Interferometric Techniques for Impulsive Signals at Radio/Microwave Frequencies Interferometry in UHE particle astrophysics Andres Romero-Wolf Jet Propulsion Laboratory, California Institute of Technology April 22, 2012 April 22, 2013 A. Romero-Wolf 0 Interferometric Techniques for Impulsive Signals at Radio/Microwave Frequencies Interferometry in UHE particle astrophysics Andres Romero-Wolf Jet Propulsion Laboratory, California Institute of Technology April 22, 2012 April 22, 2013 A. Romero-Wolf 1 Motivation • First detection of ultra-high energy neutrinos are expected to lie close to the detector threshold. • Increased demands for higher sensitivity techniques to reduce the detection threshold. • Interferometric techniques have been applied for decades to detect weak signals. April 22, 2013 A. Romero-Wolf 2 Radio Interferometry Applied to Imaging and Astrometry April 22, 2013 A. Romero-Wolf 3 Imaging VLA VLBA M87 Image credit: http://www.nrao.edu/images/M87_trifold.jpg Image Credit: http://www.vlba.nrao.edu/sites/ April 22, 2013 A. Romero-Wolf 4 Astrometry Very Long Baseline Interferometry applied to identifying a source location. Image Credit: O. Sovers, J. Fanselow, and C.S. Jacobs, Reviews of Modern Physics, Vol. 70, No. 4, October 1998 200 µas (1 nanoradian) resolution. Applied to spacecraft navigation catalogues, measuring Earth motion parameters, plate tectonics, etc. Delay and delay rate are partial derivatives of the phase. April 22, 2013 A. Romero-Wolf 5 Astrometry Astrometric Density Astrometric time-series display typical source location variations of 200 µas for the most compact sources. Image Credit: http://astrogeo.org/images/J2236+2828/J2236+2828_X_2003_05_07_pus_map.ps Image Credit: C.M. King, JPL / UH Manoa Image Credit: C.M. King, JPL / UH Manoa April 22, 2013 A. Romero-Wolf 6 Ultra-high Energy Particle Astrophysics April 22, 2013 A. Romero-Wolf 7 Ultra-high Energy Cosmic Rays Charged particles of cosmic origin constantly bombard the Earth’s atmosphere. Protons and nucleons are observed with the energy of a well thrown fastball. April 22, 2013 A. Romero-Wolf 1 per 1000 km2 per year 1 per 10 km2 per year 8 What are the sources of the highest energy particles observed in the Universe? Particles with energies > 1020 eV require very powerful and efficient accelerators. Magnetic Field Amplitude, Gauss What Are The Sources of the Highest Energy Particles in the Universe? Active Galactic Nucleus Gamma Ray Bursts Supernova Remnants Inter-galactic magnetic shocks Size, cm April 22, 2013 A. Romero-Wolf 9 Extended Air Showers Ultra-high energy cosmic rays interact with the Earth’s atmosphere to produce showers of secondary particles. These extended air showers are observed with particle counters on the ground and by UV fluorescence. April 22, 2013 A. Romero-Wolf 10 Geosynchrotron Radiation • The extended air shower contains a significant quantity of positrons and electrons moving at nearly the speed of light. • The Earth’s geomagnetic field separates the charges producing coherent synchrotron radiation April 22, 2013 A. Romero-Wolf ve- Transverse current gives polarization vector. v q q q=-|e| ve+ q=+|e| y B Magnetic field Shower Axis z x 11 Radio Detection of Extended Air Showers • First observed in the 1960’s by Jelley. • Active field during the 1960’s and 1970’s. • The technique has been revived in the last decade with modern radio detection techniques. April 22, 2013 A. Romero-Wolf Radio image produced by cosmic ray impulse data from the LOPES detector. 12 Cosmic Rays and Neutrinos • Cosmic photon backgrounds attenuate UHECR energy • Interaction threshold at 4x1019 eV • UHECRs observed with E>4x1019 eV must be within 100 MPc Cosmic Distance Scales Milkyway: 30 kpc Andromeda: 800 kpc away. Cen A: 4Mpc Virgo Cluster: 17 Mpc Coma Cluster: 90 Mpc April 22, 2013 A. Romero-Wolf 13 Neutrino Radio Detection Antenna Detector Outside of Target Target SALSA Antennas in salt domes Dense and RF Transparent Cosmic Neutrino Particle shower 20% charge excess L<l Interaction point Radio Emission Coherent Cherenkov Radiation Cone April 22, 2013 A. Romero-Wolf RICE Dipole antennas in South Pole ice. Antenna Detector in Target ARA Large detector antenna network in South Pole GLUE Lunar regolith target with DSN antenna. 14 The ANITA Ultra-high Energy Particle Telescope • Synoptic horn antenna array (200-1200 MHz) • Circumpolar trajectory on a balloon. April 22, 2013 A. Romero-Wolf 15 15 Neutrino Limits with ANITA ANITA provides the strongest limits to ultra-high energy neutrino fluxes to date. Several models of ultra-high energy neutrino production have been ruled out. April 22, 2013 A. Romero-Wolf 16 Geosynchrotron Radiation Detected with ANITA. Radar backscatter amplitude • Detected with ANITA in UHF band (200-1200 MHz). • ANITA-3 (2013) will be tuned to detect hundreds. April 22, 2013 A. Romero-Wolf 17 Interferometry in Ultra-high Energy Particle Astrophysics April 22, 2013 A. Romero-Wolf 18 Impulse response Or Effective Height Voltage Electric Field Impulse Response Time Frequency v=E★ h Voltage Electric Field Time Frequency ANITA horn antenna effective height April 22, 2013 A. Romero-Wolf 19 Geometric Delay • Beam forming combines the signals from multiple antennas. • The geometric delay is the basic quantity that connects multiple observations of the same signal. April 22, 2013 A. Romero-Wolf 20 The ANITA Array • • • ANITA antenna array observes the same impulse with multiple channels. The array is unusual in that the antennas are not all pointed in the same direction. The arrangement is designed for full azimuthal coverage. April 22, 2013 A. Romero-Wolf 21 Beam-forming The signals from the previous slide are aligned in time according to the true geometric delay of the signal. The directional response of the antennas does not affect the phase of the signal and it can be added coherently. April 22, 2013 A. Romero-Wolf 22 Coherently Summed Waveform Power Global image of the coherently summed power for each assumed direction of the incident radiation. The direction of true incidence presents itself as a sharp peak. The diametrically opposed direction sees the thermal noise background. April 22, 2013 A. Romero-Wolf 23 Beam-forming with Cross-correlations Cross-correlations of an impulsive signal event. The time-domain cross-correlation is mapped to incident direction via the geometric delay relation. April 22, 2013 A. Romero-Wolf 24 Beam-forming with Cross-correlations Example of a global coherence map derived from the sum of cross-correlations. The true direction of the signal presents itself as a sharp peak. The map is analogous to the dirty map of radio interferometry. April 22, 2013 A. Romero-Wolf 25 Beam-forming with Cross-correlations Examples of signals and background s detected with ANITA. April 22, 2013 A. Romero-Wolf 26 Angular Error ANITA-I The ANITA array has < 1-degree angular errors. This is due to the ultra-wideband signals used in the correlation. April 22, 2013 A. Romero-Wolf 27 Angular Error ANITA-II The ANITA array has < 1-degree angular errors. This is due to the ultra-wideband signals used in the correlation. April 22, 2013 A. Romero-Wolf 28 Summed Waveforms vs. Cross-Correlations The relation between the summed waveform signal to noise ratio and crosscorrelation coefficient reveals features that are specific to each kind of signal and background. April 22, 2013 A. Romero-Wolf 29 Thermal Noise Rejection A discriminant formed by the linear combination of the cross correlation coefficient and the peak of the summed waveform provides a highly efficient filter. April 22, 2013 A. Romero-Wolf 30 Discrimination Techniques Thermal noise and carrier wave signal backgrounds both have comparable peak and secondary lobes. April 22, 2013 A. Romero-Wolf 31 Signal Strength The peak of the coherent waveform sum provides additional efficient discrimination between signals of interest and thermal noise. April 22, 2013 A. Romero-Wolf 32 Imaging the Sun Averaging events in a sun-centered coordinate system reveals a radio image of the sun along with its reflection on the ice. These images can be used to measure the surface roughness of the ice. See talk by J. Stockham. April 22, 2013 A. Romero-Wolf 33 Imaging Anthropogenic Backgrounds Clusters of events that pass all cuts provide locations of anthropogenic backgrounds. Not all clusters originate from identified field camps. April 22, 2013 A. Romero-Wolf 34 Imaging Anthropogenic Backgrounds Average Correlation Coefficient Imaging of all data, including thermal noise, provides a complementary view of the Antarctic noise sources. ANITA-1 April 22, 2013 A. Romero-Wolf 35 Imaging Anthropogenic Backgrounds Average Correlation Coefficient ANITA-2 April 22, 2013 A. Romero-Wolf 36 Conclusions Pulse-phase interferometry offers highly sensitive techniques for analysis of ultra-high energy particle transients. Implementation of this technique into a real-time digitization and triggering scheme can yield improvements in detection sensitivity. Research described herein done under contract with NASA. Copyright ©2013 Jet Propulsion Laboratory, California Institute of Technology. Government sponsorship acknowledged. April 22, 2013 A. Romero-Wolf 37