Understanding and calibrating ionospheric effects. Dr Natasha Hurley-Walker Curtin University / ICRAR

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Understanding and calibrating ionospheric effects Dr Natasha HurleyWalker Curtin University / ICRAR

Ionosphere Multiple layers during the day Transitions to fewer at night Smallscale turbulence Largescale coherent features By Bhamer, updated to SVG by tizom English Wikipedia, Public Domain, https://commons.wikimedia.org/w/index.php?curid=2178742

Global ionospheric variations https://services.swpc.noaa.gov

Faraday rotation By DrBob https://en.wikipedia.org/wiki/file:faradayeffect.svg Lenc et al. (2016): Lowfrequency observations of linearly polarized structures in the ISM Blue = RM estimates from Albus; Red = RM estimates from IonFR; Green = RM measurements from the MWA toward a source of known RM

Refraction θ= 1 8π 2 e 2 η 0 m e 1 ν 2 TEC Different phase delays ε 1 and ε 2 yield geometric phase delay ΔΦ, due to the incoming signal emanating from a different [apparent] direction. Cohen & Rottgering (2009): Probing FineScale Ionospheric Structure with the VLA

Design implications A = Array size V = field of View S = ionospheric Scale Lonsdale (2005): Configuration Considerations for LowFrequency Arrays

Regime 2: A>>S, V<<S: VLA Seeing same dtec

Regime 2: A>>S, V<<S: VLA Seeing different dtec

Regime 2: A>>S, V<<S: VLA 1min snapshots of bright source w/ VLA (A) at 74MHz 30s interval phase gradients across the VLA (A) Cotton (2005): Lessons from the VLA Long Wavelength Sky Survey (VLSS)

Regime 2: A>>S, V<<S: VLA Seeing different dtec Δθ will be solved for when calculating the complex antenna gains Selfcalibration on short timescales may be necessary

Regime 3: A<<S, V>>S: MWA 128T Seeing same dtec

Regime 3: A<<S, V>>S: MWA 128T Seeing different dtec

Regime 3: A<<S, V>>S: MWA 128T

Regime 3: A<<S, V>>S: MWA 128T Seeing different dtec Δθ varies spatially and cannot be fixed in the visibilities As there is no antenna dependence, it can be fixed perfectly in image space

Regime 3: A<<S, V>>S: MWA 128T https://github.com/nhurleywalker/fits_warp HurleyWalker & Hancock (2018): Dedistorting ionospheric effects in the image plane

Regime 4: A, V >> S LOFAR GMRT

Directiondependent peeling What is peeling? Phaserotate your data to a source Solve for the antenna gains toward that source Multiply a model of the source by those gains Subtract the gainmodified source from the visibilities Repeat ad nauseum

Directiondependent peeling What is peeling? Phaserotate your data to a source Solve for the antenna gains toward that source Multiply a model of the source by those gains Subtract the gainmodified source from the visibilities Repeat ad nauseum Why peeling? Because this is both an imagebased problem AND an antennabased problem You cannot create a set of solutions in either (u,v) or (l,m) space and apply to the whole observation But, you can find and apply solution in one direction, and another, and another

Directiondependent peeling What is peeling? Phaserotate your data to a source Solve for the antenna gains toward that source Multiply a model of the source by those gains Subtract the gainmodified source from the visibilities Repeat ad nauseum Why peeling? Because this is both an imagebased problem AND an antennabased problem You cannot create a set of solutions in either (u,v) or (l,m) space and apply to the whole observation But, you can find and apply solution in one direction, and another, and another How do I do this? That depends...

Signaltonoise Creating complex (2parameter) gains for: Each polarisation Each frequency Each antenna Each direction Each time interval = huge signaltonoise problem Other sources (in sidelobes, in main lobe) reduce S/N on source (in direction) of interest

Signaltonoise Creating complex (2parameter) gains for: Each polarisation Each frequency Each antenna Each direction Each time interval = huge signaltonoise problem Other sources (in sidelobes, in main lobe) reduce S/N on source (in direction) of interest Every extra calibration parameter = less final S/N on astronomical problem e.g. Mouri & Koopmans (2018) Quantifying Suppression of the Cosmological 21cm Signal due to Direction Dependent Gain Calibration in Radio Interferometers http://adsabs.harvard.edu/abs/2018arxiv180903755m

Signaltonoise Creating complex (2parameter) gains for: Each polarisation Each frequency Each antenna Each direction Each time interval = huge signaltonoise problem Other sources (in sidelobes, in main lobe) reduce S/N on source (in direction) of interest Every extra calibration parameter = less final S/N on astronomical problem e.g. Mouri & Koopmans (2018) Quantifying Suppression of the Cosmological 21cm Signal due to Direction Dependent Gain Calibration in Radio Interferometers http://adsabs.harvard.edu/abs/2018arxiv180903755m How to increase S/N?

Building S/N: Appropriate time intervals (1s) For each antenna Φ ν

Building S/N: Appropriate time intervals (5s) For each antenna Φ ν

Building S/N: Ranking sources e.g. RTS Rank the sources by apparent brightness and peel sequentially

Building S/N: Ranking sources e.g. RTS Rank the sources by apparent brightness and peel sequentially

Building S/N: Ranking sources e.g. RTS Rank the sources by apparent brightness and peel sequentially Best S/N toward that direction

Building S/N: Ranking sources e.g. RTS Rank the sources by apparent brightness and peel sequentially Best S/N toward that direction

Building S/N: Ranking sources e.g. RTS Rank the sources by apparent brightness and peel sequentially Best S/N toward that direction Eventually your sky model needs to contain multiple sources

Building S/N: clustering sources e.g. Ionpeel, RTS, Factor Cluster size should be < S Sky model and primary beam model must be very accurate

Building S/N: frequencydependence e.g. Ionpeel, RTS, Factor θ= 1 8π 2 e 2 η 0 m e 1 ν 2 TEC

Building S/N: modelling the ionosphere e.g. SPAM Allows multiple antennas to contribute to the same phase screen solutions 5 antennas observe 3 calibrator sources (colored red/green/blue and labelled A to C) within the FoV. The (colored) LoSs from the array towards the sources run parallel for each source and pierce the phase screen at fixed height h (colored circles). (Note 1C & 4A and 2C & 5A overlap). Total (integrated) phase rotation along any LoS through the ionosphere is modeled by an instantaneous phase rotation at the phase screen height. Intema et al. (2008): Ionospheric calibration of low frequency radio interferometric observations using the peeling scheme

Building S/N: modelling the ionosphere e.g. SPAM Allows multiple antennas to contribute to the same phase screen solutions Maps the ionospheric phase variations above the array (Assuming they really are at the same height see Martin, Bray & Scaife (2016)) Example of an ionospheric phase screen model fit. The color map represents an ionospheric phase screen at 200 km height that was fitted to the peeling phase solutions of 8 calibrator sources at timeinterval n = 206 of 10 s during a VLSS observing run of the 74 MHz VLA in BnAconfiguration Intema et al. (2008): Ionospheric calibration of low frequency radio interferometric observations using the peeling scheme

Ionospheric calibration software summary Package Instrument Author(s) Webpage Obit VLA Bill Cotton www.cv.nrao.edu/~bcotton/obit.html SPAM GMRT, VLA Huib Intema www.intema.nl/doku.php?id=huibintemaspam Fits_warp MWA HW & Hancock github.com/nhurleywalker/fits_warp RTS MWA Mitchell & Ord sysadmin@mwa128t.org Ionpeel MWA Andre Offringa sysadmin@mwa128t.org LEAP MWA Rioja & Dodson Maria.rioja@icrar.org Sagecal LOFAR Sarod & Smirnov sourceforge.net/projects/sagecal/ DDFacet LOFAR Tasse & Smirnov github.com/saopicc/ddfacet Factor LOFAR van Weeren www.astron.nl/citt/facetdoc/