Burst Antennae U. Paris Meudon SECCHI - UK RAL Heliospheric Imager (HI: 12 – 300 R) Deployed IMPACT Boom IMPACT Magnetometer (MAG) IMPACT Suprathermal Electron Detector (STE) IMPACT Solar Wind Electron Analyzer (SWEA) STEREO-B (Behind) Spacecraft and Instruments • Stereo-A (Ahead) has identical instrument suite • A and B spacecraft are now 150 deg apart
SECCHI – EUVI • EUV multilayer solar telescope - Images at Fe IX 171Å, Fe XII 195Å, Fe XIV 211Å, He II 304Å • Larger detector than EIT (2048x2048 pixels) leads to - Higher spatial resolution (1.6 arcsec vs. 2.5 arcsec) - Larger field-of-view (1.7 Rʘ vs. 1.4 Rʘ) • Higher data rate ensures higher image cadence (2.5 min vs 30 min) SECCHI – COR1 & COR2 • Two coronagraphs do a similar job to the three coronagraphs on LASCO • COR1 • - 1.1 - 3.0 Rʘ and 7.5 arcsec pixels • - Measures polarization • COR2 • - 2 - 15 Rʘ and 14 arcsec pixels • - Higher spatial resolution and time cadence than LASCO C3 34
STEREO Mission OrbitsTwo identical spacecraft “lead” and “lag” Earth 4 yr. 3 yr. Ahead @ +22/year 2 yr. 1 yr. Sun Sun Earth 1yr. Ahead Behind @ -22/year Earth 2yr. Behind 3 yr. 4 yr. Heliocentric Inertial Coordinates (Ecliptic Plane Projection) Geocentric Solar Ecliptic Coordinates Fixed Earth-Sun Line (Ecliptic Plane Projection)
STEREO Spacecraft Positions • On 5th August 2010, positions were with 150 degree separation - to see the positions at any time go to: http://stereo-ssc.nascom.nasa.gov/where/ 710 790 38
NASA Solar Dynamics Observatory (SDO) • SDO is the first mission to provide full-sun imaging both above and below the Sun’s surface • Includes set of three instruments: - High Resolution Imager (HRI) for precision velocity measurements and vector magnetograms - Atmospheric Imaging Array (AIA) uses 4 telescopes for high-speed EUV images of the Corona - Extreme Ultraviolet Variablity Experiment (EVE) gives well calibrated EUV irradiance measurements • SDO, launched in February, 2010, is designed to operate for 10 years - All instruments are fully operational - Generates ~ 2 Tbyte/day of data from its main instruments!
Recent Images from the SDO AIA Instrument • Four dual-channel telescopes of similar design • to TRACE obtain images of photosphere, • chromosphere and corona for • 5000 K ≤ Te ≤ 20 MK • - 8 images/10s; pixel size: 0.6 arcsec; • FoV: 41arcmin x 41arcmin (full Sun) • Fe XX, Fe XXIII and Fe XXIV bands • available for the high Te flare plasma SDO: AR and Filament SDO: Pre-flare AR Structures SDO: AR Loops (AIA) B-field (HMI) Blue: -ve Orange: +ve Fe IX 171 1 MK Fe IX 171 1 MK
Solar Orbiter – Mission to the Inner Heliosphere • ESA/NASA mission - launch ~2017 • Approach to 0.29 AU of the Sun - up to 35o above ecliptic plane • Carries remote sensing and in-situ instruments • In-situ: • - Energetic Particle Detector • - Magnetometer • - Radio and Plasma Wave detector • - Solar Wind Analyser • Remote sensing: • - Visible Imager and Magnetograph • - EUV Imager • - EUV Spectrometer • - Coronagraph • - Heliospheric Imager • - X-ray Imager 41
Solar Probe Plus – NASA Solar Encounter Mission • Launch 2015 or 2017 • - remains in ecliptic plane • - approach to within 0.05 AU of Sun • No forward viewing solar instruments • - emphasizes in-situ observations • - sample plasmas and dust in outer corona • In-situ instruments include • - Fast Ion and electron analyzers • - Ion Composition Analyzer • - Energetic Particle Instrument • - Magnetometer • - Plasma Wave Instrument • - Neutron/Gamma-ray Spectrometer • - Coronal Dust Detector • Also carries side-viewing Heliospheric • Imager • Observations complimentary to those • of Solar Orbiter
Japan’s SOLAR-C - two mission concepts under study Plan A - out-of-ecliptic magnetic field, X-ray, optical andhelioseismic observations - emphasise studies at high solar latitude - investigate meridional flow and magnetic structure inside Sun to convection zone base Plan B - high spatial resolution, throughput and cadence spectroscopic/polarimetric observations at optical, EUV and X-ray wavelengths - emphasise photosphere to corona connection - investigate solar magnetism and its role in the heating and dynamics of solar atmosphere Launch Date: Japanese fiscal year 2016(provisional) - anticipate productive joint observations with complimentary solar missions - NASA SDO (whole sun field of view) - ESA/NASA Solar Orbiter - NASA Solar Probe Plus 44
Sun – Earth Connection Sun Interplanetary Medium Near-Earth Environment Flares, Coronal Mass Ejections, Energetic Particles Coronal Mass Ejection, Solar Wind Shock Ionosphere Atmosphere Radiationbelt
Filament Eruption and Flare – 19-May-2007 Ha movie from Kanzelhöhe Observatory STEREO – A and – B reconstruction of erupting material in He II 304 Å and Fe VIII 171 Å emission TRACE 171 Å movie – flare ribbons and eruption
Halo CME on 28-OCT-2003 • Halo CMEs are likely to be Earth-directed • - disturbances near Earth when ejected magnetic field is opposite to Earth’s field
CME-related Magnetic Clouds Near-Earth • At the Sun CMEs always involve twisted magnetic field structures or “fluxropes” • CMEs are observed in situ as transients in IP space with changes to physical parameters • stronger magnetic field (low b value) with smooth rotation indicating a twisted flux rope structure • higher density and lower temperature than the surrounding solar wind with boundary discontinuities • Spacecraft intercepting a cloud near Earth can measure its magnetic and plasma properties • - components of B give cloud magnetic Flux • - cloud model and B values yield magnetic Helicity B - Axial • Magnetic Flux is associated with a solar region • or area e.g. Active Region, Filament channel • -Φ = ∫ ∫ B. dS weber(maxwells) • MagneticHelicity H = ∫V A.B dV where A is the • vector potential with B = xA B - Azimuthal • Magnetic Helicity a globally conserved quantity • - Convection zone → Corona → IPM • In-situ measurements with magnetometers and ion analysers
ACE In-situ Observation of a Magnetic Cloud – 15th May, 1997 Solar Wind proton velocity step shows shock arrival Shock Density decreases through sheath to low value in cloud Magnetic Cloud Sheath Magnetic field shows strength increase after shock Magnetic field direction angle shows uniform rotation inside cloud Electron pitch angle distribution suggests bi-directional flow