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Featured researches published by R. Stone.


Classical and Quantum Gravity | 2008

The LSC glitch group: monitoring noise transients during the fifth LIGO science run

L. Blackburn; L. Cadonati; S. Caride; S. Caudill; S. Chatterji; N. Christensen; J. Dalrymple; S. Desai; A. Di Credico; Gregory Ely; J. Garofoli; L. M. Goggin; G. González; R. Gouaty; C. Gray; A. M. Gretarsson; D. Hoak; T. Isogai; E. Katsavounidis; J. S. Kissel; Sergey Klimenko; R. A. Mercer; S. R P Mohapatra; S. Mukherjee; F. J. Raab; K. Riles; P. R. Saulson; R. Schofield; P. Shawhan; J. Slutsky

The LIGO Scientific Collaboration (LSC) glitch group is part of the LIGO detector characterization effort. It consists of data analysts and detector experts who, during and after science runs, collaborate for a better understanding of noise transients in the detectors. Goals of the glitch group during the fifth LIGO science run (S5) included (1) offline assessment of the detector data quality, with focus on noise transients, (2) veto recommendations for astrophysical analysis and (3) feedback to the commissioning team on anomalies seen in gravitational wave and auxiliary data channels. Other activities included the study of auto-correlation of triggers from burst searches, stationarity of the detector noise and veto studies. The group identified causes for several noise transients that triggered false alarms in the gravitational wave searches; the times of such transients were identified and vetoed from the data generating the LSC astrophysical results.


Classical and Quantum Gravity | 2009

Environmentally induced nonstationarity in LIGO science run data

R. Stone; S. Mukherjee

NoiseFloorMon is a data monitoring tool (DMT) implemented at the LIGO sites to monitor instances of non-stationarity in the gravitational-wave data that are correlated with physical environmental monitors. An analysis of the fifth science run is nearly complete, and test runs preceding the sixth science run have also been analyzed. These analyses have identified time intervals in the gravitational-wave channel that indicate non-stationarity due to seismic activity, and these intervals are referred to as data quality flags. In the analyses conducted to date the majority of time segments identified as non-stationary were due to seismic activity at the corner station and the x-arm end station. We present the algorithm and its performance, and discuss the potential for an on-site pipeline that automatically generates data quality flags for use in future data runs.


Astronomy and Astrophysics | 1999

A HELIOSPHERIC DENSITY MODEL AND TYPE III RADIO BURSTS

G. Mann; F. Jansen; R. J. MacDowall; Michael L. Kaiser; R. Stone


Bulletin of the American Physical Society | 2016

A low-latency Glitch Classification Algorithm Based in Waveform Morphology

Hunter Gabbard; S. Mukherjee; R. Stone


Bulletin of the American Physical Society | 2014

RiSA: A Science Festival for the Bilingual and Bicultural Rio Grande Valley

Joey Shapiro Key; Cristina Torres; R. Stone


Bulletin of the American Physical Society | 2013

A comparison of methods to characterize non-stationarity in time series data

R. Stone; S. Mukherjee


Geophysical monograph | 2000

The astronomical low frequency array : A proposed explorer mission for radio astronomy

D. L. Jones; Ronald J. Allen; J. Basart; T. S. Bastian; W. Blume; J.-L. Bougeret; B. Dennison; M.D. Desch; K. S. Dwarakanath; W. Erickson; D. A. Finley; Nat Gopalswamy; R. Howard; Michael L. Kaiser; Namir E. Kassim; T. Kuiper; Robert J. MacDowall; M. Mahoney; Richard A. Perley; R. Preston; M. Reiner; P. Rodriguez; R. Stone; Stephen C. Unwin; Kurt W. Weiler; G. Woan; R. Woo

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S. Mukherjee

University of Texas at Brownsville

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Michael L. Kaiser

Goddard Space Flight Center

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C. Gray

National Science Foundation

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D. Hoak

University of Massachusetts Amherst

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D. L. Jones

California Institute of Technology

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E. Katsavounidis

Massachusetts Institute of Technology

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F. J. Raab

National Science Foundation

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