Limiting the effects of earthquakes on gravitational-wave interferometers

被引:19
作者
Coughlin, Michael [1 ]
Earle, Paul [2 ]
Harms, Jan [3 ,4 ]
Biscans, Sebastien [5 ]
Buchanan, Christopher [6 ]
Coughlin, Eric [7 ]
Donovan, Fred [5 ]
Fee, Jeremy [2 ]
Gabbard, Hunter [8 ]
Guy, Michelle [2 ]
Mukund, Nikhil [9 ]
Perry, Matthew [10 ]
机构
[1] Harvard Univ, Dept Phys, Cambridge, MA 02138 USA
[2] US Geol Survey, Golden, CO 80401 USA
[3] Ist Nazl Fis Nucl, Sez Firenze, I-50019 Sesto Fiorentino, Italy
[4] Univ Urbino Carlo Bo, I-61029 Urbino, Italy
[5] MIT, LIGO Lab, Cambridge, MA 02138 USA
[6] Louisiana State Univ, Dept Phys & Astron, Baton Rouge, LA 70803 USA
[7] Luther Coll, Dept Comp Sci, 700 Coll Dr, Decorah, IA 52101 USA
[8] Max Planck Inst Gravitat Phys, Albert Einstein Inst, D-30167 Hannover, Germany
[9] IUCAA, Post Bag 4, Pune 411007, Maharashtra, India
[10] Planetary Sci Inst, Lakewood, CO 80401 USA
基金
美国国家科学基金会;
关键词
earthquakes; LIGO; gravitational waves; SEISMIC NETWORK;
D O I
10.1088/1361-6382/aa5a60
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
Ground-based gravitational wave interferometers such as the Laser Interferometer Gravitational-wave Observatory (LIGO) are susceptible to ground shaking from high-magnitude teleseismic events, which can interrupt their operation in science mode and significantly reduce their duty cycle. It can take several hours for a detector to stabilize enough to return to its nominal state for scientific observations. The down time can be reduced if advance warning of impending shaking is received and the impact is suppressed in the isolation system with the goal of maintaining stable operation even at the expense of increased instrumental noise. Here, we describe an early warning system for modern gravitational-wave observatories. The system relies on near real-time earthquake alerts provided by the U.S. Geological Survey (USGS) and the National Oceanic and Atmospheric Administration (NOAA). Preliminary low latency hypocenter and magnitude information is generally available in 5 to 20 min of a significant earthquake depending on its magnitude and location. The alerts are used to estimate arrival times and ground velocities at the gravitational-wave detectors. In general, 90% of the predictions for ground-motion amplitude are within a factor of 5 of measured values. The error in both arrival time and ground-motion prediction introduced by using preliminary, rather than final, hypocenter and magnitude information is minimal. By using a machine learning algorithm, we develop a prediction model that calculates the probability that a given earthquake will prevent a detector from taking data. Our initial results indicate that by using detector control configuration changes, we could prevent interruption of operation from 40 to 100 earthquake events in a 6-month time-period.
引用
收藏
页数:14
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