Abstract

Aims.This paper describes the Polarimetric and Helioseismic Imager on the Solar Orbiter mission (SO/PHI), the first magnetograph and helioseismology instrument to observe the Sun from outside the Sun-Earth line. It is the key instrument meant to address the top-level science question: How does the solar dynamo work and drive connections between the Sun and the heliosphere? SO/PHI will also play an important role in answering the other top-level science questions of Solar Orbiter, while hosting the potential of a rich return in further science.Methods.SO/PHI measures the Zeeman effect and the Doppler shift in the Fe I617.3 nm spectral line. To this end, the instrument carries out narrow-band imaging spectro-polarimetry using a tunable LiNbO3Fabry-Perot etalon, while the polarisation modulation is done with liquid crystal variable retarders. The line and the nearby continuum are sampled at six wavelength points and the data are recorded by a 2k × 2k CMOS detector. To save valuable telemetry, the raw data are reduced on board, including being inverted under the assumption of a Milne-Eddington atmosphere, although simpler reduction methods are also available on board. SO/PHI is composed of two telescopes; one, the Full Disc Telescope, covers the full solar disc at all phases of the orbit, while the other, the High Resolution Telescope, can resolve structures as small as 200 km on the Sun at closest perihelion. The high heat load generated through proximity to the Sun is greatly reduced by the multilayer-coated entrance windows to the two telescopes that allow less than 4% of the total sunlight to enter the instrument, most of it in a narrow wavelength band around the chosen spectral line.Results.SO/PHI was designed and built by a consortium having partners in Germany, Spain, and France. The flight model was delivered to Airbus Defence and Space, Stevenage, and successfully integrated into the Solar Orbiter spacecraft. A number of innovations were introduced compared with earlier space-based spectropolarimeters, thus allowing SO/PHI to fit into the tight mass, volume, power and telemetry budgets provided by the Solar Orbiter spacecraft and to meet the (e.g. thermal) challenges posed by the mission’s highly elliptical orbit.

Highlights

  • The Sun’s magnetic field is to a large extent responsible for driving a host of active phenomena, ranging from sunspots at its surface to coronal mass ejections propagating through the heliosphere (Solanki et al 2006; Wiegelmann et al 2014)

  • SO/PHI will be the first magnetograph to observe the Sun from vantage points away from the Sun-Earth line. This will allow it to provide unique information that will address a series of fundamental solar physics questions that are not addressed in the Solar Orbiter Red Book, in other words science questions that go beyond the four top-level science goals of Solar Orbiter

  • While the continuum intensity can be considered a good proxy of the photospheric temperature at optical depth τ = 1, the other two physical quantities are derived from the imprints that physical mechanisms leave on the shapes of the four Stokes profiles of the Fe i 6173 Å line probed by SO/PHI

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Summary

Methods

SO/PHI measures the Zeeman effect and the Doppler shift in the Fe i 617.3 nm spectral line. To this end, the instrument carries out narrow-band imaging spectro-polarimetry using a tunable LiNbO3 Fabry-Perot etalon, while the polarisation modulation is done with liquid crystal variable retarders. The high heat load generated through proximity to the Sun is greatly reduced by the multilayer-coated entrance windows to the two telescopes that allow less than 4% of the total sunlight to enter the instrument, most of it in a narrow wavelength band around the chosen spectral line. A number of innovations were introduced compared with earlier space-based spectropolarimeters, allowing SO/PHI to fit into the tight mass, volume, power and telemetry budgets provided by the Solar Orbiter spacecraft and to meet the (e.g. thermal) challenges posed by the mission’s highly elliptical orbit. Key words. instrumentation: polarimeters – techniques: imaging spectroscopy – techniques: polarimetric – Sun: photosphere – Sun: magnetic fields – Sun: helioseismology

Introduction
Top level science questions
What is the structure of the solar rotation?
What is the structure of the meridional flow?
How is magnetic flux reprocessed at high solar latitudes?
Is a small-scale turbulent dynamo process acting on the Sun?
What are the solar sources of the heliospheric magnetic field?
How do solar transients drive heliospheric variability?
Science going beyond the core science aims of Solar Orbiter
Solar irradiance and luminosity variations
What is the nature of solar magnetoconvection?
What is the 3D geometry of the solar surface?
How does the brightness of magnetic features change over the solar disc?
How do active regions and sunspots evolve?
What is the global structure of the solar magnetic field?
Where does magnetic reconnection of importance for coronal heating take place?
Improving space weather forecasting
Instrument overview
Data products
Technical implementation and subsystems
Choice of the monochromatic filter
Choice of the optical arrangement of the filtergraph
Implications for the telescopes
Opto-mechanical layout
Architecture of baffling system and false light control
Structural design
Folding scheme
Protection from the intense solar load
Polarisation analysis system
Filtergraph
O-Unit thermal loads
O-Unit thermal design concept
O-Unit thermal analysis
Mechanical testing
Thermal testing
The E-Unit housing
Thermal analysis of the E-Unit
On-ground optical verification and ground calibration
In-flight calibration
Scientific operations
Software operations concept
Data acquisition
On-board data processing
Pre-processing
Inversion of the Stokes profiles
Findings
Additional on-board processing pipelines
Full Text
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